diff --git a/R/create_OSD.R b/R/create_OSD.R index f09e9a4d60..021cbd02f1 100644 --- a/R/create_OSD.R +++ b/R/create_OSD.R @@ -128,7 +128,7 @@ validateOSD <- function(logfile, filepath) { } # TODO: abstract and generalize these into rules - x <- trimws(raw[-grep("[A-Z '`][A-Z\\.'`]{2}[A-Z `']+.*|Ty[pic]+(al|fying)? ?[Pp]edon ?[:;\\-] ?.*|[A-Z]{3,}[:].*|\\(Colors are for", raw, invert = TRUE)]) + x <- trimws(raw[-grep("^[A-Z '`][A-Z \\.'`]{2}[A-Z `']+.*|Ty[pic]+(al|fying)? ?[Pp]edon ?[:;\\-] ?.*|[A-Z]{3,}[:].*|\\(Colors are for", raw, invert = TRUE)]) if (length(x) != length(unique(x))) { # x is all sorts of "headers" based on what the above pattern is allowed to match diff --git a/inst/extdata/OSD-error-reporting/RO/auburn-sections.csv b/inst/extdata/OSD-error-reporting/RO/auburn-sections.csv index e47b418379..fa595cb65a 100644 --- a/inst/extdata/OSD-error-reporting/RO/auburn-sections.csv +++ b/inst/extdata/OSD-error-reporting/RO/auburn-sections.csv @@ -7,8 +7,6 @@ "BOWMANTOWN","MULTILINE TYPICAL PEDON","[number of multilines=1]","auburn, al" "BREWTON","MULTILINE TYPICAL PEDON","[number of multilines=1]","auburn, al" "BUGLEY","DUPLICATION OF HEADERS","[RANGE IN CHARACTERISTICS:]","auburn, al" -"BUGLEY","DUPLICATE STANDARD SECTIONS","[RANGE IN CHARACTERISTICS]","auburn, al" -"BURTON","DUPLICATE STANDARD SECTIONS","[ADDITIONAL DATA]","auburn, al" "BUSSY","MULTILINE TYPICAL PEDON","[number of multilines=7]","auburn, al" "CANTUCHE","MULTILINE TYPICAL PEDON","[number of multilines=1]","auburn, al" "CHIPOLA","MULTILINE TYPICAL PEDON","[number of multilines=1]","auburn, al" @@ -16,7 +14,6 @@ "CITICO","MULTILINE TYPICAL PEDON","[number of multilines=6]","auburn, al" "CLOUDLAND","MULTILINE TYPICAL PEDON","[number of multilines=4]","auburn, al" "COLUMBUS","MULTILINE TYPICAL PEDON","[number of multilines=1]","auburn, al" -"CRAGGEY","DUPLICATE STANDARD SECTIONS","[ADDITIONAL DATA]","auburn, al" "DAWHOO","MULTILINE TYPICAL PEDON","[number of multilines=4]","auburn, al" "DEBUTE","MULTILINE TYPICAL PEDON","[number of multilines=7]","auburn, al" "DUCKBOTTOM","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Very-fine, kaolinitic, acid, thermic Fluvaquentic Endoaquepts]","auburn, al" diff --git a/inst/extdata/OSD-error-reporting/RO/bozeman-sections.csv b/inst/extdata/OSD-error-reporting/RO/bozeman-sections.csv index b5cbdafb02..ef1d24e179 100644 --- a/inst/extdata/OSD-error-reporting/RO/bozeman-sections.csv +++ b/inst/extdata/OSD-error-reporting/RO/bozeman-sections.csv @@ -24,7 +24,6 @@ "BALDRIDGE","MULTILINE TYPICAL PEDON","[number of multilines=5]","bozeman, mt" "BANDID","MULTILINE TYPICAL PEDON","[number of multilines=1]","bozeman, mt" "BARLOW","DUPLICATION OF HEADERS","[RANGE IN CHARACTERISTICS: The mean annual soil temperature ranges from 40 degrees to 47 degrees F. The average summer soil temperature is less than 47 degrees F. with an 0 horizon. The soils have an udic moisture regime. The driest period is in the summer but the soils are dry for less than 45 consecutive days. Depth to bedrock is 60 inches or more. Depth to stony glacial till ranges from 15 to 30 inches. Thickness of the solum ranges from 15 to 24 inches. The 10- to 40-inch control section has less than an average of 10 percent clay and has 20 to 30 percent sand coarser than very fine sand.,TYPE LOCATION: Clackamas County, Oregon; 200 feet west of the Timberline Highway; NE1/4 NE1/4 section 18, T.3S., R.9E. W.M.]","bozeman, mt" -"BARLOW","DUPLICATE STANDARD SECTIONS","[RANGE IN CHARACTERISTICS,TYPE LOCATION]","bozeman, mt" "BECKTON","MULTILINE TYPICAL PEDON","[number of multilines=1]","bozeman, mt" "BENDERLY","MULTILINE TYPICAL PEDON","[number of multilines=3]","bozeman, mt" "BICKERDYKE","DUPLICATION OF HEADERS","[SAR: 15 to 30]","bozeman, mt" @@ -143,7 +142,6 @@ "LAURENTZEN","MULTILINE TYPICAL PEDON","[number of multilines=5]","bozeman, mt" "LITTLE HORN","SECTION HEADINGS",NA,"bozeman, mt" "LOLITE","DUPLICATION OF HEADERS","[REMARKS:]","bozeman, mt" -"LOLITE","DUPLICATE STANDARD SECTIONS","[REMARKS]","bozeman, mt" "LOMA","MULTILINE TYPICAL PEDON","[number of multilines=1]","bozeman, mt" "LONGBRANCH","MULTILINE TYPICAL PEDON","[number of multilines=6]","bozeman, mt" "LONNA","DUPLICATION OF HEADERS","[SAR: 0 to 13]","bozeman, mt" @@ -220,7 +218,6 @@ "TEW","SECTION HEADINGS",NA,"bozeman, mt" "TEW","MULTILINE TYPICAL PEDON","[number of multilines=1]","bozeman, mt" "TEX","MULTILINE TYPICAL PEDON","[number of multilines=2]","bozeman, mt" -"TINE","DUPLICATE STANDARD SECTIONS","[USE AND VEGETATION]","bozeman, mt" "TINE","MULTILINE TYPICAL PEDON","[number of multilines=2]","bozeman, mt" "TOSTON","DUPLICATION OF HEADERS","[SAR: 13 to 30]","bozeman, mt" "TOUTLE","MULTILINE TYPICAL PEDON","[number of multilines=2]","bozeman, mt" @@ -233,7 +230,6 @@ "VANDA","DUPLICATION OF HEADERS","[SAR: 13 to 30]","bozeman, mt" "VANDERHOFF","MULTILINE TYPICAL PEDON","[number of multilines=3]","bozeman, mt" "VASQUEZ","DUPLICATION OF HEADERS","[DRAINAGE AND PERMEABILITY: Poorly drained; very slow runoff or ponded; moderate permeability. These soils have a fluctuating high water table.]","bozeman, mt" -"VASQUEZ","DUPLICATE STANDARD SECTIONS","[DRAINAGE AND PERMEABILITY,USE AND VEGETATION]","bozeman, mt" "VASQUEZ","MULTILINE TYPICAL PEDON","[number of multilines=1]","bozeman, mt" "VINCOM","DUPLICATION OF HEADERS","[SAR: 0 to 20]","bozeman, mt" "VOLINGER","MULTILINE TYPICAL PEDON","[number of multilines=1]","bozeman, mt" @@ -245,7 +241,6 @@ "WEINGART","DUPLICATION OF HEADERS","[SAR: 13 to 30]","bozeman, mt" "WELCOME","MULTILINE TYPICAL PEDON","[number of multilines=7]","bozeman, mt" "WHITEARTH","DUPLICATION OF HEADERS","[SAR: 20 to 60]","bozeman, mt" -"WILLAKENZIE","MULTILINE TYPICAL PEDON","[number of multilines=1]","bozeman, mt" "WILLOW CREEK","SECTION HEADINGS",NA,"bozeman, mt" "WINGDALE","MULTILINE TYPICAL PEDON","[number of multilines=5]","bozeman, mt" "WINRIDGE","MULTILINE TYPICAL PEDON","[number of multilines=4]","bozeman, mt" @@ -257,4 +252,3 @@ "YOST","MULTILINE TYPICAL PEDON","[number of multilines=2]","bozeman, mt" "YUTRUE","MULTILINE TYPICAL PEDON","[number of multilines=6]","bozeman, mt" "ZELDA","DUPLICATION OF HEADERS","[SAR: 13 to 30,SAR: 30 to 40]","bozeman, mt" -"ZENKER","DUPLICATE STANDARD SECTIONS","[REMARKS]","bozeman, mt" diff --git a/inst/extdata/OSD-error-reporting/RO/morgantown-sections.csv b/inst/extdata/OSD-error-reporting/RO/morgantown-sections.csv index f997ac430c..c36fe08943 100644 --- a/inst/extdata/OSD-error-reporting/RO/morgantown-sections.csv +++ b/inst/extdata/OSD-error-reporting/RO/morgantown-sections.csv @@ -1,34 +1,25 @@ "soilseriesname","errorkind","context","mlraoffice" "AMBOY","MULTILINE TYPICAL PEDON","[number of multilines=1]","morgantown, wv" "ANDERSONTOWN","MULTILINE TYPICAL PEDON","[number of multilines=2]","morgantown, wv" -"ANNAPOLIS","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" -"ANNEMESSEX","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" -"AQUASCO","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" "ASHVILLE","MULTILINE TYPICAL PEDON","[number of multilines=1]","morgantown, wv" "ATSION","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Sandy, siliceous, mesic Aeric Alaquods]","morgantown, wv" "ATSION","DUPLICATE STANDARD SECTIONS","[TAXONOMIC CLASS]","morgantown, wv" "BALTIMORE","MULTILINE TYPICAL PEDON","[number of multilines=3]","morgantown, wv" -"BELTSVILLE","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" "BERKS","MULTILINE TYPICAL PEDON","[number of multilines=1]","morgantown, wv" "BRANDYWINE","MULTILINE TYPICAL PEDON","[number of multilines=1]","morgantown, wv" "BURKETOWN","MULTILINE TYPICAL PEDON","[number of multilines=2]","morgantown, wv" "CALVERT","SECTION HEADINGS",NA,"morgantown, wv" "CHICONE","DUPLICATE STANDARD SECTIONS","[TAXONOMIC CLASS]","morgantown, wv" -"CHILI","DUPLICATE STANDARD SECTIONS","[REMARKS]","morgantown, wv" "CHILLUM","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Fine-silty, mixed, semiactive, mesic Typic Hapludults]","morgantown, wv" "CHILLUM","DUPLICATE STANDARD SECTIONS","[TAXONOMIC CLASS]","morgantown, wv" -"CHRISTIANA","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" "CHRISTIANA","MULTILINE TYPICAL PEDON","[number of multilines=1]","morgantown, wv" "CIDERMILL","MULTILINE TYPICAL PEDON","[number of multilines=3]","morgantown, wv" "COLEMANTOWN","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Fine, glauconitic, mesic Typic Albaquults]","morgantown, wv" -"COLEMANTOWN","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE,TAXONOMIC CLASS]","morgantown, wv" "COLTS NECK","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Fine-loamy, mixed, active, mesic Humic Hapludults]","morgantown, wv" "COLTS NECK","DUPLICATE STANDARD SECTIONS","[TAXONOMIC CLASS]","morgantown, wv" "COLYER","MULTILINE TYPICAL PEDON","[number of multilines=1]","morgantown, wv" "COOLVILLE","MULTILINE TYPICAL PEDON","[number of multilines=1]","morgantown, wv" "CRANSTON","MULTILINE TYPICAL PEDON","[number of multilines=2]","morgantown, wv" -"CUMBERSTONE","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" -"DEALE","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" "DONLONTON","MULTILINE TYPICAL PEDON","[number of multilines=5]","morgantown, wv" "ELKTON","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Fine-silty, mixed, active, mesic Typic Endoaquults]","morgantown, wv" "ELKTON","DUPLICATE STANDARD SECTIONS","[TAXONOMIC CLASS]","morgantown, wv" @@ -36,33 +27,22 @@ "EVENDALE","MULTILINE TYPICAL PEDON","[number of multilines=1]","morgantown, wv" "FAIRFAX","MULTILINE TYPICAL PEDON","[number of multilines=1]","morgantown, wv" "FENWICK","MULTILINE TYPICAL PEDON","[number of multilines=1]","morgantown, wv" -"FORT MOTT","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" "GALLOWAY","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Mesic, coated Aquic Quartzipsamments]","morgantown, wv" "GALLOWAY","DUPLICATE STANDARD SECTIONS","[TAXONOMIC CLASS]","morgantown, wv" "GREENWICH","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Coarse-loamy, mixed, semiactive, mesic Typic Hapludults]","morgantown, wv" -"GREENWICH","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE,TAXONOMIC CLASS]","morgantown, wv" -"GRIST MILL","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" -"GROSSTOWN","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" -"GUNSTON","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" -"HENLOPEN","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" -"HOGHOLE","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" "HOLLYWOOD","MULTILINE TYPICAL PEDON","[number of multilines=5]","morgantown, wv" "HURLOCK","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Coarse-loamy, siliceous, semiactive, mesic Typic Endoaquults]","morgantown, wv" "HURLOCK","DUPLICATE STANDARD SECTIONS","[TAXONOMIC CLASS]","morgantown, wv" "INGLESIDE","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Coarse-loamy, siliceous, semiactive, mesic Typic Hapludults]","morgantown, wv" "INGLESIDE","DUPLICATE STANDARD SECTIONS","[TAXONOMIC CLASS]","morgantown, wv" -"ISSUE","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" "KARS","MULTILINE TYPICAL PEDON","[number of multilines=4]","morgantown, wv" "KENTUCK","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Fine-silty, mixed, active, mesic Typic Umbraquults]","morgantown, wv" "KENTUCK","DUPLICATE STANDARD SECTIONS","[TAXONOMIC CLASS]","morgantown, wv" -"KINGSTOWNE","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" "KRESSON","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Fine, glauconitic, mesic Aquic Hapludults]","morgantown, wv" "KRESSON","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE,TAXONOMIC CLASS]","morgantown, wv" "LEIPSIC","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Fine-silty, mixed, semiactive, mesic Aquic Hapludults]","morgantown, wv" -"LEIPSIC","DUPLICATE STANDARD SECTIONS","[TAXONOMIC CLASS]","morgantown, wv" "LENBERG","MULTILINE TYPICAL PEDON","[number of multilines=1]","morgantown, wv" "MANOKIN","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Fine-loamy, mixed, active, mesic Aquic Hapludults]","morgantown, wv" -"MANOKIN","DUPLICATE STANDARD SECTIONS","[TAXONOMIC CLASS]","morgantown, wv" "MATAWAN","MULTILINE TYPICAL PEDON","[number of multilines=5]","morgantown, wv" "MILLROCK","MULTILINE TYPICAL PEDON","[number of multilines=1]","morgantown, wv" "MORRISON","MULTILINE TYPICAL PEDON","[number of multilines=1]","morgantown, wv" @@ -70,29 +50,22 @@ "MOSHUP","MULTILINE TYPICAL PEDON","[number of multilines=1]","morgantown, wv" "MUIRKIRK","MULTILINE TYPICAL PEDON","[number of multilines=5]","morgantown, wv" "OSSIPEE","MULTILINE TYPICAL PEDON","[number of multilines=1]","morgantown, wv" -"PAWCATUCK","MULTILINE TYPICAL PEDON","[number of multilines=1]","morgantown, wv" "PIANKESHAW","MULTILINE TYPICAL PEDON","[number of multilines=4]","morgantown, wv" "PINEGROVE","MULTILINE TYPICAL PEDON","[number of multilines=4]","morgantown, wv" "POMFRET","MULTILINE TYPICAL PEDON","[number of multilines=1]","morgantown, wv" "QUAKERBRIDGE","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Mesic, coated Spodic Quartzipsamments]","morgantown, wv" "QUEPONCO","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Fine-loamy, mixed, semiactive, mesic Typic Hapludults]","morgantown, wv" -"QUEPONCO","DUPLICATE STANDARD SECTIONS","[TAXONOMIC CLASS]","morgantown, wv" "QUINDOCQUA","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Fine-loamy, mixed, active, mesic Typic Endoaquults]","morgantown, wv" -"QUINDOCQUA","DUPLICATE STANDARD SECTIONS","[TAXONOMIC CLASS]","morgantown, wv" "RAINSBORO","MULTILINE TYPICAL PEDON","[number of multilines=3]","morgantown, wv" "RARDEN","MULTILINE TYPICAL PEDON","[number of multilines=4]","morgantown, wv" "SHELBYVILLE","MULTILINE TYPICAL PEDON","[number of multilines=6]","morgantown, wv" "TENT","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Fine-silty, mixed, active, mesic Typic Endoaquults]","morgantown, wv" "TIZZARD","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Sandy over loamy, aniso, siliceous, subactive, nonacid, mesic Sulfic Fluvaquents]","morgantown, wv" -"TIZZARD","DUPLICATE STANDARD SECTIONS","[TAXONOMIC CLASS]","morgantown, wv" "TRUSSUM","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Fine, mixed, active, mesic Typic Paleaquults]","morgantown, wv" "TRUSSUM","DUPLICATE STANDARD SECTIONS","[TAXONOMIC CLASS]","morgantown, wv" "URBANA","MULTILINE TYPICAL PEDON","[number of multilines=4]","morgantown, wv" -"WIDEWATER","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" -"WIST","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" "WOODMANSIE","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Coarse-loamy, siliceous, semiactive, mesic Typic Hapludults]","morgantown, wv" "WOODMANSIE","DUPLICATE STANDARD SECTIONS","[TAXONOMIC CLASS]","morgantown, wv" "WOODSTOWN","DUPLICATION OF HEADERS","[TAXONOMIC CLASS: Fine-loamy, mixed, active, mesic Aquic Hapludults]","morgantown, wv" "WOODSTOWN","DUPLICATE STANDARD SECTIONS","[TAXONOMIC CLASS]","morgantown, wv" "WOOLPER","MULTILINE TYPICAL PEDON","[number of multilines=4]","morgantown, wv" -"ZEKIAH","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","morgantown, wv" diff --git a/inst/extdata/OSD-error-reporting/RO/salina-sections.csv b/inst/extdata/OSD-error-reporting/RO/salina-sections.csv index 2d089242a7..a1365b3e48 100644 --- a/inst/extdata/OSD-error-reporting/RO/salina-sections.csv +++ b/inst/extdata/OSD-error-reporting/RO/salina-sections.csv @@ -34,6 +34,5 @@ "VARNA","SECTION HEADINGS",NA,"salina, ks" "VESPER","MULTILINE TYPICAL PEDON","[number of multilines=2]","salina, ks" "WABEDO","DUPLICATION OF HEADERS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: St. Paul, Minnesota]","salina, ks" -"WABEDO","DUPLICATE STANDARD SECTIONS","[MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE]","salina, ks" "WHITEBIRD","MULTILINE TYPICAL PEDON","[number of multilines=1]","salina, ks" "WOLCO","MULTILINE TYPICAL PEDON","[number of multilines=4]","salina, ks" diff --git a/inst/extdata/OSD-error-reporting/RO/wasilla-sections.csv b/inst/extdata/OSD-error-reporting/RO/wasilla-sections.csv index 5d490f44c9..fdc888461a 100644 --- a/inst/extdata/OSD-error-reporting/RO/wasilla-sections.csv +++ b/inst/extdata/OSD-error-reporting/RO/wasilla-sections.csv @@ -4,11 +4,7 @@ "ESHAMY","SECTION HEADINGS",NA,"wasilla, AK" "FROSTCIRCLE","MULTILINE TYPICAL PEDON","[number of multilines=1]","wasilla, AK" "KONIAG","DUPLICATION OF HEADERS","[GEOGRAPHIC SETTING:]","wasilla, AK" -"KONIAG","DUPLICATE STANDARD SECTIONS","[GEOGRAPHIC SETTING]","wasilla, AK" "KUSKOKWIM","SECTION HEADINGS",NA,"wasilla, AK" "KUSKOKWIM","MULTILINE TYPICAL PEDON","[number of multilines=2]","wasilla, AK" "NARROW CAPE","DUPLICATION OF HEADERS","[GEOGRAPHIC SETTING:]","wasilla, AK" -"NARROW CAPE","DUPLICATE STANDARD SECTIONS","[GEOGRAPHIC SETTING]","wasilla, AK" "REZANOF","DUPLICATION OF HEADERS","[GEOGRAPHIC SETTING:]","wasilla, AK" -"REZANOF","DUPLICATE STANDARD SECTIONS","[GEOGRAPHIC SETTING]","wasilla, AK" -"TOGHOTTHELE","DUPLICATE STANDARD SECTIONS","[ADDITIONAL DATA]","wasilla, AK" diff --git a/inst/extdata/OSD-error-reporting/log.txt b/inst/extdata/OSD-error-reporting/log.txt index f71aebf8f5..91a251d950 100644 --- a/inst/extdata/OSD-error-reporting/log.txt +++ b/inst/extdata/OSD-error-reporting/log.txt @@ -1,6 +1,6 @@ ### Problems by RO ### auburn, al bozeman, mt davis, ca morgantown, wv salina, ks - 81 840 833 108 94 + 81 840 833 107 94 temple, tx wasilla, AK 55 281 -------------------------------------------------------- @@ -10,7 +10,7 @@ auburn, al 67 14 bozeman, mt 501 339 davis, ca 460 373 - morgantown, wv 93 15 + morgantown, wv 93 14 salina, ks 49 45 temple, tx 34 21 wasilla, AK 100 181 @@ -21,7 +21,7 @@ auburn, al 74 7 bozeman, mt 508 332 davis, ca 472 361 - morgantown, wv 95 13 + morgantown, wv 94 13 salina, ks 52 42 temple, tx 47 8 wasilla, AK 94 187 @@ -35,7 +35,7 @@ AZ 8 4 CA 221 229 CO 67 31 - CT 4 1 + CT 4 0 DE 2 0 FL 19 0 FM 0 2 @@ -94,7 +94,7 @@ AZ 9 3 CA 216 234 CO 73 25 - CT 5 0 + CT 4 0 DE 2 0 FL 19 0 FM 0 2 @@ -153,7 +153,7 @@ AZ 5 7 CA 435 15 CO 81 17 - CT 5 0 + CT 4 0 DE 2 0 FL 14 5 FM 2 0 @@ -212,7 +212,7 @@ AZ 12 0 CA 450 0 CO 93 5 - CT 5 0 + CT 4 0 DE 2 0 FL 19 0 FM 2 0 @@ -271,7 +271,7 @@ AZ 12 0 CA 450 0 CO 91 7 - CT 5 0 + CT 4 0 DE 2 0 FL 17 2 FM 2 0 diff --git a/inst/extdata/OSD/A/AKALURA.json b/inst/extdata/OSD/A/AKALURA.json index efffa31f3b..058e0ead1f 100644 --- a/inst/extdata/OSD/A/AKALURA.json +++ b/inst/extdata/OSD/A/AKALURA.json @@ -26,8 +26,8 @@ "content": "COMPETING SERIES: There are no competing series." }, "GEOGRAPHIC SETTING": { - "section": "GEOGRAPHIC SETTING", - "content": "GEOGRAPHIC SETTING:\nElevation: 350 to 900 meters (1100 to 3000 feet)\nParent material: moderately decomposed herbaceous organic material over sandy and loamy volcanic ash over medial silty volcanic ash over gravelly loamy till\nLandform: mountains, hills, and ridges on flanks, back slopes or toeslopes\nSlope: 15 to 60 percent\nMean annual temperature: 0 to 4 degrees C. (32 to 39 degrees F.)\nMean annual precipitation: 1500 to 3000 mm (59 to 118 in)\nFrost free period: 20 to 50 days\nGEOGRAPHIC SETTING:\nDepth class: very deep\nDrainage class: well drained\nParent material: volcanic ash over gravelly glacial till or colluvium\nLandform: mountain, hills, and ridges\nSlopes: 3 to 75 percent\nMean annual precipitation: 900 to 2000 mm (35 to 79 in)\nMean annual temperature: 0 to 4 degrees C. (32 to 39 degrees F.)\nFrost-free season: 20 to 50 days" + "section": "GEOGRAPHIC SETTING & GEOGRAPHIC SETTING", + "content": "GEOGRAPHIC SETTING:\nElevation: 350 to 900 meters (1100 to 3000 feet)\nParent material: moderately decomposed herbaceous organic material over sandy and loamy volcanic ash over medial silty volcanic ash over gravelly loamy till\nLandform: mountains, hills, and ridges on flanks, back slopes or toeslopes\nSlope: 15 to 60 percent\nMean annual temperature: 0 to 4 degrees C. (32 to 39 degrees F.)\nMean annual precipitation: 1500 to 3000 mm (59 to 118 in)\nFrost free period: 20 to 50 days & GEOGRAPHIC SETTING:\nDepth class: very deep\nDrainage class: well drained\nParent material: volcanic ash over gravelly glacial till or colluvium\nLandform: mountain, hills, and ridges\nSlopes: 3 to 75 percent\nMean annual precipitation: 900 to 2000 mm (35 to 79 in)\nMean annual temperature: 0 to 4 degrees C. (32 to 39 degrees F.)\nFrost-free season: 20 to 50 days" }, "GEOGRAPHICALLY ASSOCIATED SOILS": { "section": "GEOGRAPHICALLY ASSOCIATED SOILS", diff --git a/inst/extdata/OSD/A/ALENEVA.json b/inst/extdata/OSD/A/ALENEVA.json index 551680dfe1..1ff485233e 100644 --- a/inst/extdata/OSD/A/ALENEVA.json +++ b/inst/extdata/OSD/A/ALENEVA.json @@ -26,8 +26,8 @@ "content": "COMPETING SERIES: This is the Terlak (AK) series.\nTerlak soils have spodic properties, have mean annual precipitation less than 775 mm (30 in), and occur on plains with parent material derived from slope alluvium." }, "GEOGRAPHIC SETTING": { - "section": "GEOGRAPHIC SETTING", - "content": "GEOGRAPHIC SETTING:\nElevation: 5 to 400 meters (15 to 1325 feet)\nParent material: moderately decomposed herbaceous organic material over medial silty volcanic ash over sandy and gravelly till\nLandform: hills, plains, in drainageways and swales and on flood plains Slope: 0 to 15 percent\nMean annual temperature: 0 to 6 degrees C. (32 to 43 degrees F.)\nMean annual precipitation: 600 to 2000 mm (24 to 79 in)\nFrost free period: 20 to 50 days\nGEOGRAPHIC SETTING:\nDepth class: very deep\nDrainage class: well drained\nParent material: volcanic ash over coarse-loamy eolian deposits\nLandform: hills and plains\nSlopes: 3 to 15 percent\nMean annual precipitation: 700 to 1500 mm (28 to 59 in)\nMean annual temperature: 0 to 6 degrees C. (32 to 43 degrees F.)\nFrost-free season: 20 to 50 days" + "section": "GEOGRAPHIC SETTING & GEOGRAPHIC SETTING", + "content": "GEOGRAPHIC SETTING:\nElevation: 5 to 400 meters (15 to 1325 feet)\nParent material: moderately decomposed herbaceous organic material over medial silty volcanic ash over sandy and gravelly till\nLandform: hills, plains, in drainageways and swales and on flood plains Slope: 0 to 15 percent\nMean annual temperature: 0 to 6 degrees C. (32 to 43 degrees F.)\nMean annual precipitation: 600 to 2000 mm (24 to 79 in)\nFrost free period: 20 to 50 days & GEOGRAPHIC SETTING:\nDepth class: very deep\nDrainage class: well drained\nParent material: volcanic ash over coarse-loamy eolian deposits\nLandform: hills and plains\nSlopes: 3 to 15 percent\nMean annual precipitation: 700 to 1500 mm (28 to 59 in)\nMean annual temperature: 0 to 6 degrees C. (32 to 43 degrees F.)\nFrost-free season: 20 to 50 days" }, "GEOGRAPHICALLY ASSOCIATED SOILS": { "section": "GEOGRAPHICALLY ASSOCIATED SOILS", diff --git a/inst/extdata/OSD/A/ALMERIA.json b/inst/extdata/OSD/A/ALMERIA.json index 32a1768af0..daab990ca9 100644 --- a/inst/extdata/OSD/A/ALMERIA.json +++ b/inst/extdata/OSD/A/ALMERIA.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic features recognized in this pedon:\nAquic soil conditions: 13 to 203 centimeters (5 to 80 inches) (Cg horizons)\nSoil moisture regime: aquic\nA wet (ponded) phase and a channeled phase are recognized.\nAreas of these soils were mapped as Barney, Loup and Tryon soils in the past.\nAdded frequent flooding and minor correction to location.\n4/24/2000\nModified the format to semitab.\nModified the taxonomy from Sandy, mixed, mesic Typic Fluvaquent\n9/30/02 PFR:" + "content": "REMARKS: Diagnostic features recognized in this pedon:\nAquic soil conditions: 13 to 203 centimeters (5 to 80 inches) (Cg horizons)\nSoil moisture regime: aquic\nA wet (ponded) phase and a channeled phase are recognized.\nAreas of these soils were mapped as Barney, Loup and Tryon soils in the past.\nAdded frequent flooding and minor correction to location.\n4/24/2000\nModified the format to semitab.\nModified the taxonomy from Sandy, mixed, mesic Typic Fluvaquent\n9/30/02 PFR:\ncorrected the family class back to \"sandy\" based on correspondence with Roger Hammer: \"Yes I tend towards Sandy. I just visited with Dave in Valentine and he scanned 23 Almeria 232 descriptions in Cherry Co. Only about 3 out of 23 had loamy (actually fsl) layers above 40 inches. Perhaps the typical pedon needs to be relocated. Also, the loamy layer in the original pedon for the Almeria OSD has 63.5% sand (S85NE115-034). I guess, the location was moved being the one in Loup Co. had a fsl surface which is allowed but maybe not typical for the series.\n5/2002 RRZ: Added loamy sand to ROC of Cg horizon\n12/29/2003 WAW: added mucky loam as texture in A horizon\n1/2006 LRM: metric conversion and changed permeability to saturated hydraulic conductivity" }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/A/ANNAPOLIS.json b/inst/extdata/OSD/A/ANNAPOLIS.json index e132810a18..4f3183cb60 100644 --- a/inst/extdata/OSD/A/ANNAPOLIS.json +++ b/inst/extdata/OSD/A/ANNAPOLIS.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Northern Coastal Plain of Maryland and possibly New Jersey\nExtent: Small\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Northern Coastal Plain of Maryland and possibly New Jersey\nExtent: Small & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES ESTABLISHED", diff --git a/inst/extdata/OSD/A/ANNEMESSEX.json b/inst/extdata/OSD/A/ANNEMESSEX.json index 377dea58a6..6d09ffad31 100644 --- a/inst/extdata/OSD/A/ANNEMESSEX.json +++ b/inst/extdata/OSD/A/ANNEMESSEX.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: MLRAs 153C, 153D, and 149A; the tidewater area of MD and possibly DE\nExtent: The series extent is small, 3,000 to 3,500 acres\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: MLRAs 153C, 153D, and 149A; the tidewater area of MD and possibly DE\nExtent: The series extent is small, 3,000 to 3,500 acres & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES ESTABLISHED", diff --git a/inst/extdata/OSD/A/AQUASCO.json b/inst/extdata/OSD/A/AQUASCO.json index 8466d061fe..2b1cbd75ba 100644 --- a/inst/extdata/OSD/A/AQUASCO.json +++ b/inst/extdata/OSD/A/AQUASCO.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Maryland, possibly Delaware, and New Jersey, MLRA 149A (Northern Coastal Plain).\nExtent: Small, but locally significant.\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Maryland, possibly Delaware, and New Jersey, MLRA 149A (Northern Coastal Plain).\nExtent: Small, but locally significant. & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES ESTABLISHED", diff --git a/inst/extdata/OSD/A/ARAVE.json b/inst/extdata/OSD/A/ARAVE.json index 6dc9ecae01..3c32cfe31d 100644 --- a/inst/extdata/OSD/A/ARAVE.json +++ b/inst/extdata/OSD/A/ARAVE.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nOchric epipedon - The zone from the soil surface to 8 inches (A horizon).\nNatric horizon - The zone from 8 to 18 inches (Btkn1 and Btkn2 horizons).\nCalcic horizon - The zone from 8 to 18 inches (Btkn1 and Btkn2 horizons).\nAquic conditions - The conditions of endosaturation, reduction, and redoximorphic features between 20 and 40 inches at certain times during normal years (parts of the C1 and C2 horizons).\nParticle-size control section - The zone from 8 to 18 inches (Btkn1 and Btkn2 horizons).\nThe revision of October 2005 updated the taxonomic class from Aquic Natrustalfs to Aquic Natrixeralfs based on the assumed moisture regime being xeric instead of ustic." + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nOchric epipedon - The zone from the soil surface to 8 inches (A horizon).\nNatric horizon - The zone from 8 to 18 inches (Btkn1 and Btkn2 horizons).\nCalcic horizon - The zone from 8 to 18 inches (Btkn1 and Btkn2 horizons).\nAquic conditions - The conditions of endosaturation, reduction, and redoximorphic features between 20 and 40 inches at certain times during normal years (parts of the C1 and C2 horizons).\nParticle-size control section - The zone from 8 to 18 inches (Btkn1 and Btkn2 horizons).\nThe revision of October 2005 updated the taxonomic class from Aquic Natrustalfs to Aquic Natrixeralfs based on the assumed moisture regime being xeric instead of ustic.\nThe superactive cation exchange activity class was added in 03/2003 to the taxonomic classification by the National Soil Survey Center on request of the Reno MLRA office, without review of the soil series property data. Later review of laboratory data places the typical pedon in the active class." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/B/BARLOW.json b/inst/extdata/OSD/B/BARLOW.json index d873431fe9..710ef9e3dd 100644 --- a/inst/extdata/OSD/B/BARLOW.json +++ b/inst/extdata/OSD/B/BARLOW.json @@ -14,12 +14,12 @@ "content": "TYPICAL PEDON: Barlow silt loam, forested. (Colors are for moist soil unless otherwise noted.)\nO1--6 to 5 inches; needles, twigs, cones, etc.\nO2--5 inches to 0; very dark gray (10YR 3/1) and very dark brown (10YR 2/2) amorphous organic matter; many roots; abrupt wavy boundary. (3 to 8 inches thick)\nA2--0 to 1 1/2 inches; dark gray (10YR 4/1) silt loam, light gray to gray (10YR 6/1) dry; massive; soft, very friable, nonsticky and nonplastic; many roots; many very fine and fine irregular pores; very strongly acid (pH 4.7); abrupt wavy boundary. (1/2 to 3 inches thick)\nB2ir--1 1/2 to 9 inches; dark yellowish brown (10YR 3/4) silt loam, brown (10YR 5/3) dry and crushed; variegated with brown (7.5YR 4/2 and 4/4 and 10YR 4/3) and dark grayish brown (10YR 4/2); massive; slightly hard, friable, nonsticky and slightly plastic; many roots; many very fine and fine irregular pores; strongly acid (pH 5.1); gradual wavy boundary. (4 to 15 inches thick)\nB3--9 to 20 inches; dark grayish brown (10YR 4/4) stony fine sandy loam, brown (10YR 5/3) dry and crushed; variegated with 20 percent dark brown (7.5YR 3/2); massive; soft, very friable, nonsticky and slightly plastic; 15 percent stones, 10 percent cobbles, and 10 percent pebbles; many roots; many very fine and fine irregular pores; strongly acid (pH 5.4). Many feet thick.\nIIC--20 to 40 inches; dark yellowish brown (10YR 4/4) stony fine sandy loam, brown (10YR 5/3) dry and crushed; variegated with 20 percent dark brown (7.5YR 3/2); massive; soft, very friable, nonsticky and slightly plastic; 15 percent stones, 10 percent cobbles, and 10 percent pebbles; many roots; many very fine and fine irregular pores; strongly acid (pH 5.4). Many feet thick." }, "TYPE LOCATION": { - "section": "TYPE LOCATION", - "content": "TYPE LOCATION: Clackamas County, Oregon; 200 feet west of the Timberline Highway; NE1/4 NE1/4 section 18, T.3S., R.9E. W.M." + "section": "TYPE LOCATION & TYPE LOCATION", + "content": "TYPE LOCATION: Clackamas County, Oregon; 200 feet west of the Timberline Highway; NE1/4 NE1/4 section 18, T.3S., R.9E. W.M. & TYPE LOCATION: Clackamas County, Oregon; 200 feet west of the Timberline Highway; NE1/4 NE1/4 section 18, T.3S., R.9E. W.M." }, "RANGE IN CHARACTERISTICS": { - "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS: The mean annual soil temperature ranges from 40 degrees to 47 degrees F. The average summer soil temperature is less than 47 degrees F. with an 0 horizon. The soils have an udic moisture regime. The driest period is in the summer but the soils are dry for less than 45 consecutive days. Depth to bedrock is 60 inches or more. Depth to stony glacial till ranges from 15 to 30 inches. Thickness of the solum ranges from 15 to 24 inches. The 10- to 40-inch control section has less than an average of 10 percent clay and has 20 to 30 percent sand coarser than very fine sand.\nThe A2 horizon has value of 4 or 5 moist, 6 or 7 dry, and chroma of 1 or 2 moist and dry. It is silt loam or very fine sandy loam.\nThe B2ir horizon has hue of 10YR through 5YR, value of 3 or 4 moist, 5 or 6 dry, and chroma of 2 through 6. The colors are commonly variegated. This horizon is silt loam or very fine sandy loam. It ranges from slightly hard to hard and from friable to firm.\nThe B3 horizon has chroma of 2 or 3 moist and dry. It is silt loam or very fine sandy loam.\nThe IIC horizon has hue of 10YR or 7.5YR, value of 3 or 4 moist and 5 or 6 dry, and chroma of 2 through 4 moist and dry. It is fine sandy loam or sandy loam. It has very friable to firm and soft to hard consistence. Rock fragments range from 20 to 40 percent to depth of 40 inches. Below depth of 40 inches they range from 60 percent in some pedons. Stone size fragments are commonly dominant.\nTYPE LOCATION: Clackamas County, Oregon; 200 feet west of the Timberline Highway; NE1/4 NE1/4 section 18, T.3S., R.9E. W.M.\nRANGE IN CHARACTERISTICS: The mean annual soil temperature ranges from 40 degrees to 47 degrees F. The average summer soil temperature is less than 47 degrees F. with an 0 horizon. The soils have an udic moisture regime. The driest period is in the summer but the soils are dry for less than 45 consecutive days. Depth to bedrock is 60 inches or more. Depth to stony glacial till ranges from 15 to 30 inches. Thickness of the solum ranges from 15 to 24 inches. The 10- to 40-inch control section has less than an average of 10 percent clay and has 20 to 30 percent sand coarser than very fine sand.\nThe A2 horizon has value of 4 or 5 moist, 6 or 7 dry, and chroma of 1 or 2 moist and dry. It is silt loam or very fine sandy loam.\nThe B2ir horizon has hue of 10YR through 5YR, value of 3 or 4 moist, 5 or 6 dry, and chroma of 2 through 6. The colors are commonly variegated. This horizon is silt loam or very fine sandy loam. It ranges from slightly hard to hard and from friable to firm.\nThe B3 horizon has chroma of 2 or 3 moist and dry. It is silt loam or very fine sandy loam.\nThe IIC horizon has hue of 10YR or 7.5YR, value of 3 or 4 moist and 5 or 6 dry, and chroma of 2 through 4 moist and dry. It is fine sandy loam or sandy loam. It has very friable to firm and soft to hard consistence. Rock fragments range from 20 to 40 percent to depth of 40 inches. Below depth of 40 inches they they range from 60 percent in some pedons. Stone size fragments are commonly dominant." + "section": "RANGE IN CHARACTERISTICS & RANGE IN CHARACTERISTICS", + "content": "RANGE IN CHARACTERISTICS: The mean annual soil temperature ranges from 40 degrees to 47 degrees F. The average summer soil temperature is less than 47 degrees F. with an 0 horizon. The soils have an udic moisture regime. The driest period is in the summer but the soils are dry for less than 45 consecutive days. Depth to bedrock is 60 inches or more. Depth to stony glacial till ranges from 15 to 30 inches. Thickness of the solum ranges from 15 to 24 inches. The 10- to 40-inch control section has less than an average of 10 percent clay and has 20 to 30 percent sand coarser than very fine sand.\nThe A2 horizon has value of 4 or 5 moist, 6 or 7 dry, and chroma of 1 or 2 moist and dry. It is silt loam or very fine sandy loam.\nThe B2ir horizon has hue of 10YR through 5YR, value of 3 or 4 moist, 5 or 6 dry, and chroma of 2 through 6. The colors are commonly variegated. This horizon is silt loam or very fine sandy loam. It ranges from slightly hard to hard and from friable to firm.\nThe B3 horizon has chroma of 2 or 3 moist and dry. It is silt loam or very fine sandy loam.\nThe IIC horizon has hue of 10YR or 7.5YR, value of 3 or 4 moist and 5 or 6 dry, and chroma of 2 through 4 moist and dry. It is fine sandy loam or sandy loam. It has very friable to firm and soft to hard consistence. Rock fragments range from 20 to 40 percent to depth of 40 inches. Below depth of 40 inches they range from 60 percent in some pedons. Stone size fragments are commonly dominant. & RANGE IN CHARACTERISTICS: The mean annual soil temperature ranges from 40 degrees to 47 degrees F. The average summer soil temperature is less than 47 degrees F. with an 0 horizon. The soils have an udic moisture regime. The driest period is in the summer but the soils are dry for less than 45 consecutive days. Depth to bedrock is 60 inches or more. Depth to stony glacial till ranges from 15 to 30 inches. Thickness of the solum ranges from 15 to 24 inches. The 10- to 40-inch control section has less than an average of 10 percent clay and has 20 to 30 percent sand coarser than very fine sand.\nThe A2 horizon has value of 4 or 5 moist, 6 or 7 dry, and chroma of 1 or 2 moist and dry. It is silt loam or very fine sandy loam.\nThe B2ir horizon has hue of 10YR through 5YR, value of 3 or 4 moist, 5 or 6 dry, and chroma of 2 through 6. The colors are commonly variegated. This horizon is silt loam or very fine sandy loam. It ranges from slightly hard to hard and from friable to firm.\nThe B3 horizon has chroma of 2 or 3 moist and dry. It is silt loam or very fine sandy loam.\nThe IIC horizon has hue of 10YR or 7.5YR, value of 3 or 4 moist and 5 or 6 dry, and chroma of 2 through 4 moist and dry. It is fine sandy loam or sandy loam. It has very friable to firm and soft to hard consistence. Rock fragments range from 20 to 40 percent to depth of 40 inches. Below depth of 40 inches they they range from 60 percent in some pedons. Stone size fragments are commonly dominant." }, "COMPETING SERIES": { "section": "COMPETING SERIES", diff --git a/inst/extdata/OSD/B/BEEFORK.json b/inst/extdata/OSD/B/BEEFORK.json index 160006aa61..5d1a6cd1f6 100644 --- a/inst/extdata/OSD/B/BEEFORK.json +++ b/inst/extdata/OSD/B/BEEFORK.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nDiagnostic horizons and features recognized in this pedon are:\nHistic epipedon: 0 to 36 centimeters (Oe and Oa horizons).\nMollic epipedon : 36 to 61 centimeters (A horizons).\nBeefork soils have been identified in areas mapped as Batcave, Farewell, Deible, Midco, Raftville, Gabriel, Racoon Freeburg, and a variety of other hydric soil series. Argillic horizons, if present, are considered relict and were formed during a previous period of soil formation." + "content": "REMARKS:\nDiagnostic horizons and features recognized in this pedon are:\nHistic epipedon: 0 to 36 centimeters (Oe and Oa horizons).\nMollic epipedon : 36 to 61 centimeters (A horizons).\nBeefork soils have been identified in areas mapped as Batcave, Farewell, Deible, Midco, Raftville, Gabriel, Racoon Freeburg, and a variety of other hydric soil series. Argillic horizons, if present, are considered relict and were formed during a previous period of soil formation.\nSite and pedon ID 2020M0093101 represents the typical pedon.\nTaxonomy version--Keys to Soil Taxonomy, thirteenth edition, 2022." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/B/BELTSVILLE.json b/inst/extdata/OSD/B/BELTSVILLE.json index d27ef82ce3..995f22b556 100644 --- a/inst/extdata/OSD/B/BELTSVILLE.json +++ b/inst/extdata/OSD/B/BELTSVILLE.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Maryland, Virginia, and Pennsylvania\nExtent: Large\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Maryland, Virginia, and Pennsylvania\nExtent: Large & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES ESTABLISHED", diff --git a/inst/extdata/OSD/B/BLANDBURG.json b/inst/extdata/OSD/B/BLANDBURG.json index 4229cbf56a..030aa1fbdd 100644 --- a/inst/extdata/OSD/B/BLANDBURG.json +++ b/inst/extdata/OSD/B/BLANDBURG.json @@ -10,8 +10,8 @@ "content": "TAXONOMIC CLASS: Loamy-skeletal, siliceous, semiactive, frigid Typic Haplorthods" }, "TYPICAL PEDON": { - "section": "TYPICAL PEDON & The 7/2020 revision moves the Type Location and the Typical Pedon for the series to Potter County, PA from Garrett Co. MD where it was never correlated. It also revises the mineralogy class from mixed to siliceous. The revision of the mineralogy class is based on laboratory data and the classification of soils which have formed in materials weathered from the same parent bedrock; these include Dekalb, Gauley, Hazleton, Leetonia, and Paddyknob soils.", - "content": "TYPICAL PEDON: Blandburg very channery fine sandy loam on a 4 percent convex south-west facing slope in a hardwood forest at an elevation of 722 meters (2,367 feet) (Colors are for moist soil unless otherwise indicated.)\nOi--0 to 5 centimeters (0 to 2 inches); slightly decomposed hardwood leaf litter; 30 percent flat subangular indurated sandstone channers.\nOa--5 to 8 centimeters (2 to 3 inches); highly decomposed hardwood leaf litter; many very fine and fine, and common medium and coarse roots throughout; 30 percent sandstone channers; clear smooth boundary. (Combined thickness of the O horizon is 0 to 15 cm [0 to 6 inches] thick)\nA--8 to 13 centimeters (3 to 5 inches); black (10YR 2/1) very channery fine sandy loam; weak fine granular structure; very friable, slightly sticky, nonplastic; many very fine and fine, and common medium and coarse roots throughout; 35 percent sandstone channers; very strongly acid (pH 4.6); clear wavy boundary. (0 to 15 cm [0 to 6 inches] thick)\nE--13 to 48 centimeters (5 to 19 inches); brown (7.5YR 5/2) extremely channery loamy sand; weak fine subangular blocky structure; very friable, nonsticky, nonplastic; many very fine and fine, and common medium and coarse roots throughout; 10 percent sandstone flagstones, 15 percent sandstone stones, and 40 percent sandstone channers; very strongly acid (pH 4.6); abrupt wavy boundary. (0 to 46 cm [0 to 18 inches] thick)\nBhs--48 to 53 centimeters (19 to 21 inches); dusky red (2.5YR 3/2) extremely channery sandy loam; weak fine and medium subangular blocky structure; friable, slightly sticky, slightly plastic, moderately smeary; many very fine and fine roots throughout; 25 percent continuous faint organoargillans on all faces of peds; 10 percent sandstone flagstones, 15 percent sandstone stones, and 40 percent sandstone channers; very strongly acid (pH 4.6); abrupt irregular boundary.\nBs--53 to 76 centimeters (21 to 30 inches); strong brown (7.5YR 4/6) extremely channery sandy loam; weak medium subangular blocky structure; friable, slightly sticky, nonplastic, weakly smeary; many very fine and fine roots throughout; 10 percent sandstone flagstones, 15 percent sandstone stones, and 40 percent sandstone channers; very strongly acid (pH 4.8); gradual wavy boundary. (Combined thickness of the Bhs and Bh horizons is 5 to 69 cm (2 to 27 inches) thick)\nBC--76 to 112 centimeters (30 to 44 inches); yellowish brown (10YR 5/6) extremely stony sandy loam; weak fine and medium subangular blocky structure; very friable, nonsticky, nonplastic; few very fine roots throughout; 20 percent sandstone flagstones, 20 percent sandstone stones, and 30 percent sandstone channers; very strongly acid (pH 5.0); gradual wavy boundary. (0 to 61 cm (0 to 24 inches) thick)\nC--112 to 163 centimeters (44 to 65 inches); yellowish brown (10YR 5/6) extremely stony sandy loam; loose single grain; very friable, nonsticky, nonplastic; 15 percent sandstone flagstones, 35 percent sandstone stones, and 30 percent sandstone channers; very strongly acid (pH 5.0). & The 7/2020 revision moves the Type Location and the Typical Pedon for the series to Potter County, PA from Garrett Co. MD where it was never correlated. It also revises the mineralogy class from mixed to siliceous. The revision of the mineralogy class is based on laboratory data and the classification of soils which have formed in materials weathered from the same parent bedrock; these include Dekalb, Gauley, Hazleton, Leetonia, and Paddyknob soils.\nPrevious revisions: 1/84--DLY, CER; 12/05-DLY, CER\nThese soils were previously recognized as members of the Hazleton and Leetonia series in areas where soil temperature studies by the Pennsylvania State University and NRCS have shown that the soil temperature class is frigid." + "section": "TYPICAL PEDON", + "content": "TYPICAL PEDON: Blandburg very channery fine sandy loam on a 4 percent convex south-west facing slope in a hardwood forest at an elevation of 722 meters (2,367 feet) (Colors are for moist soil unless otherwise indicated.)\nOi--0 to 5 centimeters (0 to 2 inches); slightly decomposed hardwood leaf litter; 30 percent flat subangular indurated sandstone channers.\nOa--5 to 8 centimeters (2 to 3 inches); highly decomposed hardwood leaf litter; many very fine and fine, and common medium and coarse roots throughout; 30 percent sandstone channers; clear smooth boundary. (Combined thickness of the O horizon is 0 to 15 cm [0 to 6 inches] thick)\nA--8 to 13 centimeters (3 to 5 inches); black (10YR 2/1) very channery fine sandy loam; weak fine granular structure; very friable, slightly sticky, nonplastic; many very fine and fine, and common medium and coarse roots throughout; 35 percent sandstone channers; very strongly acid (pH 4.6); clear wavy boundary. (0 to 15 cm [0 to 6 inches] thick)\nE--13 to 48 centimeters (5 to 19 inches); brown (7.5YR 5/2) extremely channery loamy sand; weak fine subangular blocky structure; very friable, nonsticky, nonplastic; many very fine and fine, and common medium and coarse roots throughout; 10 percent sandstone flagstones, 15 percent sandstone stones, and 40 percent sandstone channers; very strongly acid (pH 4.6); abrupt wavy boundary. (0 to 46 cm [0 to 18 inches] thick)\nBhs--48 to 53 centimeters (19 to 21 inches); dusky red (2.5YR 3/2) extremely channery sandy loam; weak fine and medium subangular blocky structure; friable, slightly sticky, slightly plastic, moderately smeary; many very fine and fine roots throughout; 25 percent continuous faint organoargillans on all faces of peds; 10 percent sandstone flagstones, 15 percent sandstone stones, and 40 percent sandstone channers; very strongly acid (pH 4.6); abrupt irregular boundary.\nBs--53 to 76 centimeters (21 to 30 inches); strong brown (7.5YR 4/6) extremely channery sandy loam; weak medium subangular blocky structure; friable, slightly sticky, nonplastic, weakly smeary; many very fine and fine roots throughout; 10 percent sandstone flagstones, 15 percent sandstone stones, and 40 percent sandstone channers; very strongly acid (pH 4.8); gradual wavy boundary. (Combined thickness of the Bhs and Bh horizons is 5 to 69 cm (2 to 27 inches) thick)\nBC--76 to 112 centimeters (30 to 44 inches); yellowish brown (10YR 5/6) extremely stony sandy loam; weak fine and medium subangular blocky structure; very friable, nonsticky, nonplastic; few very fine roots throughout; 20 percent sandstone flagstones, 20 percent sandstone stones, and 30 percent sandstone channers; very strongly acid (pH 5.0); gradual wavy boundary. (0 to 61 cm (0 to 24 inches) thick)\nC--112 to 163 centimeters (44 to 65 inches); yellowish brown (10YR 5/6) extremely stony sandy loam; loose single grain; very friable, nonsticky, nonplastic; 15 percent sandstone flagstones, 35 percent sandstone stones, and 30 percent sandstone channers; very strongly acid (pH 5.0)." }, "TYPE LOCATION": { "section": "TYPE LOCATION", @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and soil characteristics recognized in this pedon are:\nOchric epipedon--the zone from 0 to 48 cm (Oi, Oa, A and E horizons)\nAlbic horizon--the zone from 13 to 48 cm (E horizon)\nSpodic horizon--the zone from 48 to 76 cm (Bhs and Bs horizons)\nSeries control section--the zone from 0 to 76 cm" + "content": "REMARKS: Diagnostic horizons and soil characteristics recognized in this pedon are:\nOchric epipedon--the zone from 0 to 48 cm (Oi, Oa, A and E horizons)\nAlbic horizon--the zone from 13 to 48 cm (E horizon)\nSpodic horizon--the zone from 48 to 76 cm (Bhs and Bs horizons)\nSeries control section--the zone from 0 to 76 cm\nThe 7/2020 revision moves the Type Location and the Typical Pedon for the series to Potter County, PA from Garrett Co. MD where it was never correlated. It also revises the mineralogy class from mixed to siliceous. The revision of the mineralogy class is based on laboratory data and the classification of soils which have formed in materials weathered from the same parent bedrock; these include Dekalb, Gauley, Hazleton, Leetonia, and Paddyknob soils.\nPrevious revisions: 1/84--DLY, CER; 12/05-DLY, CER\nThese soils were previously recognized as members of the Hazleton and Leetonia series in areas where soil temperature studies by the Pennsylvania State University and NRCS have shown that the soil temperature class is frigid." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", @@ -253,7 +253,7 @@ "eff_class": "NA", "distinctness": "NA", "topography": "NA", - "narrative": "C--112 to 163 centimeters (44 to 65 inches); yellowish brown (10YR 5/6) extremely stony sandy loam; loose single grain; very friable, nonsticky, nonplastic; 15 percent sandstone flagstones, 35 percent sandstone stones, and 30 percent sandstone channers; very strongly acid (pH 5.0). & The 7/2020 revision moves the Type Location and the Typical Pedon for the series to Potter County, PA from Garrett Co. MD where it was never correlated. It also revises the mineralogy class from mixed to siliceous. The revision of the mineralogy class is based on laboratory data and the classification of soils which have formed in materials weathered from the same parent bedrock; these include Dekalb, Gauley, Hazleton, Leetonia, and Paddyknob soils." + "narrative": "C--112 to 163 centimeters (44 to 65 inches); yellowish brown (10YR 5/6) extremely stony sandy loam; loose single grain; very friable, nonsticky, nonplastic; 15 percent sandstone flagstones, 35 percent sandstone stones, and 30 percent sandstone channers; very strongly acid (pH 5.0)." } ] ] diff --git a/inst/extdata/OSD/B/BLOCHER.json b/inst/extdata/OSD/B/BLOCHER.json index f13dca05b4..c032d3145a 100644 --- a/inst/extdata/OSD/B/BLOCHER.json +++ b/inst/extdata/OSD/B/BLOCHER.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: This series crosses both above and below the 15 percent 0.1 to 75 mm fraction size average in the particle-size control section. Additional data indicates this series is dominantly in the fine-silty rather than fine-loamy particle-size class and is revised to the fine-silty class as of 5/2000. The typical pedon averages 13.8 percent in the 0.1 to 75 mm fraction size. Lab data on two other phases average 21 and 23 percent in the 0.1 to 75 mm fraction size.\nHard bedrock substratum, soft bedrock, severely eroded and gullied phases are recognized.\nDiagnostic horizons and features recognized in this pedon are:\nOchric epipedon: the zone from 0 to 15 cm (6 inches) (Ap horizon).\nArgillic horizon: the zone from 15 to 157 cm (6 to 62 inches) (Bt, 2Bt horizons).\nRedoximorphic features: at 43 to 135 cm (17 to 53 inches); clay films with a chroma of 2 or less are iron depleted redoximorphic features." + "content": "REMARKS: This series crosses both above and below the 15 percent 0.1 to 75 mm fraction size average in the particle-size control section. Additional data indicates this series is dominantly in the fine-silty rather than fine-loamy particle-size class and is revised to the fine-silty class as of 5/2000. The typical pedon averages 13.8 percent in the 0.1 to 75 mm fraction size. Lab data on two other phases average 21 and 23 percent in the 0.1 to 75 mm fraction size.\nHard bedrock substratum, soft bedrock, severely eroded and gullied phases are recognized.\nDiagnostic horizons and features recognized in this pedon are:\nOchric epipedon: the zone from 0 to 15 cm (6 inches) (Ap horizon).\nArgillic horizon: the zone from 15 to 157 cm (6 to 62 inches) (Bt, 2Bt horizons).\nRedoximorphic features: at 43 to 135 cm (17 to 53 inches); clay films with a chroma of 2 or less are iron depleted redoximorphic features.\nRepresentative component and horizon data for the Blocher Series is in the following data mapunits: DMU ID 124488 for the typical pedon; DMU ID 124480 for the soft bedrock substratum; and DMU ID 124520 for the hard bedrock substratum." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/B/BUGLEY.json b/inst/extdata/OSD/B/BUGLEY.json index 9064d76c4c..0d57e454c4 100644 --- a/inst/extdata/OSD/B/BUGLEY.json +++ b/inst/extdata/OSD/B/BUGLEY.json @@ -18,8 +18,8 @@ "content": "TYPE LOCATION: Nelson County, Virginia; about 0.4 miles east (88 degrees) of the intersection of Highways VA-56 and VA-646 and 1.5 miles southeast (126 degrees) of the intersection of Highways VA-644 and VA- 626." }, "RANGE IN CHARACTERISTICS": { - "section": "RANGE IN CHARACTERISTICS & RANGE OF INDIVIDUAL HORIZONS", - "content": "RANGE IN CHARACTERISTICS:\nThickness: Solum ranges from 10 to 20 inches. Depth to rock: 10 to 20 inches to hard bedrock. Rock fragments: 15 to 60 percent gravel or channers in A, Ap, and E, 35 to 80 percent in Bw and C horizons. Reaction:..\nRANGE IN CHARACTERISTICS:\nDepth to Bedrock: 10 to 20 inches to hard\nDepth to Seasonal High Water Table: 00 to 00 inches, Month to Month\nRock Fragment content: gravel and channers, 15 to 60 percent, by volume, in the A, Ap, and E horizons, 35 to 80 percent in the Bw and C horizons\nSoil Reaction: Extremely acid through strongly acid, except where limed\nOther Features: Finely divided mica flakes are common to many throughout the soil of most pedons & RANGE OF INDIVIDUAL HORIZONS:\nA horizon (if it occurs):\nColor--hue of 10YR or 2.5Y, value of 3 or 4 , and chroma of 2 through 4\nTexture (fine-earth fraction)-- SIL, L\nAp horizon:\nColor--hue of 7.5YR or 10YR, value of 4 through 6, and chroma of 4 through 6\nTexture (fine-earth fraction)-- SIL, L\nE horizon (if it occurs):\nColor--hue of 7.5YR or 10YR, value of 4 through 6, and chroma of 3 through 6\nTexture (fine-earth fraction)-- SIL, L\nBw horizon:\nColor--hue of 5YR through 10YR, value of 4 through 6, and chroma of 4 through 8\nTexture (fine-earth fraction)-- SIL, SICL, or CL\nC horizon, where present, has hue of 5YR through 10YR, value of 4 through 8, chroma of 1 through 8.. Texture is L, SIL, SICL, or CL saprolite in the\nC horizon (if it occurs):\nColor--hue of 5YR through 10YR, value of 4 through 8, and chroma of 1 through 8; colors often variegated, chroma of 1 or 2 are inherited from the bedrock\nTexture (fine-earth fraction)-L, SIL, SICL, or CL\nCr layer:\nColor--hue of 5YR through 10YR, value of 4 through 8, and chroma of 1 through 8; colors often variegated\nTexture (fine-earth fraction)-L, SIL, SICL, or CL" + "section": "RANGE IN CHARACTERISTICS & RANGE IN CHARACTERISTICS & RANGE OF INDIVIDUAL HORIZONS", + "content": "RANGE IN CHARACTERISTICS:\nThickness: Solum ranges from 10 to 20 inches. Depth to rock: 10 to 20 inches to hard bedrock. Rock fragments: 15 to 60 percent gravel or channers in A, Ap, and E, 35 to 80 percent in Bw and C horizons. Reaction:.. & RANGE IN CHARACTERISTICS:\nDepth to Bedrock: 10 to 20 inches to hard\nDepth to Seasonal High Water Table: 00 to 00 inches, Month to Month\nRock Fragment content: gravel and channers, 15 to 60 percent, by volume, in the A, Ap, and E horizons, 35 to 80 percent in the Bw and C horizons\nSoil Reaction: Extremely acid through strongly acid, except where limed\nOther Features: Finely divided mica flakes are common to many throughout the soil of most pedons & RANGE OF INDIVIDUAL HORIZONS:\nA horizon (if it occurs):\nColor--hue of 10YR or 2.5Y, value of 3 or 4 , and chroma of 2 through 4\nTexture (fine-earth fraction)-- SIL, L\nAp horizon:\nColor--hue of 7.5YR or 10YR, value of 4 through 6, and chroma of 4 through 6\nTexture (fine-earth fraction)-- SIL, L\nE horizon (if it occurs):\nColor--hue of 7.5YR or 10YR, value of 4 through 6, and chroma of 3 through 6\nTexture (fine-earth fraction)-- SIL, L\nBw horizon:\nColor--hue of 5YR through 10YR, value of 4 through 6, and chroma of 4 through 8\nTexture (fine-earth fraction)-- SIL, SICL, or CL\nC horizon, where present, has hue of 5YR through 10YR, value of 4 through 8, chroma of 1 through 8.. Texture is L, SIL, SICL, or CL saprolite in the\nC horizon (if it occurs):\nColor--hue of 5YR through 10YR, value of 4 through 8, and chroma of 1 through 8; colors often variegated, chroma of 1 or 2 are inherited from the bedrock\nTexture (fine-earth fraction)-L, SIL, SICL, or CL\nCr layer:\nColor--hue of 5YR through 10YR, value of 4 through 8, and chroma of 1 through 8; colors often variegated\nTexture (fine-earth fraction)-L, SIL, SICL, or CL" }, "COMPETING SERIES": { "section": "COMPETING SERIES", diff --git a/inst/extdata/OSD/B/BURTON.json b/inst/extdata/OSD/B/BURTON.json index ac18a7f666..b0e01e06b6 100644 --- a/inst/extdata/OSD/B/BURTON.json +++ b/inst/extdata/OSD/B/BURTON.json @@ -55,11 +55,11 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: This series was formerly classified as an acid Brown Forest soil. Burton series was initially placed in a mesic family. Soil temperature data has been collected in North Carolina in several counties and supports the frigid family.\nThe 1/97 revision placed Burton soils in a fine-loamy particle-size class. This series was formerly placed in a coarse-loamy particle-size class. Laboratory PSA (pipette method) and corresponding field texture estimates (feel method) indicate control section clay contents of generally 12 to 24 percent, with most pedons marginally coarse-loamy. Fine-loamy particle-size class placement is based on the presence of amorphous (non-crystalline) clay-size material associated with the relatively high organic matter content found in these soils. Although field estimates, laboratory measurements, and calculated values may vary, clay content in the particle-size control section is generally less than 25 percent. Although Burton soils may exhibit some of the characteristics of andic soil properties, they lack the volcanic glass found in soils of similar taxa in the Western United States." + "content": "REMARKS: This series was formerly classified as an acid Brown Forest soil. Burton series was initially placed in a mesic family. Soil temperature data has been collected in North Carolina in several counties and supports the frigid family.\nThe 1/97 revision placed Burton soils in a fine-loamy particle-size class. This series was formerly placed in a coarse-loamy particle-size class. Laboratory PSA (pipette method) and corresponding field texture estimates (feel method) indicate control section clay contents of generally 12 to 24 percent, with most pedons marginally coarse-loamy. Fine-loamy particle-size class placement is based on the presence of amorphous (non-crystalline) clay-size material associated with the relatively high organic matter content found in these soils. Although field estimates, laboratory measurements, and calculated values may vary, clay content in the particle-size control section is generally less than 25 percent. Although Burton soils may exhibit some of the characteristics of andic soil properties, they lack the volcanic glass found in soils of similar taxa in the Western United States.\nThe 3/03 revision reflects the movement of the typical pedon from Transylvania County, NC to Buncombe County, NC." }, "ADDITIONAL DATA": { - "section": "ADDITIONAL DATA", - "content": "ADDITIONAL DATA: Characterization data are available from the NSSC Soil Survey Laboratory, Lincoln, NE for this pedon: S91NC-021-008.\nDiagnostic horizons and features recognized in this pedon are:\nUmbric epipedon - the zone from the mineral soil surface to a depth of 17 inches (A1 and A2 horizons)\nCambic horizon - the zone between 17 and 26 inches (Bw horizon)\nParalithic contact - weathered bedrock contact at 26 inches (upper boundary of Cr horizon).\nLithic contact - the occurrence of hard bedrock at a depth of 29 inches (R horizon)\nIsotic mineralogy class - In more than one-half of the control section, a 1500 kPa water to clay ratio of 0.6 or more and a pH in NaF solution of more than 8.4.\nADDITIONAL DATA: Characterization data is available from the National Soil Survey Laboratory, Lincoln, NE for the following pedons: S88NC-199-017, S91NC-021-007, and S91NC-021-008.\nMLRA: 130B SIR(S): NC0093, NC0114 (STONY)\nRevised: 10/92-HJB,DLN,AG; 1/97-DHK, 12/97-DHK, 3/03-MHS, MKC\n02/11-BPS: Taxonomic Classification -- 11th Keys, update competing and associated series, MLRA clarification" + "section": "ADDITIONAL DATA & ADDITIONAL DATA", + "content": "ADDITIONAL DATA: Characterization data are available from the NSSC Soil Survey Laboratory, Lincoln, NE for this pedon: S91NC-021-008.\nDiagnostic horizons and features recognized in this pedon are:\nUmbric epipedon - the zone from the mineral soil surface to a depth of 17 inches (A1 and A2 horizons)\nCambic horizon - the zone between 17 and 26 inches (Bw horizon)\nParalithic contact - weathered bedrock contact at 26 inches (upper boundary of Cr horizon).\nLithic contact - the occurrence of hard bedrock at a depth of 29 inches (R horizon)\nIsotic mineralogy class - In more than one-half of the control section, a 1500 kPa water to clay ratio of 0.6 or more and a pH in NaF solution of more than 8.4.\nADDITIONAL DATA: Characterization data is available from the National Soil Survey Laboratory, Lincoln, NE for the following pedons: S88NC-199-017, S91NC-021-007, and S91NC-021-008.\nMLRA: 130B SIR(S): NC0093, NC0114 (STONY)\nRevised: 10/92-HJB,DLN,AG; 1/97-DHK, 12/97-DHK, 3/03-MHS, MKC\n02/11-BPS: Taxonomic Classification -- 11th Keys, update competing and associated series, MLRA clarification & ADDITIONAL DATA: Characterization data is available from the National Soil Survey Laboratory, Lincoln, NE for the following pedons: S88NC-199-017, S91NC-021-007, and S91NC-021-008.\nMLRA: 130B SIR(S): NC0093, NC0114 (STONY)\nRevised: 10/92-HJB,DLN,AG; 1/97-DHK, 12/97-DHK, 3/03-MHS, MKC\n02/11-BPS: Taxonomic Classification -- 11th Keys, update competing and associated series, MLRA clarification" }, "SITE": [ [ diff --git a/inst/extdata/OSD/C/CATEACHE.json b/inst/extdata/OSD/C/CATEACHE.json index 2e65271098..555d02d304 100644 --- a/inst/extdata/OSD/C/CATEACHE.json +++ b/inst/extdata/OSD/C/CATEACHE.json @@ -10,8 +10,8 @@ "content": "TAXONOMIC CLASS: Fine-loamy, mixed, active, mesic Ultic Hapludalfs" }, "TYPICAL PEDON": { - "section": "TYPICAL PEDON & The 04/2010 revision moves the Type Location and the Typical Pedon from Pocahontas County, WV to Summers County, WV based on analysis of lab data collected in 2003. The OSD format is changed and metric units are added. The range of fine-earth textures for the Bt, BC, and C horizons is expanded to include SIC.", - "content": "TYPICAL PEDON: Cateache channery silt loam on a south-facing, convex 74 percent slope in a forested area. (Colors are for moist soil.)\nA--0 to 9 cm (0 to 3 inches); dark brown (7.5YR 3/2) channery silt loam; weak fine and medium granular structure; very friable; common very fine roots to very coarse roots throughout; 2 percent extremely firm siltstone flagstones and 20 percent extremely firm siltstone channers; very strongly acid; pH 4.8; clear wavy boundary. (3 to 13 cm thick)\nBt1--9 to 21 cm (3 to 8 inches); reddish brown (5YR 4/3) very channery silty clay loam; weak fine and medium subangular blocky structure; friable; common very fine to very coarse roots throughout; 4 percent faint clay films on all faces of peds; 2 percent extremely firm siltstone flagstones and 36 percent extremely firm siltstone channers; very strongly acid, pH 4.9; clear wavy boundary.\nBt2--21 to 53 cm (8 to 21 inches); dark reddish brown (5YR 3/3) channery silty clay loam; moderate fine and medium subangular blocky structure; firm; common very fine to medium roots throughout; 10 percent faint clay films on all faces of peds; 2 percent extremely firm siltstone flagstones and 30 percent extremely firm siltstone channers; strongly acid, pH 5.1; clear wavy boundary.\nBt3--53 to 75 cm (21 to 29 inches); dark reddish brown (2.5YR 3/4) silty clay loam; moderate medium subangular blocky structure; friable; common fine roots throughout; 30 percent distinct clay films on all faces of peds; 10 percent extremely firm siltstone channers; moderately acid, pH 5.7; gradual wavy boundary.\nBt4--75 to 92 cm (29 to 36 inches); dark reddish brown (2.5YR 3/4) channery silty clay; moderate fine and medium subangular blocky structure; friable; common fine roots throughout; 20 percent faint clay films on all faces of peds; 10 percent extremely firm siltstone flagstones and 11 percent extremely firm siltstone channers; moderately acid, pH 5.8; abrupt broken boundary.(Combined thickness of the Bt horizon is 30 to 89 cm)\nCr--92 cm (36 inches); extremely firm; dark reddish brown (2.5YR 3/3) highly weathered and fractured siltstone; moderately strongly cemented; moderate excavation difficulty. & The 04/2010 revision moves the Type Location and the Typical Pedon from Pocahontas County, WV to Summers County, WV based on analysis of lab data collected in 2003. The OSD format is changed and metric units are added. The range of fine-earth textures for the Bt, BC, and C horizons is expanded to include SIC.\nPrevious revisions: DGF-ART 06/2001" + "section": "TYPICAL PEDON", + "content": "TYPICAL PEDON: Cateache channery silt loam on a south-facing, convex 74 percent slope in a forested area. (Colors are for moist soil.)\nA--0 to 9 cm (0 to 3 inches); dark brown (7.5YR 3/2) channery silt loam; weak fine and medium granular structure; very friable; common very fine roots to very coarse roots throughout; 2 percent extremely firm siltstone flagstones and 20 percent extremely firm siltstone channers; very strongly acid; pH 4.8; clear wavy boundary. (3 to 13 cm thick)\nBt1--9 to 21 cm (3 to 8 inches); reddish brown (5YR 4/3) very channery silty clay loam; weak fine and medium subangular blocky structure; friable; common very fine to very coarse roots throughout; 4 percent faint clay films on all faces of peds; 2 percent extremely firm siltstone flagstones and 36 percent extremely firm siltstone channers; very strongly acid, pH 4.9; clear wavy boundary.\nBt2--21 to 53 cm (8 to 21 inches); dark reddish brown (5YR 3/3) channery silty clay loam; moderate fine and medium subangular blocky structure; firm; common very fine to medium roots throughout; 10 percent faint clay films on all faces of peds; 2 percent extremely firm siltstone flagstones and 30 percent extremely firm siltstone channers; strongly acid, pH 5.1; clear wavy boundary.\nBt3--53 to 75 cm (21 to 29 inches); dark reddish brown (2.5YR 3/4) silty clay loam; moderate medium subangular blocky structure; friable; common fine roots throughout; 30 percent distinct clay films on all faces of peds; 10 percent extremely firm siltstone channers; moderately acid, pH 5.7; gradual wavy boundary.\nBt4--75 to 92 cm (29 to 36 inches); dark reddish brown (2.5YR 3/4) channery silty clay; moderate fine and medium subangular blocky structure; friable; common fine roots throughout; 20 percent faint clay films on all faces of peds; 10 percent extremely firm siltstone flagstones and 11 percent extremely firm siltstone channers; moderately acid, pH 5.8; abrupt broken boundary.(Combined thickness of the Bt horizon is 30 to 89 cm)\nCr--92 cm (36 inches); extremely firm; dark reddish brown (2.5YR 3/3) highly weathered and fractured siltstone; moderately strongly cemented; moderate excavation difficulty." }, "TYPE LOCATION": { "section": "TYPE LOCATION", @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Cateache soils were previously mapped as members of the Teas series (inactive) or as a high base substratum phase of the Calvin series.\nDiagnostic horizons and soil characteristics recognized in this pedon are:\nOchric epipedon--the zone from 0 to 9 cm (A horizon)\nArgillic horizon--the zone from 9 to 92 cm (Bt horizons)\nOther soil features identified with this pedon:\nBase saturation (by sum of cations)--58 percent at paralithic contact (92 cm).\nSeries control section--the zone from 0 to 117 cm" + "content": "REMARKS: Cateache soils were previously mapped as members of the Teas series (inactive) or as a high base substratum phase of the Calvin series.\nDiagnostic horizons and soil characteristics recognized in this pedon are:\nOchric epipedon--the zone from 0 to 9 cm (A horizon)\nArgillic horizon--the zone from 9 to 92 cm (Bt horizons)\nOther soil features identified with this pedon:\nBase saturation (by sum of cations)--58 percent at paralithic contact (92 cm).\nSeries control section--the zone from 0 to 117 cm\nThe 04/2010 revision moves the Type Location and the Typical Pedon from Pocahontas County, WV to Summers County, WV based on analysis of lab data collected in 2003. The OSD format is changed and metric units are added. The range of fine-earth textures for the Bt, BC, and C horizons is expanded to include SIC.\nPrevious revisions: DGF-ART 06/2001" }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", @@ -207,7 +207,7 @@ "eff_class": "NA", "distinctness": "NA", "topography": "NA", - "narrative": "Cr--92 cm (36 inches); extremely firm; dark reddish brown (2.5YR 3/3) highly weathered and fractured siltstone; moderately strongly cemented; moderate excavation difficulty. & The 04/2010 revision moves the Type Location and the Typical Pedon from Pocahontas County, WV to Summers County, WV based on analysis of lab data collected in 2003. The OSD format is changed and metric units are added. The range of fine-earth textures for the Bt, BC, and C horizons is expanded to include SIC." + "narrative": "Cr--92 cm (36 inches); extremely firm; dark reddish brown (2.5YR 3/3) highly weathered and fractured siltstone; moderately strongly cemented; moderate excavation difficulty." } ] ] diff --git a/inst/extdata/OSD/C/CEDARFALLS.json b/inst/extdata/OSD/C/CEDARFALLS.json index eb2ac6072f..10264b7a2a 100644 --- a/inst/extdata/OSD/C/CEDARFALLS.json +++ b/inst/extdata/OSD/C/CEDARFALLS.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are: ochric epipedon - the zone from a depth of about 1 to 6 inches (A horizon); lithic contact - at a depth of about 58 inches." + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are: ochric epipedon - the zone from a depth of about 1 to 6 inches (A horizon); lithic contact - at a depth of about 58 inches.\n02/2022 revision: Oi had 1 to 0 inch depths, corrected to be 0 to 1 in horizon depths then added 1 inches to all horizon depths throughout the typical pedon. WJN" }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/C/CHEOAH.json b/inst/extdata/OSD/C/CHEOAH.json index 5e8db3052f..8c99e375aa 100644 --- a/inst/extdata/OSD/C/CHEOAH.json +++ b/inst/extdata/OSD/C/CHEOAH.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: This series was formerly included with the Burton and Porters series. However, Burton is frigid and has bedrock within a depth of 20 to 40 inches. Both formed in residuum weathered from felsic to mafic, igneous and high-grade metamorphic rocks such as granite, hornblende gneiss, and mica gneiss and contain fragments of those rocks.\nThe 1/97 revision placed Cheoah soils in a fine-loamy particle-size class. This series was formerly placed in a coarse-loamy particle-size class. Laboratory PSA (pipette method) and corresponding field texture estimates (feel method) indicate control section clay contents of generally 12 to 24 percent, with most pedons marginally coarse-loamy. Fine-loamy particle-size class placement is based on the presence of amorphous (non-crystalline) clay-size material associated with the relatively high organic matter content found in these soils. Although field estimates, laboratory measurements, and calculated values may vary, clay content in the particle-size control section is generally less than 25 percent. Although Cheoah soils may exhibit some of the characteristics of andic soil properties, they lack the volcanic glass found in soils of similar taxa in the Western United States." + "content": "REMARKS: This series was formerly included with the Burton and Porters series. However, Burton is frigid and has bedrock within a depth of 20 to 40 inches. Both formed in residuum weathered from felsic to mafic, igneous and high-grade metamorphic rocks such as granite, hornblende gneiss, and mica gneiss and contain fragments of those rocks.\nThe 1/97 revision placed Cheoah soils in a fine-loamy particle-size class. This series was formerly placed in a coarse-loamy particle-size class. Laboratory PSA (pipette method) and corresponding field texture estimates (feel method) indicate control section clay contents of generally 12 to 24 percent, with most pedons marginally coarse-loamy. Fine-loamy particle-size class placement is based on the presence of amorphous (non-crystalline) clay-size material associated with the relatively high organic matter content found in these soils. Although field estimates, laboratory measurements, and calculated values may vary, clay content in the particle-size control section is generally less than 25 percent. Although Cheoah soils may exhibit some of the characteristics of andic soil properties, they lack the volcanic glass found in soils of similar taxa in the Western United States.\nThe 10/07 revision reflects the movement of the typical pedon from Graham County, NC to Jackson County, NC.\nRevised 02/11-BPS: Taxonomic Classification -- 11th Keys" }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/C/CHILI.json b/inst/extdata/OSD/C/CHILI.json index cc4974c6e7..6112fcb6ba 100644 --- a/inst/extdata/OSD/C/CHILI.json +++ b/inst/extdata/OSD/C/CHILI.json @@ -54,8 +54,8 @@ "content": "SERIES ESTABLISHED: Huron County, Ohio, 1950." }, "REMARKS": { - "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon\nare:\n1. Ochric epipedon - 0 to 36 centimeters (Ap, BE horizons)\n2. Argillic horizon - 36 to 89 centimeters (Bt1, Bt2 horizons)\nA loamy substratum phase has been recognized. These soils will need to be evaluated during MLRA update activities.\nLatitude and Longitude cannot be accurately located from distance on TYPE LOCATION.\nREMARKS: Refer to pedons CA-33, CO-42, CO-53, CO-60, CO-79, CO-131, CO-132, CO-137, LK-18, MH-50, SK-8, ST-18, ST-B4, and TU-16 for characterization data analyzed by the Ohio State University Soil Characterization Laboratory, Columbus, Ohio." + "section": "REMARKS & REMARKS", + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon\nare:\n1. Ochric epipedon - 0 to 36 centimeters (Ap, BE horizons)\n2. Argillic horizon - 36 to 89 centimeters (Bt1, Bt2 horizons)\nA loamy substratum phase has been recognized. These soils will need to be evaluated during MLRA update activities.\nLatitude and Longitude cannot be accurately located from distance on TYPE LOCATION. & REMARKS: Refer to pedons CA-33, CO-42, CO-53, CO-60, CO-79, CO-131, CO-132, CO-137, LK-18, MH-50, SK-8, ST-18, ST-B4, and TU-16 for characterization data analyzed by the Ohio State University Soil Characterization Laboratory, Columbus, Ohio." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/C/CHRISTIANA.json b/inst/extdata/OSD/C/CHRISTIANA.json index 99edb2b88a..36af241254 100644 --- a/inst/extdata/OSD/C/CHRISTIANA.json +++ b/inst/extdata/OSD/C/CHRISTIANA.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Maryland, Delaware, District of Columbia, and possibly northern Virginia\nExtent: Moderate, but locally important\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Maryland, Delaware, District of Columbia, and possibly northern Virginia\nExtent: Moderate, but locally important & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES ESTABLISHED", diff --git a/inst/extdata/OSD/C/CIERVO.json b/inst/extdata/OSD/C/CIERVO.json index 788cfce61b..c0b4eea240 100644 --- a/inst/extdata/OSD/C/CIERVO.json +++ b/inst/extdata/OSD/C/CIERVO.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Previously mapped as Oxalis and Panoche series in the Soil Survey of the Mendota Area, California, Series 1940, No. 18 and in the Soil Survey of the Coalinga Area, California, Series 1944, No 1.\nClay texture is the dominant surface texture of this soil and texture which was determined in the field, therefore clay texture was described in the Ap1 horizon. The laboratory data showed 39.3 percent clay. This soil occurs in an area which is subject to dramatic changes in soil salinity and sodicity due to position on the landscape (fan skirts) and the prevalence of perched water tables near the surface.\nMajor Diagnostic Horizons:\nThe Ciervo series was initially classified as Vertic Torriorthents. This was changed to Vertic Haplocambids when a cambic horizon was described in the Ciervo profiles. The presence of a cambic horizon is based on the following characteristics:\n1. Soil structure in the cambic horizon (unless moist from irrigation or rainfall or drastically modified by deep ripping).\n2. Removal of carbonates or gypsum from the cambic horizon.\n3. Accumulation of carbonates or gypsum below the cambic horizon which supports loss of carbonate or gypsum from overlying horizons.\n4. Higher chroma in the cambic horizon in some pedons.\n5. Most areas of Ciervo soil are irrigated with 2 to 3 feet of water per year applied for crop production. Previous to irrigation, only about 7 inches of precipitation, coupled with flood water, was available for soil development. Movement of carbonates, gypsum, fertilizers, and salt through the soil profile has created more pronounced cambic horizons because of application of irrigation water.\n1. Ochric Epipedon--0 to 17 inches (Ap1, Ap2).\n1.1 Cambic Horizon -- 17 to 27 inches (Bw).\n1.2 Removal of carbonates or gypsum from the cambic horizon. Pedons which have a horizon with 5 percent gypsum qualify for a gypsic horizon. They are not classified as gypsic horizons however, because 5 percent gypsum is the minimum requirement for a gypsic horizon and 5 percent gypsum is the maximum gypsum found in the Ciervo series. In all instances where gypsum content is as high as 5 percent, there have been significant amounts of gypsum that have been added as a soil amendment.\n1.3 Zone of redistribution -- 27 to 60 inches (Bknyz, Bknz).\nOther Diagnostic Features and Characteristics:\n1. Fine Family" + "content": "REMARKS: Previously mapped as Oxalis and Panoche series in the Soil Survey of the Mendota Area, California, Series 1940, No. 18 and in the Soil Survey of the Coalinga Area, California, Series 1944, No 1.\nClay texture is the dominant surface texture of this soil and texture which was determined in the field, therefore clay texture was described in the Ap1 horizon. The laboratory data showed 39.3 percent clay. This soil occurs in an area which is subject to dramatic changes in soil salinity and sodicity due to position on the landscape (fan skirts) and the prevalence of perched water tables near the surface.\nMajor Diagnostic Horizons:\nThe Ciervo series was initially classified as Vertic Torriorthents. This was changed to Vertic Haplocambids when a cambic horizon was described in the Ciervo profiles. The presence of a cambic horizon is based on the following characteristics:\n1. Soil structure in the cambic horizon (unless moist from irrigation or rainfall or drastically modified by deep ripping).\n2. Removal of carbonates or gypsum from the cambic horizon.\n3. Accumulation of carbonates or gypsum below the cambic horizon which supports loss of carbonate or gypsum from overlying horizons.\n4. Higher chroma in the cambic horizon in some pedons.\n5. Most areas of Ciervo soil are irrigated with 2 to 3 feet of water per year applied for crop production. Previous to irrigation, only about 7 inches of precipitation, coupled with flood water, was available for soil development. Movement of carbonates, gypsum, fertilizers, and salt through the soil profile has created more pronounced cambic horizons because of application of irrigation water.\n1. Ochric Epipedon--0 to 17 inches (Ap1, Ap2).\n1.1 Cambic Horizon -- 17 to 27 inches (Bw).\n1.2 Removal of carbonates or gypsum from the cambic horizon. Pedons which have a horizon with 5 percent gypsum qualify for a gypsic horizon. They are not classified as gypsic horizons however, because 5 percent gypsum is the minimum requirement for a gypsic horizon and 5 percent gypsum is the maximum gypsum found in the Ciervo series. In all instances where gypsum content is as high as 5 percent, there have been significant amounts of gypsum that have been added as a soil amendment.\n1.3 Zone of redistribution -- 27 to 60 inches (Bknyz, Bknz).\nOther Diagnostic Features and Characteristics:\n1. Fine Family\n1.1 NSSL results show 34 to 47 percent clay in the typical pedon. There is an average 45 percent clay from 10 to 40 inches.\n2. Smectitic Mineralogy\n2.1 X-ray diffraction studies show smectite is the dominant clay mineral in this soil.\n3. Thermic Temperature Regime\n3.1 Soil temperature regime is assumed to be thermic based upon data from Mendota Dam and Panoche Junction. MAAT is 62 to 64 degrees F.\n4. Vertic Subgroup\n4.1 Linear extensibility percent is 8for the typical pedon to a depth of 104 cm.\n4.2 Since this soil is cultivated and irrigated, cracks are difficult to observe. If unirrigated, cracks are assumed to be at least 5 mm wide at a depth of 50 cm, at least 30 cm long in some part, and extend upward to the soil surface or the base of an Ap horizon.\n5. Torric Moisture Regime\n5.1 Unless irrigated, the 4 to 12 inch SMCS is assumed to be dry in all parts from April 1 to December 1 and is moist in some or all parts for only 70 to 90 consecutive days. Based upon data from Mendota Dam (MAP 7.7 inches) and Panoche Junction (MAP 6.0 inches) climate stations.\n5.2 The soil temperature exceeds 47 degrees F. from January to December (365 days)." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/C/CLIME.json b/inst/extdata/OSD/C/CLIME.json index 755fbc4788..bf81b86809 100644 --- a/inst/extdata/OSD/C/CLIME.json +++ b/inst/extdata/OSD/C/CLIME.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nDiagnostic horizons and features recognized in this pedon are:\nParticle-size control section: The zone from 25 to 84 centimeters (10 to 33 inches) (Bw and C horizons)\nMollic epipedon: the zone from 0 to 46 centimeters (0 to 18 inches) (A and Bw horizon).\nParalithic contact: the contact at 84 centimeters (33 inches) (Cr horizon)\nKeys to Taxonomy: Twelfth Edition, 2014.\n07/2003 WAW Change to semi-tabular format, changed runoff from rapid to very high. Updated cation exchange activity class to active based on laboratory data collected near the type location." + "content": "REMARKS:\nDiagnostic horizons and features recognized in this pedon are:\nParticle-size control section: The zone from 25 to 84 centimeters (10 to 33 inches) (Bw and C horizons)\nMollic epipedon: the zone from 0 to 46 centimeters (0 to 18 inches) (A and Bw horizon).\nParalithic contact: the contact at 84 centimeters (33 inches) (Cr horizon)\nKeys to Taxonomy: Twelfth Edition, 2014.\n07/2003 WAW Change to semi-tabular format, changed runoff from rapid to very high. Updated cation exchange activity class to active based on laboratory data collected near the type location.\n01/2012 JLG Up-dated to meet MO5 Soil Technical Note-1 (Revision 4); conversion from English to metric; added the following: longitude and latitude to typical pedon, particle-size control section, sand and clay ranges, calcium carbonate equivalent based on lab data, mean annual soil temperature and soil moisture in characteristics, elevation, precipitation patterns, frost-free days, saturated hydraulic conductivity, Land Resource Region, Taxonomic Version, a couple of diagnostic features, lab samples under additional data, and soil moisture. Broaden range of mean annual precipitation; Removed Thornthwaites Annual PE Index.\n6/2020 BKN updated some tabular RIC data. Changed Keys to Taxonomy version to Twelfth Edition." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/C/COLEMANTOWN.json b/inst/extdata/OSD/C/COLEMANTOWN.json index f84b50a507..a619d5fcc2 100644 --- a/inst/extdata/OSD/C/COLEMANTOWN.json +++ b/inst/extdata/OSD/C/COLEMANTOWN.json @@ -6,8 +6,8 @@ "STATES": "MD,NJ", "OVERVIEW": "NA", "TAXONOMIC CLASS": { - "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Fine, glauconitic, mesic Typic Albaquults\nDepth Class: Very deep\nDrainage Class (Agricultural): Poorly drained\nSaturated Hydraulic Conductivity Class: Moderately low or low\nLandscape: Northern Atlantic Coastal Plain\nParent Material: Glauconite bearing fluviomarine deposits\nSlope: 0 to 2 percent\nMean Annual Air Temperature (type location): 13 degrees C. (56 degrees F.)\nMean Annual Precipitation (type location): 1143 mm (45 inches)\nTAXONOMIC CLASS: Fine, glauconitic, mesic Typic Albaquults" + "section": "TAXONOMIC CLASS & TAXONOMIC CLASS", + "content": "TAXONOMIC CLASS: Fine, glauconitic, mesic Typic Albaquults\nDepth Class: Very deep\nDrainage Class (Agricultural): Poorly drained\nSaturated Hydraulic Conductivity Class: Moderately low or low\nLandscape: Northern Atlantic Coastal Plain\nParent Material: Glauconite bearing fluviomarine deposits\nSlope: 0 to 2 percent\nMean Annual Air Temperature (type location): 13 degrees C. (56 degrees F.)\nMean Annual Precipitation (type location): 1143 mm (45 inches) & TAXONOMIC CLASS: Fine, glauconitic, mesic Typic Albaquults" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", @@ -43,11 +43,11 @@ }, "DISTRIBUTION AND EXTENT": { "section": "DISTRIBUTION AND EXTENT", - "content": "DISTRIBUTION AND EXTENT:\nDistribution: The Northern Atlantic Coastal Plain of Maryland and New Jersey\nExtent: Small\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "content": "DISTRIBUTION AND EXTENT:\nDistribution: The Northern Atlantic Coastal Plain of Maryland and New Jersey\nExtent: Small" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nMajor Uses: Most areas have been cleared and used for crop production. The most common are hay, pasture, turf, corn, and soybeans.\nVegetation: Wooded areas are dominantly sweetgum, red maple, white oak, American holly, and yellow-poplar." + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nMajor Uses: Most areas have been cleared and used for crop production. The most common are hay, pasture, turf, corn, and soybeans.\nVegetation: Wooded areas are dominantly sweetgum, red maple, white oak, American holly, and yellow-poplar. & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES ESTABLISHED", diff --git a/inst/extdata/OSD/C/CRAGGEY.json b/inst/extdata/OSD/C/CRAGGEY.json index b51ab29651..21a2a0d665 100644 --- a/inst/extdata/OSD/C/CRAGGEY.json +++ b/inst/extdata/OSD/C/CRAGGEY.json @@ -58,8 +58,8 @@ "content": "REMARKS: Craggey soils were formerly mapped in the Cleveland and Porters series and in miscellaneous stony land units. These soils would have been classified in the Lithosol great soil group. Craggey series was initially placed in a mesic soil temperature class. Soil temperature data collected in North Carolina support placement of this series in the frigid soil temperature class. Although Craggey soils may exhibit some of the characteristics of andic soil properties, they lack the volcanic glass found in soils of similar taxa in the Western United States." }, "ADDITIONAL DATA": { - "section": "ADDITIONAL DATA", - "content": "ADDITIONAL DATA: Characterization data are available from the NSSC Soil Survey Laboratory, Lincoln, NE for this pedon: S91NC-021-009.\nDiagnostic horizons and features recognized in this pedon are:\nUmbric epipedon - the zone from the mineral soil surface to a depth of 14 inches (A1 and A2 horizons)\nLithic contact - the occurrence of hard bedrock at a depth of 14 inches (R horizon)\nIsotic mineralogy class - In more than one-half of the control section, a 1500 kPa water to clay ratio of 0.6 or more and a pH in NaF solution of more than 8.4.\nADDITIONAL DATA:\nNASIS Data Map Unit ID: NASIS data for the typical pedon in Buncombe County, NC are represented by DMU ID # 368632.\nMLRA: 130B SIR: NC0117, NC0232 (Organic Surface)\nRevised: 3/03-MSH,MKC\n02/11-BPS: Taxonomic Classification -- 11th Keys, update competing and associated series, MLRA clarification" + "section": "ADDITIONAL DATA & ADDITIONAL DATA", + "content": "ADDITIONAL DATA: Characterization data are available from the NSSC Soil Survey Laboratory, Lincoln, NE for this pedon: S91NC-021-009.\nDiagnostic horizons and features recognized in this pedon are:\nUmbric epipedon - the zone from the mineral soil surface to a depth of 14 inches (A1 and A2 horizons)\nLithic contact - the occurrence of hard bedrock at a depth of 14 inches (R horizon)\nIsotic mineralogy class - In more than one-half of the control section, a 1500 kPa water to clay ratio of 0.6 or more and a pH in NaF solution of more than 8.4.\nADDITIONAL DATA:\nNASIS Data Map Unit ID: NASIS data for the typical pedon in Buncombe County, NC are represented by DMU ID # 368632.\nMLRA: 130B SIR: NC0117, NC0232 (Organic Surface)\nRevised: 3/03-MSH,MKC\n02/11-BPS: Taxonomic Classification -- 11th Keys, update competing and associated series, MLRA clarification & ADDITIONAL DATA:\nNASIS Data Map Unit ID: NASIS data for the typical pedon in Buncombe County, NC are represented by DMU ID # 368632.\nMLRA: 130B SIR: NC0117, NC0232 (Organic Surface)\nRevised: 3/03-MSH,MKC\n02/11-BPS: Taxonomic Classification -- 11th Keys, update competing and associated series, MLRA clarification" }, "SITE": [ [ diff --git a/inst/extdata/OSD/C/CRANFILL.json b/inst/extdata/OSD/C/CRANFILL.json index b6a60490e7..a7d5cdc6ac 100644 --- a/inst/extdata/OSD/C/CRANFILL.json +++ b/inst/extdata/OSD/C/CRANFILL.json @@ -10,12 +10,12 @@ "content": "TAXONOMIC CLASS: Fine-loamy, carbonatic, thermic Udic Haplustepts" }, "TYPICAL PEDON": { - "section": "TYPICAL PEDON & Typical pedon of Cranfill gravelly clay loam, 3 to 5 percent slopes; from the intersection of Texas Highway 6 and Texas Highway 22 in Meridian, 6.3 miles south on Texas Highway 6; 600 feet west in a native grass pasture. USGS topographic quadrangle: Clifton, TX:", - "content": "TYPICAL PEDON: Cranfill gravelly clay loam--rangeland. (Colors are for dry soil unless otherwise stated.)\nA--0 to 25 cm(0 to 10 in); grayish brown (10YR 5/2) gravelly clay loam, dark grayish brown (10YR 4/2) moist; moderate fine granular structure; hard, friable; few fine pores; common fine roots; common films, threads, and concretions of calcium carbonate; 20 percent by volume of limestone fragments from 2 mm to 2.5 cm in diameter; about 80 percent calcium carbonate equivalent; violently effervescent; moderately alkaline, gradual smooth boundary. (Thickness is 20 to 38 cm [8 to 15 in])\nBk1--25 to 56 cm(10 to 22 in); very pale brown (10YR 7/4) gravelly clay loam, light yellowish brown (10YR 6/4) moist; moderate medium granular and weak medium subangular blocky structure; hard, friable; few fine roots; few fine pores; many films, threads, and concretions of calcium carbonate; 26 percent by volume of limestone fragments from 2 mm to 4 cm in diameter; about 90 percent calcium carbonate equivalent; violently effervescent; moderately alkaline; gradual smooth boundary. (Thickness is 25 to 58 cm [10 to 23 in])\nBk2--56 to 137 cm(22 to 54 in); light yellowish brown (10YR 6/4) gravelly clay loam, yellowish brown (10YR 5/4) moist; moderate medium granular and moderate medium subangular blocky structure; hard, friable; few fine roots; few fine pores; many films, threads, and concretions of calcium carbonate; 31 percent by volume of limestone fragments from 2 mm to 4 cm in diameter; about 90 percent calcium carbonate equivalent; violently effervescent; moderately alkaline; gradual smooth boundary. (Thickness is 56 to 86 cm [22 to 34 in])\nBCk--137 to 203 cm (54 to 80 in); very pale brown (10YR 7/4) gravelly clay loam, light yellowish brown (10YR 6/4) moist; weak fine subangular blocky structure; hard, friable; many films, threads, and concretions of calcium carbonate; 20 percent by volume of limestone fragments from 2 mm to 4 cm in diameter; about 90 percent calcium carbonate equivalent; violently effervescent; moderately alkaline. & Typical pedon of Cranfill gravelly clay loam, 3 to 5 percent slopes; from the intersection of Texas Highway 6 and Texas Highway 22 in Meridian, 6.3 miles south on Texas Highway 6; 600 feet west in a native grass pasture. USGS topographic quadrangle: Clifton, TX:\nLatitude: 31 degrees, 50 minutes, 32.62 seconds, N;\nLongitude: 97 degrees, 37 minutes, 22.67 seconds, W;\nDatum: WGS84.\nUTM Easting 630164.65 m, UTM Northing 3523790.98m; UTM Zone 14." + "section": "TYPICAL PEDON", + "content": "TYPICAL PEDON: Cranfill gravelly clay loam--rangeland. (Colors are for dry soil unless otherwise stated.)\nA--0 to 25 cm(0 to 10 in); grayish brown (10YR 5/2) gravelly clay loam, dark grayish brown (10YR 4/2) moist; moderate fine granular structure; hard, friable; few fine pores; common fine roots; common films, threads, and concretions of calcium carbonate; 20 percent by volume of limestone fragments from 2 mm to 2.5 cm in diameter; about 80 percent calcium carbonate equivalent; violently effervescent; moderately alkaline, gradual smooth boundary. (Thickness is 20 to 38 cm [8 to 15 in])\nBk1--25 to 56 cm(10 to 22 in); very pale brown (10YR 7/4) gravelly clay loam, light yellowish brown (10YR 6/4) moist; moderate medium granular and weak medium subangular blocky structure; hard, friable; few fine roots; few fine pores; many films, threads, and concretions of calcium carbonate; 26 percent by volume of limestone fragments from 2 mm to 4 cm in diameter; about 90 percent calcium carbonate equivalent; violently effervescent; moderately alkaline; gradual smooth boundary. (Thickness is 25 to 58 cm [10 to 23 in])\nBk2--56 to 137 cm(22 to 54 in); light yellowish brown (10YR 6/4) gravelly clay loam, yellowish brown (10YR 5/4) moist; moderate medium granular and moderate medium subangular blocky structure; hard, friable; few fine roots; few fine pores; many films, threads, and concretions of calcium carbonate; 31 percent by volume of limestone fragments from 2 mm to 4 cm in diameter; about 90 percent calcium carbonate equivalent; violently effervescent; moderately alkaline; gradual smooth boundary. (Thickness is 56 to 86 cm [22 to 34 in])\nBCk--137 to 203 cm (54 to 80 in); very pale brown (10YR 7/4) gravelly clay loam, light yellowish brown (10YR 6/4) moist; weak fine subangular blocky structure; hard, friable; many films, threads, and concretions of calcium carbonate; 20 percent by volume of limestone fragments from 2 mm to 4 cm in diameter; about 90 percent calcium carbonate equivalent; violently effervescent; moderately alkaline." }, "TYPE LOCATION": { "section": "TYPE LOCATION", - "content": "TYPE LOCATION: Bosque County, Texas;" + "content": "TYPE LOCATION: Bosque County, Texas;\nTypical pedon of Cranfill gravelly clay loam, 3 to 5 percent slopes; from the intersection of Texas Highway 6 and Texas Highway 22 in Meridian, 6.3 miles south on Texas Highway 6; 600 feet west in a native grass pasture. USGS topographic quadrangle: Clifton, TX:\nLatitude: 31 degrees, 50 minutes, 32.62 seconds, N;\nLongitude: 97 degrees, 37 minutes, 22.67 seconds, W;\nDatum: WGS84.\nUTM Easting 630164.65 m, UTM Northing 3523790.98m; UTM Zone 14." }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", @@ -161,7 +161,7 @@ "eff_class": "violently effervescent", "distinctness": "NA", "topography": "NA", - "narrative": "BCk--137 to 203 cm (54 to 80 in); very pale brown (10YR 7/4) gravelly clay loam, light yellowish brown (10YR 6/4) moist; weak fine subangular blocky structure; hard, friable; many films, threads, and concretions of calcium carbonate; 20 percent by volume of limestone fragments from 2 mm to 4 cm in diameter; about 90 percent calcium carbonate equivalent; violently effervescent; moderately alkaline. & Typical pedon of Cranfill gravelly clay loam, 3 to 5 percent slopes; from the intersection of Texas Highway 6 and Texas Highway 22 in Meridian, 6.3 miles south on Texas Highway 6; 600 feet west in a native grass pasture. USGS topographic quadrangle: Clifton, TX:" + "narrative": "BCk--137 to 203 cm (54 to 80 in); very pale brown (10YR 7/4) gravelly clay loam, light yellowish brown (10YR 6/4) moist; weak fine subangular blocky structure; hard, friable; many films, threads, and concretions of calcium carbonate; 20 percent by volume of limestone fragments from 2 mm to 4 cm in diameter; about 90 percent calcium carbonate equivalent; violently effervescent; moderately alkaline." } ] ] diff --git a/inst/extdata/OSD/C/CUMBERSTONE.json b/inst/extdata/OSD/C/CUMBERSTONE.json index 1212109a1e..25c866bbdc 100644 --- a/inst/extdata/OSD/C/CUMBERSTONE.json +++ b/inst/extdata/OSD/C/CUMBERSTONE.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Quaternary Talbot formation; terraces along the Chesapeake Bay, Maryland\nExtent: Small\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Quaternary Talbot formation; terraces along the Chesapeake Bay, Maryland\nExtent: Small & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES ESTABLISHED", diff --git a/inst/extdata/OSD/D/DEALE.json b/inst/extdata/OSD/D/DEALE.json index 48ad983ef4..c91a72a35d 100644 --- a/inst/extdata/OSD/D/DEALE.json +++ b/inst/extdata/OSD/D/DEALE.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Quaternary Talbot formation in the Coastal Plain of Maryland\nExtent: Small\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Quaternary Talbot formation in the Coastal Plain of Maryland\nExtent: Small & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES ESTABLISHED", diff --git a/inst/extdata/OSD/D/DERROC.json b/inst/extdata/OSD/D/DERROC.json index bb2b70dd84..d5721e722d 100644 --- a/inst/extdata/OSD/D/DERROC.json +++ b/inst/extdata/OSD/D/DERROC.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\n1. Ochric epipedon - the zone from 3 to 6 inches. (the A horizon)\n2. Cambic horizon - the zone from 6 to 40 inches. (Bw horizon)\n3. Fluventic feature - irregular decrease in organic-carbon content.\n4. Udic moisture regime.\nSoils now within the range of the Derroc series were correlated Craigsville in several published soil surveys." + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\n1. Ochric epipedon - the zone from 3 to 6 inches. (the A horizon)\n2. Cambic horizon - the zone from 6 to 40 inches. (Bw horizon)\n3. Fluventic feature - irregular decrease in organic-carbon content.\n4. Udic moisture regime.\nSoils now within the range of the Derroc series were correlated Craigsville in several published soil surveys.\n02/2022 revision: Oi had 3 to 0 inch depths, corrected to be 0 to 3 in horizon depths then added 3 inches to all horizon depths throughout the typical pedon. WJN" }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/E/ELLSWORTH.json b/inst/extdata/OSD/E/ELLSWORTH.json index 1df5e591ac..543a891c6b 100644 --- a/inst/extdata/OSD/E/ELLSWORTH.json +++ b/inst/extdata/OSD/E/ELLSWORTH.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon include:\n1. Ochric epipedon - the zone from 0 to 28 cm (0 to 11 inches) (Ap, BE)\n2. Argillic horizon - the zone from 28 to 94 cm (11 to 37 inches) (Bt1, Bt2, Bt3)\n3. Aquic conditions - the upper limit of a seasonal high water table is at 28 cm (11 inches) (Bt horizon)." + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon include:\n1. Ochric epipedon - the zone from 0 to 28 cm (0 to 11 inches) (Ap, BE)\n2. Argillic horizon - the zone from 28 to 94 cm (11 to 37 inches) (Bt1, Bt2, Bt3)\n3. Aquic conditions - the upper limit of a seasonal high water table is at 28 cm (11 inches) (Bt horizon).\nThe typical pedon appears to have a densic contact described. This feature will need to be properly evaluated during future MLRA projects. These projects are identified in NASIS.\nThe sandstone and shale substratum bedrock phases will need to be evaluated during future MLRA project activities." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/F/FILLMORE.json b/inst/extdata/OSD/F/FILLMORE.json index 96d86e3362..c5ae223866 100644 --- a/inst/extdata/OSD/F/FILLMORE.json +++ b/inst/extdata/OSD/F/FILLMORE.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nMollic epipedon: The zone from 0 to 81 centimeters (0 to 32 inches) (A, E, Bt1, Bt2 horizons)\nAlbic horizon: The zone from 23 to 33 centimeters (9 to 13 inches) (E horizon)\nArgillic horizon:--The zone from 33 to 81 centimeters (13 to 32 inches) (Bt1, Bt2 horizons).\nVertic features: The presence of linear Extensibility of 6.0 cm or more between 0 and 100 cm (0 to 40 inches). This was determined from lab data for Fillmore and similar soils.\nTerrace phases are recognized that have sand or coarse textured material below the loess cap at a depth of 3 to 10 meters (10 to 30 ft.).\nA poorly drained, ponded phase is also recognized that has interpretations similar to the Scott series.\nOSD Modification 6/2002RRZ\nDark shot as described the E horizons of Fillmore soil is questionable as a natural occurring event. This observation is probably due to tillage or drainage operations, which have destroyed or mixed some of the E horizon with Bt material containing the (shot-like) material. Possibly some freeze/thaw activities could move the concretions into the contact zone of the lower Bt horizon. The silty clay loam surface layer is due to farming or landscaping activities. Under natural conditions the surface layer is silt loam. Added redox information; added Sturges to competing series.\n10/17/05 JCR\nChanged format to semi-tab. Changed permeability to saturated hydraulic conductivity\n12/2011 DJK\nChanged mean annual precipitation from 23 inches to 27 inches.\nAdded in elevation for typical pedon.\nAdded quadrangle and latitude/longitude to type location.\nAdded mollic thickness and depth to argillic in RIC. Added in clay content and sand content for each horizon in RIC. For E horizon added value of 6 to moist color. For Bt horizon deleted 5Y an N from hue, added silty clay loam, deleted clay, and changed clay percent. BC horizon added silty clay.\nUnder geomorphic setting, added in closed depressions for landform and deleted stream terraces, entered in elevation range and frost-free days, and updated precipitation and temperature.\nUnder geographically associated soils, deleted Belfore, Holder, Holdrege, and Tomek and updated other soils.\nUnder Drainage and Kst, deleted runoff, changed flooding to ponding, added in ponding and saturation statement, and changed Ksat from very low to low. Added soybeans in for crops.\nAdded LRRs and MLRAs to distribution and extent, and change to large extent." + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nMollic epipedon: The zone from 0 to 81 centimeters (0 to 32 inches) (A, E, Bt1, Bt2 horizons)\nAlbic horizon: The zone from 23 to 33 centimeters (9 to 13 inches) (E horizon)\nArgillic horizon:--The zone from 33 to 81 centimeters (13 to 32 inches) (Bt1, Bt2 horizons).\nVertic features: The presence of linear Extensibility of 6.0 cm or more between 0 and 100 cm (0 to 40 inches). This was determined from lab data for Fillmore and similar soils.\nTerrace phases are recognized that have sand or coarse textured material below the loess cap at a depth of 3 to 10 meters (10 to 30 ft.).\nA poorly drained, ponded phase is also recognized that has interpretations similar to the Scott series.\nOSD Modification 6/2002RRZ\nDark shot as described the E horizons of Fillmore soil is questionable as a natural occurring event. This observation is probably due to tillage or drainage operations, which have destroyed or mixed some of the E horizon with Bt material containing the (shot-like) material. Possibly some freeze/thaw activities could move the concretions into the contact zone of the lower Bt horizon. The silty clay loam surface layer is due to farming or landscaping activities. Under natural conditions the surface layer is silt loam. Added redox information; added Sturges to competing series.\n10/17/05 JCR\nChanged format to semi-tab. Changed permeability to saturated hydraulic conductivity\n12/2011 DJK\nChanged mean annual precipitation from 23 inches to 27 inches.\nAdded in elevation for typical pedon.\nAdded quadrangle and latitude/longitude to type location.\nAdded mollic thickness and depth to argillic in RIC. Added in clay content and sand content for each horizon in RIC. For E horizon added value of 6 to moist color. For Bt horizon deleted 5Y an N from hue, added silty clay loam, deleted clay, and changed clay percent. BC horizon added silty clay.\nUnder geomorphic setting, added in closed depressions for landform and deleted stream terraces, entered in elevation range and frost-free days, and updated precipitation and temperature.\nUnder geographically associated soils, deleted Belfore, Holder, Holdrege, and Tomek and updated other soils.\nUnder Drainage and Kst, deleted runoff, changed flooding to ponding, added in ponding and saturation statement, and changed Ksat from very low to low. Added soybeans in for crops.\nAdded LRRs and MLRAs to distribution and extent, and change to large extent.\nAdded in additional data showing NSSL characterization pedons and typical pedon.\n8/2012 DJK Added mean annual soil temperature and horizons where have redox to RIC. Lowered the sand content in PSCS and the Bt horizon from 3 to 2 percent. Removed moderately acid from reaction for the Bt horizon. Removed moderately alkaline from reaction for the BC horizon. Added CCE to the BC and C horizons in RIC and added statement on now being Bk horizons . Added precipitation pattern to geographic setting. Updated competing series. Removed Hastings from geographically associated soils. Removed statement about changing classification to match Filbert, Massie, and Scott from remarks." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/F/FLATWOODS.json b/inst/extdata/OSD/F/FLATWOODS.json index de228541ea..15092902a5 100644 --- a/inst/extdata/OSD/F/FLATWOODS.json +++ b/inst/extdata/OSD/F/FLATWOODS.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Flatwoods soils have been included in the Needmore series in the past. Diagnostic horizons and features recognized in this pedon are:\na. Ochric epipedon - the zone from 3 to 9 inches (A and E horizons).\nb. Argillic horizon - the zone from 9 to 35 inches (Bt and BC horizons).\nc. Aquic feature - mottles of chroma 2 or less at 20 inches (Bt3 horizon).\nd. lithic contact ? at 35 inches (top of R horizon)\nThe 12/2005 revision updates this soil to the 9th Edition of the Keys to Soil Taxonomy (2003). The CEC activity class placement is based on similar soils and not on laboratory data. Class placement may be revised in the future when laboratory data are reviewed or become available.\nCompeting series, pedon description (including horizon nomenclature redoximorphic features and/or descriptive terms), and other sections on the OSD were not revised.\nPrevious revision dates: 10/90" + "content": "REMARKS: Flatwoods soils have been included in the Needmore series in the past. Diagnostic horizons and features recognized in this pedon are:\na. Ochric epipedon - the zone from 3 to 9 inches (A and E horizons).\nb. Argillic horizon - the zone from 9 to 35 inches (Bt and BC horizons).\nc. Aquic feature - mottles of chroma 2 or less at 20 inches (Bt3 horizon).\nd. lithic contact ? at 35 inches (top of R horizon)\nThe 12/2005 revision updates this soil to the 9th Edition of the Keys to Soil Taxonomy (2003). The CEC activity class placement is based on similar soils and not on laboratory data. Class placement may be revised in the future when laboratory data are reviewed or become available.\nCompeting series, pedon description (including horizon nomenclature redoximorphic features and/or descriptive terms), and other sections on the OSD were not revised.\nPrevious revision dates: 10/90\n03/2022 revision: Oi had 3 to 1 inch depths and Oe had 1 to 0 inch depths, corrected to be 0 to 2 inch horizon depths and 2 to 3 inch horizon depths then add 2 inches to all horizon depths throughout the typical pedon. WJN" }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/F/FLORENCE.json b/inst/extdata/OSD/F/FLORENCE.json index 24ed9a2449..1a16e05338 100644 --- a/inst/extdata/OSD/F/FLORENCE.json +++ b/inst/extdata/OSD/F/FLORENCE.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizon and features recognized in this pedon are:\nMollic epipedon: the zone from 0 to 38 centimeters (0 to 15 inches) (A1, A2, & BA horizons)\nArgillic horizon: the zone from 38 to 112 centimeters (15 to 44 inches) (Bt horizon)\nLithic contact: cherty limestone at 112 centimeters (44 inches) (R horizon)\n07/2012 JLG converted English measurements to metric; Updated introduction paragraph, geographical setting, geographically associated soils, and Drainage and Saturated Hydraulic Conductivity; Added quadrangle to type location; Added soil moisture, mean annual soil temperature, particle size control sections, and clay & sand percentages to range of characteristics, and Land Resource Region and MLRA to distribution and extent.\n07/2003 WAW changed to semi-tabular format, updated terminology for runoff and reaction classes." + "content": "REMARKS: Diagnostic horizon and features recognized in this pedon are:\nMollic epipedon: the zone from 0 to 38 centimeters (0 to 15 inches) (A1, A2, & BA horizons)\nArgillic horizon: the zone from 38 to 112 centimeters (15 to 44 inches) (Bt horizon)\nLithic contact: cherty limestone at 112 centimeters (44 inches) (R horizon)\n07/2012 JLG converted English measurements to metric; Updated introduction paragraph, geographical setting, geographically associated soils, and Drainage and Saturated Hydraulic Conductivity; Added quadrangle to type location; Added soil moisture, mean annual soil temperature, particle size control sections, and clay & sand percentages to range of characteristics, and Land Resource Region and MLRA to distribution and extent.\n07/2003 WAW changed to semi-tabular format, updated terminology for runoff and reaction classes.\n06/2020 BKN Added site information to typical pedon and type location headings. Added soil temperature regime, soil moisture regime, and rock fragment percent to RIC.\nKeys to Soil Taxonomy: Twelfth Edition, 2014." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/F/FORT_MOTT.json b/inst/extdata/OSD/F/FORT_MOTT.json index ba5edfbd44..30b62a679b 100644 --- a/inst/extdata/OSD/F/FORT_MOTT.json +++ b/inst/extdata/OSD/F/FORT_MOTT.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution--The Coastal Plain of New Jersey, Delaware, and Maryland.\nExtent--Moderate\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution--The Coastal Plain of New Jersey, Delaware, and Maryland.\nExtent--Moderate & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES ESTABLISHED", diff --git a/inst/extdata/OSD/G/GEARY.json b/inst/extdata/OSD/G/GEARY.json index e2b4f2a7f1..2237360350 100644 --- a/inst/extdata/OSD/G/GEARY.json +++ b/inst/extdata/OSD/G/GEARY.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nMollic epipedon: the zone from 0 to 38 centimeters (0 to 15 inches). (Ap and BA horizons).\nArgillic horizon: the zone from 38 to 81 centimeters (15 to 32 inches). (Bt1 and Bt2 horizons).\nMoisture regime: Ustic\n07/2003 WAW Changed to semi-tabular format, update runoff and reaction terminology, added additional data.\n10/17/05 JCR Added metric to the description." + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nMollic epipedon: the zone from 0 to 38 centimeters (0 to 15 inches). (Ap and BA horizons).\nArgillic horizon: the zone from 38 to 81 centimeters (15 to 32 inches). (Bt1 and Bt2 horizons).\nMoisture regime: Ustic\n07/2003 WAW Changed to semi-tabular format, update runoff and reaction terminology, added additional data.\n10/17/05 JCR Added metric to the description.\n08/2012 DJK Added hillslopes for landform in introduction and geographic setting. Changed MAP from 26 inches to 30 inches. Added elevation to typical pedon. Added quad and lat/long to type location. Added depth to argillic and PSCS weighted averages to RIC. Added soil moisture and temperature statement to RIC. Added ranges for BA and BC in RIC. Added clay and sand content for the other horizons. Added CCE for the BC and C horizons. Changed Avans competing series reason. Under geographic setting, added elevation, dropped the upper MAAT from 58 degrees F to 57, changed MAP from 23 to 31 inches to 26 to 33 inches, and added in frost-free period. Removed Hastings and Wells from geographically associated soils. Under Drainage and Saturated Hydraulic Conductivity, changed runoff to include low and changed Ksat from moderately low to moderately high. Added LRR and MLRA to Distribution and Extent. Added KSSL characterization pedons that have been sampled to additional data." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/G/GOESSEL.json b/inst/extdata/OSD/G/GOESSEL.json index 3c09b3a113..e7b0fba5a0 100644 --- a/inst/extdata/OSD/G/GOESSEL.json +++ b/inst/extdata/OSD/G/GOESSEL.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nDiagnostic horizons and features recognized in this profile are:\nParticle-size control section: The zone from 25 to 100 centimeters (20 to 40 inches). (A, Bss, BC1, and BC2 horizons)\nMollic epipedon: The zone from 0 to 64 centimeters (0 to 25 inches). (Ap, A, and Bss horizons)\nRedoximorphic features: In the zone from 64 to 200 centimeters (25 to 80 inches). (BC1, BC2, 2C1, and 2C2 horizons)\nVertic features: The presence of slickensides at 36 to 64 centimeters (14 to 25 inches). (Bss horizon)\nLithologic discontinuity: At the upper boundary of the 2C horizon.\nGilgai features have been observed in areas of Goessel soils in native pasture.\nKeys to Taxonomy: Eleventh Edition, 2010.\nUpdated the classification, competing series and placed in semitab format. LRM 03/01\nJLG 1/2012 Updated to meet MO 5 Soil Technical Note-1 (Revision 3);" + "content": "REMARKS:\nDiagnostic horizons and features recognized in this profile are:\nParticle-size control section: The zone from 25 to 100 centimeters (20 to 40 inches). (A, Bss, BC1, and BC2 horizons)\nMollic epipedon: The zone from 0 to 64 centimeters (0 to 25 inches). (Ap, A, and Bss horizons)\nRedoximorphic features: In the zone from 64 to 200 centimeters (25 to 80 inches). (BC1, BC2, 2C1, and 2C2 horizons)\nVertic features: The presence of slickensides at 36 to 64 centimeters (14 to 25 inches). (Bss horizon)\nLithologic discontinuity: At the upper boundary of the 2C horizon.\nGilgai features have been observed in areas of Goessel soils in native pasture.\nKeys to Taxonomy: Eleventh Edition, 2010.\nUpdated the classification, competing series and placed in semitab format. LRM 03/01\nJLG 1/2012 Updated to meet MO 5 Soil Technical Note-1 (Revision 3);\nConversion from English to metric; added the following: longitude and latitude and clay and sand percents to typical pedon, particle-size control section, sand and clay ranges in characteristics, elevation, saturated hydraulic conductivity, Land Resource Region, Major Land Resource Area, Taxonomic Version, precipitation pattern, a couple of diagnostic features, soil moisture, and additional data; divided out upper and lower AC horizons based on lab data for typical pedon.\nDJK 05/2014 Revisited and redescribed the type location with new horizonation (Bss, BC, 2C). Updated RIC for new horizonation including redox, EC, gypsum, rock fragments in 2C, and reaction. Changed classification to Udic Haplusterts. Updated competing series for new classification. Changed parent material to clayey alluvium over loamy alluvium. Changed landform to paleoterrace on river valley based on visiting type location and examining maps and data of area Goessel is mapped. Edited climate data. Added saturation statement to Drainage and Ksat section. Edited diagnostic horizons and features in remarks section for new description. Added gilgai statement. Added KSSL data to additional data section." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/G/GREENSON.json b/inst/extdata/OSD/G/GREENSON.json index 386c298125..b40f355e0d 100644 --- a/inst/extdata/OSD/G/GREENSON.json +++ b/inst/extdata/OSD/G/GREENSON.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nMollic epipedon - The zone from the soil surface to 16 inches (Ap and A horizons).\nCambic horizon - The zone from 16 to 23 inches (Bw horizon).\nCalcic horizon - The zone from 23 to 51 inches (Bk1 and Bk2 horizons).\nEndosaturation feature - The condition of ground water with an upper boundary between 30 and 60 inches at certain times during normal years (parts of the Bk1, Bk2, and C horizons).\nParticle-size control section - The zone from 10 to 40 inches (Bw and Bk1 horizons and parts of the A and Bk2 horizons).\nThis revision of February 2006 updates the taxonomic class from Fine-silty, mixed, superactive, mesic Aquic Calciustolls based on depth to aquic conditions deeper than 30 inches and the assumed moisture regime being xeric instead of ustic." + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nMollic epipedon - The zone from the soil surface to 16 inches (Ap and A horizons).\nCambic horizon - The zone from 16 to 23 inches (Bw horizon).\nCalcic horizon - The zone from 23 to 51 inches (Bk1 and Bk2 horizons).\nEndosaturation feature - The condition of ground water with an upper boundary between 30 and 60 inches at certain times during normal years (parts of the Bk1, Bk2, and C horizons).\nParticle-size control section - The zone from 10 to 40 inches (Bw and Bk1 horizons and parts of the A and Bk2 horizons).\nThis revision of February 2006 updates the taxonomic class from Fine-silty, mixed, superactive, mesic Aquic Calciustolls based on depth to aquic conditions deeper than 30 inches and the assumed moisture regime being xeric instead of ustic.\nThe superactive cation exchange activity class was added in 03/2003 to the taxonomic classification by the National Soil Survey Center on request of the Reno MLRA office, without review of the soil series property data. Laboratory data of the typical pedon verifies the activity class." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/G/GREENWICH.json b/inst/extdata/OSD/G/GREENWICH.json index bbd7743e8f..979db0ba1e 100644 --- a/inst/extdata/OSD/G/GREENWICH.json +++ b/inst/extdata/OSD/G/GREENWICH.json @@ -6,8 +6,8 @@ "STATES": "DE", "OVERVIEW": "NA", "TAXONOMIC CLASS": { - "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Coarse-loamy, mixed, semiactive, mesic Typic Hapludults\nDepth class: Very deep\nDrainage class (Agricultural): Well drained\nSaturated Hydraulic Conductivity: Moderately high in the upper subsoil and high or very high in the lower subsoil and substratum\nLandscape: Coastal plain\nParent material: Loamy eolian and alluvial deposits high in silt underlain by loamy and sandy alluvial sediments\nSlope: 0 to 5 percent\nMean Annual Air Temperature (type location): 13 degrees C. (55 degrees F.)\nMean Annual Precipitation (type location): 1118 mm (44 inches)\nTAXONOMIC CLASS: Coarse-loamy, mixed, semiactive, mesic Typic Hapludults" + "section": "TAXONOMIC CLASS & TAXONOMIC CLASS", + "content": "TAXONOMIC CLASS: Coarse-loamy, mixed, semiactive, mesic Typic Hapludults\nDepth class: Very deep\nDrainage class (Agricultural): Well drained\nSaturated Hydraulic Conductivity: Moderately high in the upper subsoil and high or very high in the lower subsoil and substratum\nLandscape: Coastal plain\nParent material: Loamy eolian and alluvial deposits high in silt underlain by loamy and sandy alluvial sediments\nSlope: 0 to 5 percent\nMean Annual Air Temperature (type location): 13 degrees C. (55 degrees F.)\nMean Annual Precipitation (type location): 1118 mm (44 inches) & TAXONOMIC CLASS: Coarse-loamy, mixed, semiactive, mesic Typic Hapludults" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", @@ -43,11 +43,11 @@ }, "DISTRIBUTION AND EXTENT": { "section": "DISTRIBUTION AND EXTENT", - "content": "DISTRIBUTION AND EXTENT: Southeastern Delaware, Maryland and possibly New Jersey. The extent is small.\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "content": "DISTRIBUTION AND EXTENT: Southeastern Delaware, Maryland and possibly New Jersey. The extent is small." }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES ESTABLISHED", diff --git a/inst/extdata/OSD/G/GRIST_MILL.json b/inst/extdata/OSD/G/GRIST_MILL.json index 1ff1586383..5f37973bae 100644 --- a/inst/extdata/OSD/G/GRIST_MILL.json +++ b/inst/extdata/OSD/G/GRIST_MILL.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Virginia\nExtent: Small\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Virginia\nExtent: Small & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES PROPOSED", diff --git a/inst/extdata/OSD/G/GRITNEY.json b/inst/extdata/OSD/G/GRITNEY.json index 132ec012b7..86d281001d 100644 --- a/inst/extdata/OSD/G/GRITNEY.json +++ b/inst/extdata/OSD/G/GRITNEY.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nResponsibility for Gritney series was transferred to North Carolina in l986. The classification of this series was changed with the 12/86 revision from clayey, mixed, thermic Typic Hapludults to clayey, mixed, thermic Aquic Hapludults. This is based on selected water table studies. The November 2025 revision moved the type location from Northampton County, North Carolina to Halifax County, North Carolina to a more representative site. No data was changed.\nDiagnostic horizons and soil characteristics recognized in this pedon are:\nOchric epipedon--the zone from 0 to 15 centimeters (0-6 inches) (Ap horizon)\nArgillic horizon--the zone from 15 to 107 centimeters (6 to 42 inches) (Bt horizons)\nAquic conditions--periodic saturation and iron depletions in the zone from 69 to 152 centimeters (27 to 60 inches) (Bt3, BC, and C horizons)" + "content": "REMARKS:\nResponsibility for Gritney series was transferred to North Carolina in l986. The classification of this series was changed with the 12/86 revision from clayey, mixed, thermic Typic Hapludults to clayey, mixed, thermic Aquic Hapludults. This is based on selected water table studies. The November 2025 revision moved the type location from Northampton County, North Carolina to Halifax County, North Carolina to a more representative site. No data was changed.\nDiagnostic horizons and soil characteristics recognized in this pedon are:\nOchric epipedon--the zone from 0 to 15 centimeters (0-6 inches) (Ap horizon)\nArgillic horizon--the zone from 15 to 107 centimeters (6 to 42 inches) (Bt horizons)\nAquic conditions--periodic saturation and iron depletions in the zone from 69 to 152 centimeters (27 to 60 inches) (Bt3, BC, and C horizons)\nCharacterization analysis for typical pedon (S85NC-131-1) was completed by NCSU." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA & TABULAR SERIES DATA", diff --git a/inst/extdata/OSD/G/GROSSTOWN.json b/inst/extdata/OSD/G/GROSSTOWN.json index 218446a314..491c35c74a 100644 --- a/inst/extdata/OSD/G/GROSSTOWN.json +++ b/inst/extdata/OSD/G/GROSSTOWN.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Coastal plain of southern Maryland and possibly parts of Delaware and New Jersey\nExtent: The series is of small extent, but locally significant.\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Coastal plain of southern Maryland and possibly parts of Delaware and New Jersey\nExtent: The series is of small extent, but locally significant. & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES ESTABLISHED", diff --git a/inst/extdata/OSD/G/GUNSTON.json b/inst/extdata/OSD/G/GUNSTON.json index 05459847bd..75356e2cae 100644 --- a/inst/extdata/OSD/G/GUNSTON.json +++ b/inst/extdata/OSD/G/GUNSTON.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Virginia\nExtent: Small\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Virginia\nExtent: Small & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES PROPOSED", diff --git a/inst/extdata/OSD/H/HAYWOOD.json b/inst/extdata/OSD/H/HAYWOOD.json index 38f3dc1906..3422178245 100644 --- a/inst/extdata/OSD/H/HAYWOOD.json +++ b/inst/extdata/OSD/H/HAYWOOD.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:" + "content": "REMARKS:\n3/2022 This layer was removed from the typical pedon description because /freshly fallen, or undecomposed leaf litter or simlar undeceomposed material should not be included as a surface layer in the soil description. The typical pedon originally had a top layer described as undecomposed leaf material or similar undecomposed material. WJN" }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/H/HENLOPEN.json b/inst/extdata/OSD/H/HENLOPEN.json index e7a6a8de4a..2d223142ce 100644 --- a/inst/extdata/OSD/H/HENLOPEN.json +++ b/inst/extdata/OSD/H/HENLOPEN.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Coastal Plain of Maryland and Delaware\nExtent: Small\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Coastal Plain of Maryland and Delaware\nExtent: Small & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES ESTABLISHED", diff --git a/inst/extdata/OSD/H/HICO.json b/inst/extdata/OSD/H/HICO.json index 9f74c57787..f79fca9c13 100644 --- a/inst/extdata/OSD/H/HICO.json +++ b/inst/extdata/OSD/H/HICO.json @@ -10,12 +10,12 @@ "content": "TAXONOMIC CLASS: Fine-loamy, siliceous, active, thermic Udic Haplustalfs" }, "TYPICAL PEDON": { - "section": "TYPICAL PEDON & Typical pedon of Cisco fine sandy loam, 1 to 5 percent slopes; from the intersection of Texas Highway 6 and U.S. Highway 281 in Hico, 0.8 south on U.S. Highway 281, 4.7 miles south on Farm Road 1602, 0.6 mile west on private road, and 900 feet north of farm house in old cropland field. USGS topographic quadrangle: Hico, TX;", - "content": "TYPICAL PEDON: Hico fine sandy loam--rangeland. (Colors are for dry soil unless otherwise stated.)\nAp--0 to 15 cm (0 to 6 in); brown (7.5YR 5/4) fine sandy loam, brown (7.5YR 4/4) moist; weak fine subangular blocky structure; slightly hard, friable; many very fine roots; 1 percent wormcast; noneffervescent; neutral; abrupt smooth boundary.\nA--15 to 30 cm (6 to 12 in); brown (7.5YR 5/4) fine sandy loam, brown (7.5YR 4/4) moist; weak fine subangular structure; slightly hard, friable; many very fine roots; 1 percent wormcast; noneffervescent; neutral; abrupt smooth boundary. Combined Thickness of A horizons is 6 to 46 cm (2 to 18 in)\nBt1--30 to 46 cm (12 to 18 in); reddish brown (5YR 4/4) sandy clay loam, dark reddish brown (5YR 3/4) moist; moderate medium subangular blocky structure; hard, firm; common fine roots; 1 percent wormcast; many prominent clay films on faces of peds; neutral; gradual smooth boundary.\nBt2--46 to 94 cm (18 to 37 in); yellowish red (5YR 5/6) sandy clay loam, yellowish red (5YR 4/6) moist; moderate medium subangular blocky structure; hard, firm; common fine roots; many prominent clay films on faces of peds; neutral; gradual smooth boundary.\nBt3--94 to 130 cm (37 to 51 in); yellowish red (5YR 5/6) sandy clay loam, yellowish red (55YR 4/6) moist; moderate medium subangular blocky structure; few fine faint brown (7.5YR 5/4) masses of oxidized iron; hard, firm; few fine roots; common distinct clay films on faces of peds; neutral; clear wavy boundary. Combined thickness of Bt horizons is 30 to 120 cm (11 to 47 in)\nBCk--130 to 1203 cm (51 to 80 in); light gray (10YR 8/2) fine sandy loam, light brownish gray (10YR 7/2) moist; weak fine subangular blocky structure; slightly hard, friable; few fine distinct brown (7.5YR 5/6) masses of oxidized iron; few fine distinct yellowish red (5YR 5/8) masses of oxidized iron; 1 percent fine calcium carbonate concretions; slightly effervescent; moderately alkaline. Thickness of BCk horizon is 50 to 130 cm (20 to 51 in) & Typical pedon of Cisco fine sandy loam, 1 to 5 percent slopes; from the intersection of Texas Highway 6 and U.S. Highway 281 in Hico, 0.8 south on U.S. Highway 281, 4.7 miles south on Farm Road 1602, 0.6 mile west on private road, and 900 feet north of farm house in old cropland field. USGS topographic quadrangle: Hico, TX;\nLatitude: 31 degrees, 55 minutes, 14.83 seconds, N;\nLongitude: 98 degrees, 0 minutes, 26.03 seconds, W;\nDatum: WGS84.\nUTM Easting 593855.02 m, UTM Northing 33532085.36m; UTM Zone 14." + "section": "TYPICAL PEDON", + "content": "TYPICAL PEDON: Hico fine sandy loam--rangeland. (Colors are for dry soil unless otherwise stated.)\nAp--0 to 15 cm (0 to 6 in); brown (7.5YR 5/4) fine sandy loam, brown (7.5YR 4/4) moist; weak fine subangular blocky structure; slightly hard, friable; many very fine roots; 1 percent wormcast; noneffervescent; neutral; abrupt smooth boundary.\nA--15 to 30 cm (6 to 12 in); brown (7.5YR 5/4) fine sandy loam, brown (7.5YR 4/4) moist; weak fine subangular structure; slightly hard, friable; many very fine roots; 1 percent wormcast; noneffervescent; neutral; abrupt smooth boundary. Combined Thickness of A horizons is 6 to 46 cm (2 to 18 in)\nBt1--30 to 46 cm (12 to 18 in); reddish brown (5YR 4/4) sandy clay loam, dark reddish brown (5YR 3/4) moist; moderate medium subangular blocky structure; hard, firm; common fine roots; 1 percent wormcast; many prominent clay films on faces of peds; neutral; gradual smooth boundary.\nBt2--46 to 94 cm (18 to 37 in); yellowish red (5YR 5/6) sandy clay loam, yellowish red (5YR 4/6) moist; moderate medium subangular blocky structure; hard, firm; common fine roots; many prominent clay films on faces of peds; neutral; gradual smooth boundary.\nBt3--94 to 130 cm (37 to 51 in); yellowish red (5YR 5/6) sandy clay loam, yellowish red (55YR 4/6) moist; moderate medium subangular blocky structure; few fine faint brown (7.5YR 5/4) masses of oxidized iron; hard, firm; few fine roots; common distinct clay films on faces of peds; neutral; clear wavy boundary. Combined thickness of Bt horizons is 30 to 120 cm (11 to 47 in)\nBCk--130 to 1203 cm (51 to 80 in); light gray (10YR 8/2) fine sandy loam, light brownish gray (10YR 7/2) moist; weak fine subangular blocky structure; slightly hard, friable; few fine distinct brown (7.5YR 5/6) masses of oxidized iron; few fine distinct yellowish red (5YR 5/8) masses of oxidized iron; 1 percent fine calcium carbonate concretions; slightly effervescent; moderately alkaline. Thickness of BCk horizon is 50 to 130 cm (20 to 51 in)" }, "TYPE LOCATION": { "section": "TYPE LOCATION", - "content": "TYPE LOCATION: Hamilton County, Texas;" + "content": "TYPE LOCATION: Hamilton County, Texas;\nTypical pedon of Cisco fine sandy loam, 1 to 5 percent slopes; from the intersection of Texas Highway 6 and U.S. Highway 281 in Hico, 0.8 south on U.S. Highway 281, 4.7 miles south on Farm Road 1602, 0.6 mile west on private road, and 900 feet north of farm house in old cropland field. USGS topographic quadrangle: Hico, TX;\nLatitude: 31 degrees, 55 minutes, 14.83 seconds, N;\nLongitude: 98 degrees, 0 minutes, 26.03 seconds, W;\nDatum: WGS84.\nUTM Easting 593855.02 m, UTM Northing 33532085.36m; UTM Zone 14." }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", @@ -207,7 +207,7 @@ "eff_class": "slightly effervescent", "distinctness": "NA", "topography": "NA", - "narrative": "BCk--130 to 1203 cm (51 to 80 in); light gray (10YR 8/2) fine sandy loam, light brownish gray (10YR 7/2) moist; weak fine subangular blocky structure; slightly hard, friable; few fine distinct brown (7.5YR 5/6) masses of oxidized iron; few fine distinct yellowish red (5YR 5/8) masses of oxidized iron; 1 percent fine calcium carbonate concretions; slightly effervescent; moderately alkaline. Thickness of BCk horizon is 50 to 130 cm (20 to 51 in) & Typical pedon of Cisco fine sandy loam, 1 to 5 percent slopes; from the intersection of Texas Highway 6 and U.S. Highway 281 in Hico, 0.8 south on U.S. Highway 281, 4.7 miles south on Farm Road 1602, 0.6 mile west on private road, and 900 feet north of farm house in old cropland field. USGS topographic quadrangle: Hico, TX;" + "narrative": "BCk--130 to 1203 cm (51 to 80 in); light gray (10YR 8/2) fine sandy loam, light brownish gray (10YR 7/2) moist; weak fine subangular blocky structure; slightly hard, friable; few fine distinct brown (7.5YR 5/6) masses of oxidized iron; few fine distinct yellowish red (5YR 5/8) masses of oxidized iron; 1 percent fine calcium carbonate concretions; slightly effervescent; moderately alkaline. Thickness of BCk horizon is 50 to 130 cm (20 to 51 in)" } ] ] diff --git a/inst/extdata/OSD/H/HOCKLEY.json b/inst/extdata/OSD/H/HOCKLEY.json index bc067fe0d2..b0c3cba5a3 100644 --- a/inst/extdata/OSD/H/HOCKLEY.json +++ b/inst/extdata/OSD/H/HOCKLEY.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nDiagnostic horizons and features recognized in this pedon are:\nParticle size control section: 58 to 108 cm (23 to 43 in). (Bt horizon)\nOchric epipedon: 0 to 58 cm (0 to 23 in). (A1 and A2 horizons)\nArgillic horizon: 58 to 254 cm (23 to 100 in). (Bt, Btvc1, B't horizons)\nMore than 5 percent plinthite: 127 to 191 cm (50 to 75 in)in (Btvc)" + "content": "REMARKS:\nDiagnostic horizons and features recognized in this pedon are:\nParticle size control section: 58 to 108 cm (23 to 43 in). (Bt horizon)\nOchric epipedon: 0 to 58 cm (0 to 23 in). (A1 and A2 horizons)\nArgillic horizon: 58 to 254 cm (23 to 100 in). (Bt, Btvc1, B't horizons)\nMore than 5 percent plinthite: 127 to 191 cm (50 to 75 in)in (Btvc)\nAdditional Comments: This series recognizes graded phases. The series description was updated during the soil data join and recorrelation initiative in 2014. MLRA 150 Soil Survey office sampled and redescribed the typical pedon during the update of MLRA 150A. The surface texture was changed from a fine sandy loam to a loamy fine sand.\nThe assignment of the cation-exchange activity class is supported by laboratory data number S00TX-473-1 from Waller County, Texas.\nThe mineralogy is supported by laboratory data on sample 72TX-101-3 (72L107)." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/H/HOGHOLE.json b/inst/extdata/OSD/H/HOGHOLE.json index 14cf987e6c..f5ad57cfe8 100644 --- a/inst/extdata/OSD/H/HOGHOLE.json +++ b/inst/extdata/OSD/H/HOGHOLE.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Coastal plain of southern Maryland; possibly New Jersey.\nExtent: Not extensive, but locally significant.\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Coastal plain of southern Maryland; possibly New Jersey.\nExtent: Not extensive, but locally significant. & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES ESTABLISHED", diff --git a/inst/extdata/OSD/H/HONEOYE.json b/inst/extdata/OSD/H/HONEOYE.json index 754042b621..e55585be82 100644 --- a/inst/extdata/OSD/H/HONEOYE.json +++ b/inst/extdata/OSD/H/HONEOYE.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: The more gently sloping Honeoye soils are among the most productive upland soils in New York State. The Honeoye series has been unofficially recognized as the state soil of New York." + "content": "REMARKS: The more gently sloping Honeoye soils are among the most productive upland soils in New York State. The Honeoye series has been unofficially recognized as the state soil of New York.\nA new pedon from Onondaga County (the typical from the Onondaga Soil Survey) was used because the typical pedon did not match the typical pedon for Honeoye in the Ontario County, NY Soil Survey.\nCEC activity class changed from active to semi-active based on lab data for the Honeoye-Lima-Kendaia catena.\nDiagnostic horizons and other features recognized in the typical pedon are as follows:\n(1) Ochric epipedon - the zone from the surface to 20 cm (8 in) (Ap horizon).\n(2) Argillic horizon - the zone from 25 to 74 cm (10 to 29 in) (Bt/E and Bt horizons).\n(3) Glossic subgroup - as evidenced by interfingering of Albic material around peds in the upper part of the Argillic horizon (Bt/E horizon)." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/I/ISSUE.json b/inst/extdata/OSD/I/ISSUE.json index 2ad87bddc5..d5a67dc19b 100644 --- a/inst/extdata/OSD/I/ISSUE.json +++ b/inst/extdata/OSD/I/ISSUE.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Flood plains of the mid-Atlantic Coastal Plain of Maryland, Delaware, and possibly New Jersey\nExtent: Moderate\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Flood plains of the mid-Atlantic Coastal Plain of Maryland, Delaware, and possibly New Jersey\nExtent: Moderate & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES ESTABLISHED", diff --git a/inst/extdata/OSD/J/JUDYVILLE.json b/inst/extdata/OSD/J/JUDYVILLE.json index 4ebba3492c..109d4eccc5 100644 --- a/inst/extdata/OSD/J/JUDYVILLE.json +++ b/inst/extdata/OSD/J/JUDYVILLE.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Judyville soils were previously correlated as Weikert Variant and Muskingum soils in previous surveys.\nThe differentiae needed to clearly separate Judyville series from the Matewan series is not well defined in terms of soil properties. Until they can be better defined, Judyville soils will be restricted to LRR M in MLRAs 111D, 114B and 115C.\nDiagnostic horizons and features recognized in this pedon are:\nOchric epipedon: from the surface to a depth of 23 cm (Oi, A, BA horizons).\nCambic horizon: from a depth of 13 to 86 cm (BA, Bw1, Bw2, Bw3 horizons).\nLithic contact: at 86 cm (top of the R layer)." + "content": "REMARKS: Judyville soils were previously correlated as Weikert Variant and Muskingum soils in previous surveys.\nThe differentiae needed to clearly separate Judyville series from the Matewan series is not well defined in terms of soil properties. Until they can be better defined, Judyville soils will be restricted to LRR M in MLRAs 111D, 114B and 115C.\nDiagnostic horizons and features recognized in this pedon are:\nOchric epipedon: from the surface to a depth of 23 cm (Oi, A, BA horizons).\nCambic horizon: from a depth of 13 to 86 cm (BA, Bw1, Bw2, Bw3 horizons).\nLithic contact: at 86 cm (top of the R layer).\nRepresentative data mapunit for the typical pedon is DMU ID 153344 in MO 11." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/K/KINGSTOWNE.json b/inst/extdata/OSD/K/KINGSTOWNE.json index 38f6c85baa..da5c6e7b53 100644 --- a/inst/extdata/OSD/K/KINGSTOWNE.json +++ b/inst/extdata/OSD/K/KINGSTOWNE.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Virginia\nExtent: Small\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Virginia\nExtent: Small & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES PROPOSED", diff --git a/inst/extdata/OSD/K/KONIAG.json b/inst/extdata/OSD/K/KONIAG.json index ed65953f95..c6598ba8ac 100644 --- a/inst/extdata/OSD/K/KONIAG.json +++ b/inst/extdata/OSD/K/KONIAG.json @@ -26,8 +26,8 @@ "content": "COMPETING SERIES: There are no competing series." }, "GEOGRAPHIC SETTING": { - "section": "GEOGRAPHIC SETTING", - "content": "GEOGRAPHIC SETTING:\nElevation: 5 to 365 meters (15 to 1200 feet)\nParent material: moderately decomposed herbaceous organic material over medial silty volcanic ash over gravelly loamy till\nLandform: plains and hills\nSlope: 15 to 60 percent\nMean annual temperature: 0 to 6 degrees C. (32 to 43 degrees F.)\nMean annual precipitation: 600 to 2000 mm (23 to 79 in)\nFrost free period: 20 to 50 days\nGEOGRAPHIC SETTING:\nDepth class: very deep\nDrainage class: well drained\nParent material: moderately decomposed herbaceous organic material over medial silty volcanic ash over gravelly loamy till\nLandform: plains and hills\nSlopes: 0 to 30 percent\nMean annual precipitation: 900 to 2000 mm (35 to 79 in)\nMean annual temperature: 0 to 6 degrees C. (32 to 43 degrees F.)\nFrost-free season: 20 to 50 days" + "section": "GEOGRAPHIC SETTING & GEOGRAPHIC SETTING", + "content": "GEOGRAPHIC SETTING:\nElevation: 5 to 365 meters (15 to 1200 feet)\nParent material: moderately decomposed herbaceous organic material over medial silty volcanic ash over gravelly loamy till\nLandform: plains and hills\nSlope: 15 to 60 percent\nMean annual temperature: 0 to 6 degrees C. (32 to 43 degrees F.)\nMean annual precipitation: 600 to 2000 mm (23 to 79 in)\nFrost free period: 20 to 50 days & GEOGRAPHIC SETTING:\nDepth class: very deep\nDrainage class: well drained\nParent material: moderately decomposed herbaceous organic material over medial silty volcanic ash over gravelly loamy till\nLandform: plains and hills\nSlopes: 0 to 30 percent\nMean annual precipitation: 900 to 2000 mm (35 to 79 in)\nMean annual temperature: 0 to 6 degrees C. (32 to 43 degrees F.)\nFrost-free season: 20 to 50 days" }, "GEOGRAPHICALLY ASSOCIATED SOILS": { "section": "GEOGRAPHICALLY ASSOCIATED SOILS", diff --git a/inst/extdata/OSD/L/LANCASTER.json b/inst/extdata/OSD/L/LANCASTER.json index 050e8983ac..1df816132e 100644 --- a/inst/extdata/OSD/L/LANCASTER.json +++ b/inst/extdata/OSD/L/LANCASTER.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are: Particle-size control section: The zone from 41 to 76 centimeters (16 to 30 inches). (Bt1, Bt2 horizons)\nMollic epipedon: The zone from 0 to 41 centimeters (0 to 16 inches). (A and BA horizons)\nArgillic horizon: The zone from 41 to 76 centimeters (16 to 30 inches). (Bt1, Bt2 horizons)\nParalithic contact: The contact with weathered sandy shale at 76 centimeters (30 inches). (Cr horizons)\nThe assignment of the CEC activity class is supported by KSSL lab sample numbers 81P0658 (pedon 81KS115001), 99P0643 (pedon 99KS169003), 02N0361 (pedon S02KS-029-002), and 40A1794 (pedon 53KS169006).\nLRR=H\nAdded \"moderately deep\" to first sentence in the first paragraph. Increase slope range to \"16 percent\".\nDescribed wet consistence in typical pedon and added clay film to the Bt horizons.\nRemoved series that did compete within the same family from the competing series paragraph.\nChanged runoff from rapid to medium to reflect permeability.\nAdded Soil Interpretation Record clay content and sand content to \"Range In Characteristics\".\nModified format by LRM in 2/2006 to include metric conversion and change permeability to saturated hydraulic conductivity." + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are: Particle-size control section: The zone from 41 to 76 centimeters (16 to 30 inches). (Bt1, Bt2 horizons)\nMollic epipedon: The zone from 0 to 41 centimeters (0 to 16 inches). (A and BA horizons)\nArgillic horizon: The zone from 41 to 76 centimeters (16 to 30 inches). (Bt1, Bt2 horizons)\nParalithic contact: The contact with weathered sandy shale at 76 centimeters (30 inches). (Cr horizons)\nThe assignment of the CEC activity class is supported by KSSL lab sample numbers 81P0658 (pedon 81KS115001), 99P0643 (pedon 99KS169003), 02N0361 (pedon S02KS-029-002), and 40A1794 (pedon 53KS169006).\nLRR=H\nAdded \"moderately deep\" to first sentence in the first paragraph. Increase slope range to \"16 percent\".\nDescribed wet consistence in typical pedon and added clay film to the Bt horizons.\nRemoved series that did compete within the same family from the competing series paragraph.\nChanged runoff from rapid to medium to reflect permeability.\nAdded Soil Interpretation Record clay content and sand content to \"Range In Characteristics\".\nModified format by LRM in 2/2006 to include metric conversion and change permeability to saturated hydraulic conductivity.\n05/2014 DJK Updated intro paragraph to SSRO5 standards. Updated activity class in classification from superactive to active (added statement in remarks about this being from KSSL lab data). Added slope, aspect, slope shape, and elevation to typical pedon. Added quadrangle and lat/long to type location. Updated soil moisture regime to SSRO5 requirements and added mean annual soil temperature. Added sand content and BA horizon data to RIC. Updated parent material, changed slopes to 20 percent from 16 percent because of the 3396 3-20 percent map unit. Updated climate data, added precipitation pattern, and added elevation to geographic setting. Updated competing series for new classification with active activity class. Changed runoff to high. Updated geographically associated soils and distribution and extent sections." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/L/LEIPSIC.json b/inst/extdata/OSD/L/LEIPSIC.json index 37a3404a28..e302f37dc8 100644 --- a/inst/extdata/OSD/L/LEIPSIC.json +++ b/inst/extdata/OSD/L/LEIPSIC.json @@ -6,8 +6,8 @@ "STATES": "DE", "OVERVIEW": "MLRA(s): 153C", "TAXONOMIC CLASS": { - "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Fine-silty, mixed, semiactive, mesic Aquic Hapludults\nDepth Class: Very deep\nAgricultural Drainage Class: Moderately well drained\nIndex Surface Runoff: Low or medium\nInternal Free Water Occurance: Moderately deep; common\nPermeability: Moderate or moderately slow\nParent Material: Silty eolian deposits underlain by stratified alluvial sediments\nSlope: 0 to 10 percent\nMean Annual Air Temperature (type location): 55 degrees F.\nMean Annual Precipitation (type location): 44 inches\nTAXONOMIC CLASS: Fine-silty, mixed, semiactive, mesic Aquic Hapludults" + "section": "TAXONOMIC CLASS & TAXONOMIC CLASS", + "content": "TAXONOMIC CLASS: Fine-silty, mixed, semiactive, mesic Aquic Hapludults\nDepth Class: Very deep\nAgricultural Drainage Class: Moderately well drained\nIndex Surface Runoff: Low or medium\nInternal Free Water Occurance: Moderately deep; common\nPermeability: Moderate or moderately slow\nParent Material: Silty eolian deposits underlain by stratified alluvial sediments\nSlope: 0 to 10 percent\nMean Annual Air Temperature (type location): 55 degrees F.\nMean Annual Precipitation (type location): 44 inches & TAXONOMIC CLASS: Fine-silty, mixed, semiactive, mesic Aquic Hapludults" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", diff --git a/inst/extdata/OSD/L/LEONARDTOWN.json b/inst/extdata/OSD/L/LEONARDTOWN.json index b8b84f3d61..7d1cb88d8b 100644 --- a/inst/extdata/OSD/L/LEONARDTOWN.json +++ b/inst/extdata/OSD/L/LEONARDTOWN.json @@ -10,8 +10,8 @@ "content": "TAXONOMIC CLASS: Fine-silty, mixed, active, mesic Typic Fragiaquults" }, "TYPICAL PEDON": { - "section": "TYPICAL PEDON & The 2007 revision moves the Typical Pedon. The previous Typical Pedon was imprecisely located and could not be found for study. It also changes the CE activity Class from semiactive to active based on the classification of similar soils in the region.", - "content": "TYPICAL PEDON: Leonardtown silt loam in a forested area (Colors are for moist soil)\nOi--0 to 2.5 cm (0 to 1 inch); very dark brown (7.5YR 2.5/2) slightly decomposed leaves and twigs; clear smooth boundary. (0 to 8 cm thick)\nAg--2.5 to 5 cm (1 to 2 inches); black (10YR 2/1) silt loam; weak medium subangular blocky structure; slightly hard, friable; slightly sticky, slightly plastic; many very coarse, coarse, medium and fine roots; extremely acid; clear smooth boundary. (2.5 to 18 cm thick)\nBtg1--5 to 36 cm (2 to 14 inches); gray (10YR 5/1) silty clay loam; weak coarse subangular blocky structure; slightly hard, friable; slightly sticky, slightly plastic; common coarse, medium and fine roots; few medium tubular pores; common medium prominent yellowish red (5YR 4/6) iron masses in matrix; common distinct gray (2.5Y 6/1) clay films on faces of peds and in pores; extremely acid; abrupt smooth boundary.\nBtg2--36 to 46 cm (14 to 18 inches); gray (2.5Y 6/1) silt loam; moderate coarse subangular blocky structure; slightly hard, friable; slightly sticky, slightly plastic; common medium and fine roots; few medium tubular pores; many medium prominent brownish yellow (10YR 6/8) iron masses in matrix; common distinct gray (2.5Y 6/1) clay films on faces of peds and in pores; extremely acid; clear smooth boundary.\nBtg3--46 to 56 cm (18 to 22 inches); light gray (2.5Y 7/1) silt loam; weak coarse subangular blocky structure; slightly hard, friable; slightly sticky, slightly plastic; few medium, fine, and very fine roots; few medium tubular pores; few medium prominent brownish yellow (10YR 6/8) iron masses in matrix; common distinct white (10YR 8/1) clay depletions on faces of peds and in pores; extremely acid; abrupt smooth boundary. (Combined thickness of the Btg horizon is 30 to 64 cm)\nBtgx1--56 to 71 cm (22 to 28 inches); gray (10YR 6/1) loam; strong very coarse prismatic structure parting to strong coarse subangular blocky and thick platy; very hard, very firm and brittle in 60 percent of the volume; moderately sticky, moderately plastic; few medium, fine and very fine roots between faces of prisms; common very fine, fine, and medium tubular and vesicular pores throughout; common medium prominent light olive brown (2.5Y 5/6) iron masses in the matrix; common distinct gray (10YR 5/1) clay films on faces of peds and in pores; common fine distinct white (2.5Y 8/1) clay depletions on faces of prisms; extremely acid; abrupt smooth boundary.\nBtgx2--71 to 109 cm (28 to 43 inches); gray (10YR 6/1) loam; weak very coarse prismatic structure parting to weak coarse subangular blocky and thick platy; very hard, very firm and brittle in 60 percent of the volume; moderately sticky, moderately plastic; few fine and very fine roots between faces of prisms; common very fine and fine tubular and vesicular pores throughout; common medium prominent strong brown (7.5YR 4/6) iron masses in the matrix; common distinct gray (10YR 5/1) clay films on faces of prisms, and common fine distinct white (10YR 8/1) clay depletions on faces of prisms; extremely acid; abrupt smooth boundary. (Combined thickness of the Btgx horizon is 18 to 53 cm)\n2BCg--109 to 157 cm (43 to 62 inches); gray (10YR 5/1) sandy clay loam; moderate very coarse subangular blocky structure; slightly hard, firm and brittle in 5 percent of the volume; moderately sticky, moderately plastic; common very fine, fine, and medium tubular and vesicular pores throughout; common medium prominent strong brown (7.5YR 4/6) iron masses in the matrix; and common fine prominent white (2.5Y 8/1) clay depletions on faces of peds; 1 percent gravel; extremely acid. & The 2007 revision moves the Typical Pedon. The previous Typical Pedon was imprecisely located and could not be found for study. It also changes the CE activity Class from semiactive to active based on the classification of similar soils in the region." + "section": "TYPICAL PEDON", + "content": "TYPICAL PEDON: Leonardtown silt loam in a forested area (Colors are for moist soil)\nOi--0 to 2.5 cm (0 to 1 inch); very dark brown (7.5YR 2.5/2) slightly decomposed leaves and twigs; clear smooth boundary. (0 to 8 cm thick)\nAg--2.5 to 5 cm (1 to 2 inches); black (10YR 2/1) silt loam; weak medium subangular blocky structure; slightly hard, friable; slightly sticky, slightly plastic; many very coarse, coarse, medium and fine roots; extremely acid; clear smooth boundary. (2.5 to 18 cm thick)\nBtg1--5 to 36 cm (2 to 14 inches); gray (10YR 5/1) silty clay loam; weak coarse subangular blocky structure; slightly hard, friable; slightly sticky, slightly plastic; common coarse, medium and fine roots; few medium tubular pores; common medium prominent yellowish red (5YR 4/6) iron masses in matrix; common distinct gray (2.5Y 6/1) clay films on faces of peds and in pores; extremely acid; abrupt smooth boundary.\nBtg2--36 to 46 cm (14 to 18 inches); gray (2.5Y 6/1) silt loam; moderate coarse subangular blocky structure; slightly hard, friable; slightly sticky, slightly plastic; common medium and fine roots; few medium tubular pores; many medium prominent brownish yellow (10YR 6/8) iron masses in matrix; common distinct gray (2.5Y 6/1) clay films on faces of peds and in pores; extremely acid; clear smooth boundary.\nBtg3--46 to 56 cm (18 to 22 inches); light gray (2.5Y 7/1) silt loam; weak coarse subangular blocky structure; slightly hard, friable; slightly sticky, slightly plastic; few medium, fine, and very fine roots; few medium tubular pores; few medium prominent brownish yellow (10YR 6/8) iron masses in matrix; common distinct white (10YR 8/1) clay depletions on faces of peds and in pores; extremely acid; abrupt smooth boundary. (Combined thickness of the Btg horizon is 30 to 64 cm)\nBtgx1--56 to 71 cm (22 to 28 inches); gray (10YR 6/1) loam; strong very coarse prismatic structure parting to strong coarse subangular blocky and thick platy; very hard, very firm and brittle in 60 percent of the volume; moderately sticky, moderately plastic; few medium, fine and very fine roots between faces of prisms; common very fine, fine, and medium tubular and vesicular pores throughout; common medium prominent light olive brown (2.5Y 5/6) iron masses in the matrix; common distinct gray (10YR 5/1) clay films on faces of peds and in pores; common fine distinct white (2.5Y 8/1) clay depletions on faces of prisms; extremely acid; abrupt smooth boundary.\nBtgx2--71 to 109 cm (28 to 43 inches); gray (10YR 6/1) loam; weak very coarse prismatic structure parting to weak coarse subangular blocky and thick platy; very hard, very firm and brittle in 60 percent of the volume; moderately sticky, moderately plastic; few fine and very fine roots between faces of prisms; common very fine and fine tubular and vesicular pores throughout; common medium prominent strong brown (7.5YR 4/6) iron masses in the matrix; common distinct gray (10YR 5/1) clay films on faces of prisms, and common fine distinct white (10YR 8/1) clay depletions on faces of prisms; extremely acid; abrupt smooth boundary. (Combined thickness of the Btgx horizon is 18 to 53 cm)\n2BCg--109 to 157 cm (43 to 62 inches); gray (10YR 5/1) sandy clay loam; moderate very coarse subangular blocky structure; slightly hard, firm and brittle in 5 percent of the volume; moderately sticky, moderately plastic; common very fine, fine, and medium tubular and vesicular pores throughout; common medium prominent strong brown (7.5YR 4/6) iron masses in the matrix; and common fine prominent white (2.5Y 8/1) clay depletions on faces of peds; 1 percent gravel; extremely acid." }, "TYPE LOCATION": { "section": "TYPE LOCATION", @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Prior to 1939, the Leonardtown series included moderately well drained soils that are now correlated to the Beltsville series, and somewhat poorly drained soils that are now correlated to the Aquasco series.\nDiagnostic horizons and soil characteristics recognized in this pedon are:\nOchric epipedon--the zone from 0 to 5 cm (0 to 2 inches) (Ag horizon)\nArgillic horizon--the zone from 5 to 109 cm (2 to 43 inches) (Btg horizons)\nFragipan--the zone from 56 to 109 cm (22 to 43 inches) (Btgx horizon)\nAquic conditions--redoximorphic features occur in all horizons below the mineral soil surface, with periodic saturation and reduction at some time during the year\nOther soil features identified with this pedon:\nSeries control section--the zone from 0 to 150 cm (0 to 59 inches)\nPrevious revisions: 03/2006-WDC, 08/2006-WDC/Rev. DRPV" + "content": "REMARKS: Prior to 1939, the Leonardtown series included moderately well drained soils that are now correlated to the Beltsville series, and somewhat poorly drained soils that are now correlated to the Aquasco series.\nDiagnostic horizons and soil characteristics recognized in this pedon are:\nOchric epipedon--the zone from 0 to 5 cm (0 to 2 inches) (Ag horizon)\nArgillic horizon--the zone from 5 to 109 cm (2 to 43 inches) (Btg horizons)\nFragipan--the zone from 56 to 109 cm (22 to 43 inches) (Btgx horizon)\nAquic conditions--redoximorphic features occur in all horizons below the mineral soil surface, with periodic saturation and reduction at some time during the year\nOther soil features identified with this pedon:\nSeries control section--the zone from 0 to 150 cm (0 to 59 inches)\nPrevious revisions: 03/2006-WDC, 08/2006-WDC/Rev. DRPV\nThe 2007 revision moves the Typical Pedon. The previous Typical Pedon was imprecisely located and could not be found for study. It also changes the CE activity Class from semiactive to active based on the classification of similar soils in the region." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", @@ -253,7 +253,7 @@ "eff_class": "NA", "distinctness": "NA", "topography": "NA", - "narrative": "2BCg--109 to 157 cm (43 to 62 inches); gray (10YR 5/1) sandy clay loam; moderate very coarse subangular blocky structure; slightly hard, firm and brittle in 5 percent of the volume; moderately sticky, moderately plastic; common very fine, fine, and medium tubular and vesicular pores throughout; common medium prominent strong brown (7.5YR 4/6) iron masses in the matrix; and common fine prominent white (2.5Y 8/1) clay depletions on faces of peds; 1 percent gravel; extremely acid. & The 2007 revision moves the Typical Pedon. The previous Typical Pedon was imprecisely located and could not be found for study. It also changes the CE activity Class from semiactive to active based on the classification of similar soils in the region." + "narrative": "2BCg--109 to 157 cm (43 to 62 inches); gray (10YR 5/1) sandy clay loam; moderate very coarse subangular blocky structure; slightly hard, firm and brittle in 5 percent of the volume; moderately sticky, moderately plastic; common very fine, fine, and medium tubular and vesicular pores throughout; common medium prominent strong brown (7.5YR 4/6) iron masses in the matrix; and common fine prominent white (2.5Y 8/1) clay depletions on faces of peds; 1 percent gravel; extremely acid." } ] ] diff --git a/inst/extdata/OSD/L/LEW.json b/inst/extdata/OSD/L/LEW.json index c746e3652e..acfad151e7 100644 --- a/inst/extdata/OSD/L/LEW.json +++ b/inst/extdata/OSD/L/LEW.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Lew soils were formerly included with the Clifton, Catoctin, Myersville, and Unison series; also miscellaneous land types of Stony colluvial land and Stony land.\nDiagnostic horizons and features recognized in this pedon are:\nOchric epipedon - the zone from the surface to 13 inches (A and E horizons)\nArgillic horizon - zone from 13 to 74 or more inches (Bt horizons)\nSIR = VA0015, VA0016 (STONY), VA0247 (FLAGGY), VA0248 (CHANNERY)\nMLRA = 130\nREVISED = 9/97, 2/2022" + "content": "REMARKS: Lew soils were formerly included with the Clifton, Catoctin, Myersville, and Unison series; also miscellaneous land types of Stony colluvial land and Stony land.\nDiagnostic horizons and features recognized in this pedon are:\nOchric epipedon - the zone from the surface to 13 inches (A and E horizons)\nArgillic horizon - zone from 13 to 74 or more inches (Bt horizons)\nSIR = VA0015, VA0016 (STONY), VA0247 (FLAGGY), VA0248 (CHANNERY)\nMLRA = 130\nREVISED = 9/97, 2/2022\n2/2022 revision: Oi had 2 to 0 inch depths, corrected to be 0 to 2 in horizon depths then added 2 inches to all horizon depths throughout the typical pedon. WJN" }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/L/LEWBATH.json b/inst/extdata/OSD/L/LEWBATH.json index b874b43cc0..10f60649a2 100644 --- a/inst/extdata/OSD/L/LEWBATH.json +++ b/inst/extdata/OSD/L/LEWBATH.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: This series is the frigid equivalent of the Bath series, and the brown colored equivalent of the Lewbeach series.\nDiagnostic horizons and features recognized in this pedon include:\n1. Ochric epipedon - the zone from the surface to 20 cm (8 in) (Ap horizon).\n2. Cambic horizon - the zone from 20 to 53 cm (8 to 21 in) (Bw and BE horizons).\n3. Fragipan - the zone from 53 to 132 cm (21 to 52 in) (Bx1 and Bx2 horizons)." + "content": "REMARKS: This series is the frigid equivalent of the Bath series, and the brown colored equivalent of the Lewbeach series.\nDiagnostic horizons and features recognized in this pedon include:\n1. Ochric epipedon - the zone from the surface to 20 cm (8 in) (Ap horizon).\n2. Cambic horizon - the zone from 20 to 53 cm (8 to 21 in) (Bw and BE horizons).\n3. Fragipan - the zone from 53 to 132 cm (21 to 52 in) (Bx1 and Bx2 horizons).\n4. CEC activity class of semiactive based on lab data from one pedon (S85NY077-02) which is the typical pedon.\n5. Udic soil moisture regime." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/L/LILLIS.json b/inst/extdata/OSD/L/LILLIS.json index 178fea5acb..a5f70d5ddc 100644 --- a/inst/extdata/OSD/L/LILLIS.json +++ b/inst/extdata/OSD/L/LILLIS.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Previously mapped as Levis silty clay in the Soil Survey of the Mendota Area, California, Series 1940, No. 18.\nDiagnostic horizons and features recognized in this pedon are:\n1. OCHRIC EPIPEDON--0 to 13 inches (Apl, Ap2, Bnssz).\n1.1 Moist colors have values greater than 3.5.\n1. VERTISOL FEATURES\n1.1 Unless irrigated, vertical cracks extend from the surface and range from 0.5 to 2 inches wide at a depth of 20 inches.\n1.2 The typical pedon, which was cultivated and irrigated, had cracks to a depth of 21 inches. They ranged in size from 4 cm to 1 mm. Intersecting slickensides occur between the depths of 7 and 21 inches in the typical pedon.\n1.3 The cracks usually close from December thru April for 100 to 150 consecutive days" + "content": "REMARKS: Previously mapped as Levis silty clay in the Soil Survey of the Mendota Area, California, Series 1940, No. 18.\nDiagnostic horizons and features recognized in this pedon are:\n1. OCHRIC EPIPEDON--0 to 13 inches (Apl, Ap2, Bnssz).\n1.1 Moist colors have values greater than 3.5.\n1. VERTISOL FEATURES\n1.1 Unless irrigated, vertical cracks extend from the surface and range from 0.5 to 2 inches wide at a depth of 20 inches.\n1.2 The typical pedon, which was cultivated and irrigated, had cracks to a depth of 21 inches. They ranged in size from 4 cm to 1 mm. Intersecting slickensides occur between the depths of 7 and 21 inches in the typical pedon.\n1.3 The cracks usually close from December thru April for 100 to 150 consecutive days\n1.4 COLE values range from 0.12 to 0.20 cm/cm in the typical pedon.\n2. VERY-FINE FAMILY\n2.1 NSSL results show 61 to 66 percent clay in the typical pedon. There is 64 percent clay in the 10 to 40 inch particle-size control section.\n3. SMECTITIC MINERALOGY\n3.1 NSSL results show a predominance of smectite. Cracking and very-fine particle-size class are further evidence of the mineralogy.\n4. THERMIC TEMPERATURE REGIME\n4.1 Soil temperature regime is assumed to be thermic based upon data from Helm, CA (about 20 miles SE of typical site).\n4.2 Based on two of our soil temperature sites 18 and 24 miles SE of the typical site with 3 years of quarterly data. Soil temperature is 62 to 65 degrees F.\n5. PRECIPITATION\n5.1 MAP is about 8 inches based upon data from Mendota Dam, CA (about 10 miles N of the typical pedon).\n6. XERERT SUBORDER\n6.1 The soil temperature exceeds 47 degrees F, from Jan. to Dec. (365 days). Within this time period cracks are closed for 100 to 151 consecutive days.\n6.2 Cracks are open from May thru November.\nThe moisture control section data are as follows:" }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/L/LOLITE.json b/inst/extdata/OSD/L/LOLITE.json index 55ffe59885..4e4fcb1a2a 100644 --- a/inst/extdata/OSD/L/LOLITE.json +++ b/inst/extdata/OSD/L/LOLITE.json @@ -54,8 +54,8 @@ "content": "SERIES ESTABLISHED: Natrona County, Wyoming; 1985." }, "REMARKS": { - "section": "REMARKS", - "content": "REMARKS:\nThe superactive cation exchange activity class was added in 03/2003 to the taxonomic classification by the National Soil Survey Center on request of the Reno MLRA office, without review of the soil series property data. The remainder of this document has not been updated." + "section": "REMARKS & REMARKS", + "content": "REMARKS:\nThe superactive cation exchange activity class was added in 03/2003 to the taxonomic classification by the National Soil Survey Center on request of the Reno MLRA office, without review of the soil series property data. The remainder of this document has not been updated. & REMARKS:\nThe superactive cation exchange activity class was added in 03/2003 to the taxonomic classification by the National Soil Survey Center on request of the Reno MLRA office, without review of the soil series property data. The remainder of this document has not been updated." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/L/LONGFORD.json b/inst/extdata/OSD/L/LONGFORD.json index 3e5d4ad03f..e0a2106894 100644 --- a/inst/extdata/OSD/L/LONGFORD.json +++ b/inst/extdata/OSD/L/LONGFORD.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are: Mollic epipedon: The zone from 0 to 41 centimeters (0 to 16 inches). (A and BA horizons)\nArgillic horizon: The zone from 41 to 117 centimeters (16 to 46 inches). (Bt1, Bt2, and Bt3 horizons)\nRedoximorphic concentrations: The zone from 102 to 152 centimeters (40 to 60 inches). (Bt3 and 2BC horizons)\nLithologic discontinuity: at the upper boundary of the 2BC horizon.\nKeys to Taxonomy: Twelth Edition, 2014." + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are: Mollic epipedon: The zone from 0 to 41 centimeters (0 to 16 inches). (A and BA horizons)\nArgillic horizon: The zone from 41 to 117 centimeters (16 to 46 inches). (Bt1, Bt2, and Bt3 horizons)\nRedoximorphic concentrations: The zone from 102 to 152 centimeters (40 to 60 inches). (Bt3 and 2BC horizons)\nLithologic discontinuity: at the upper boundary of the 2BC horizon.\nKeys to Taxonomy: Twelth Edition, 2014.\n04/2013 DJK - Updated to meet current MO5 standards (Tech Note 1, revision 4). Added metric conversions, updated climate, and updated landform positions. Added elevation to typical pedon. Added quad and lat/long to type location. Added clay and sand contents, rock fragments, calcium carbonate equivalent, redox to RIC. Added a BA section to RIC. Added Lasita to competing series. Edited parent material and climate in geographic setting. Updated geographically associated soils (deleted Hastings, Hedville, and Hobbs). Changed permeability to Ksat. Added LRR and MLRA to distribution and extent. Added redox and lithologic discontinuity to remarks section. Added KSSL characterization to additional data." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/M/MANASTASH.json b/inst/extdata/OSD/M/MANASTASH.json index b8f42746ae..7e92a8387b 100644 --- a/inst/extdata/OSD/M/MANASTASH.json +++ b/inst/extdata/OSD/M/MANASTASH.json @@ -10,8 +10,8 @@ "content": "TAXONOMIC CLASS: Fine, smectitic, mesic Abruptic Argiduridic Durixerolls" }, "TYPICAL PEDON": { - "section": "TYPICAL PEDON & Typical pedon revision 10/2005 based on SSPL documention and updated modal pedon description.", - "content": "TYPICAL PEDON: Manastash loam - irrigated pasture, on a 2 percent slope at an elevation of 1,730 feet. The soil was moist when described. (Colors are for dry soil unless otherwise stated.)\nAp--0 to 5 inches; brown (10YR 4/3) loam, very dark grayish brown (10YR 3/2) moist; moderate medium platy structure; slightly hard, friable, nonsticky and slightly plastic; many very fine, fine and common medium roots; common fine tubular pores; neutral (pH 7.0); clear wavy boundary. (3 to 7 inches thick)\nAB--5 to 10 inches; brown (10YR 5/3) loam, dark brown (10YR 3/3) moist; moderate fine subangular blocky structure; slightly hard, friable, slightly sticky and slightly plastic; common very fine, fine roots; common very fine irregular pores; neutral (pH 7.0); abrupt wavy boundary. (0 to 10 inches thick)\nBt1--10 to 15 inches; brown (10YR 5/3) loam, dark brown (10YR 3/3) moist; moderate fine and medium subangular blocky structure; slightly hard, friable, slightly sticky and slightly plastic; common very fine, fine roots; common very fine irregular pores; few faint clay films on faces of peds; neutral (pH 7.0); abrupt wavy boundary. (5 to 10 inches thick)\nBt2--15 to 22 inches; dark yellowish brown (10YR 4/4) clay, dark yellowish brown (10YR 3/4) moist; strong medium prismatic structure parting to strong fine and medium angular blocky; very hard, very firm, very sticky and very plastic; common very fine, fine roots; common very fine irregular pores; many distinct clay films on faces of peds; 5 percent gravel and 5 percent cobbles; moderately alkaline (pH 8.0); clear wavy boundary. (7 to 17 inches thick.)\nBtk--22 to 25 inches; brown (7.5YR 4/4) gravelly clay, dark brown (7.5YR 3/4) moist; strong fine and medium angular blocky structure; very hard, firm, sticky and plastic; many very fine, fine roots; violently effervescent; lime segregated in many large irregular soft masses; common distinct clay films on faces of peds; 10 percent gravel and 5 percent cobbles; moderately alkaline (pH 8.2); clear wavy boundary. (0 to 6 inches thick)\n2Bkqm1--25 to 42 inches; white (10YR 8/1) indurated lime-silica cemented very cobbly duripan, pale brown (10YR 6/3) moist; impervious to roots and water; violently effervescent; 30 percent imbedded gravel, 30 percent imbedded cobbles; grading to strongly cemented below 3 1/2 feet.\n2Bkqm2--42 to 60 inches; moderately cemented very gravelly sandy loam & Typical pedon revision 10/2005 based on SSPL documention and updated modal pedon description." + "section": "TYPICAL PEDON", + "content": "TYPICAL PEDON: Manastash loam - irrigated pasture, on a 2 percent slope at an elevation of 1,730 feet. The soil was moist when described. (Colors are for dry soil unless otherwise stated.)\nAp--0 to 5 inches; brown (10YR 4/3) loam, very dark grayish brown (10YR 3/2) moist; moderate medium platy structure; slightly hard, friable, nonsticky and slightly plastic; many very fine, fine and common medium roots; common fine tubular pores; neutral (pH 7.0); clear wavy boundary. (3 to 7 inches thick)\nAB--5 to 10 inches; brown (10YR 5/3) loam, dark brown (10YR 3/3) moist; moderate fine subangular blocky structure; slightly hard, friable, slightly sticky and slightly plastic; common very fine, fine roots; common very fine irregular pores; neutral (pH 7.0); abrupt wavy boundary. (0 to 10 inches thick)\nBt1--10 to 15 inches; brown (10YR 5/3) loam, dark brown (10YR 3/3) moist; moderate fine and medium subangular blocky structure; slightly hard, friable, slightly sticky and slightly plastic; common very fine, fine roots; common very fine irregular pores; few faint clay films on faces of peds; neutral (pH 7.0); abrupt wavy boundary. (5 to 10 inches thick)\nBt2--15 to 22 inches; dark yellowish brown (10YR 4/4) clay, dark yellowish brown (10YR 3/4) moist; strong medium prismatic structure parting to strong fine and medium angular blocky; very hard, very firm, very sticky and very plastic; common very fine, fine roots; common very fine irregular pores; many distinct clay films on faces of peds; 5 percent gravel and 5 percent cobbles; moderately alkaline (pH 8.0); clear wavy boundary. (7 to 17 inches thick.)\nBtk--22 to 25 inches; brown (7.5YR 4/4) gravelly clay, dark brown (7.5YR 3/4) moist; strong fine and medium angular blocky structure; very hard, firm, sticky and plastic; many very fine, fine roots; violently effervescent; lime segregated in many large irregular soft masses; common distinct clay films on faces of peds; 10 percent gravel and 5 percent cobbles; moderately alkaline (pH 8.2); clear wavy boundary. (0 to 6 inches thick)\n2Bkqm1--25 to 42 inches; white (10YR 8/1) indurated lime-silica cemented very cobbly duripan, pale brown (10YR 6/3) moist; impervious to roots and water; violently effervescent; 30 percent imbedded gravel, 30 percent imbedded cobbles; grading to strongly cemented below 3 1/2 feet.\n2Bkqm2--42 to 60 inches; moderately cemented very gravelly sandy loam" }, "TYPE LOCATION": { "section": "TYPE LOCATION", @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nmollic epipedon - the zone from the surface to 15 inches\nargillic horizon - the zone from 10 to 25 inches\nduripan - the zone beginning at 25 inches.\npscs - the zone from 10 to 25 inches" + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nmollic epipedon - the zone from the surface to 15 inches\nargillic horizon - the zone from 10 to 25 inches\nduripan - the zone beginning at 25 inches.\npscs - the zone from 10 to 25 inches\nTypical pedon revision 10/2005 based on SSPL documention and updated modal pedon description." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", @@ -230,7 +230,7 @@ "eff_class": "NA", "distinctness": "NA", "topography": "NA", - "narrative": "2Bkqm2--42 to 60 inches; moderately cemented very gravelly sandy loam & Typical pedon revision 10/2005 based on SSPL documention and updated modal pedon description." + "narrative": "2Bkqm2--42 to 60 inches; moderately cemented very gravelly sandy loam" } ] ] diff --git a/inst/extdata/OSD/M/MANOKIN.json b/inst/extdata/OSD/M/MANOKIN.json index 1e6af3e6b4..7d7e4f3d66 100644 --- a/inst/extdata/OSD/M/MANOKIN.json +++ b/inst/extdata/OSD/M/MANOKIN.json @@ -6,8 +6,8 @@ "STATES": "MD", "OVERVIEW": "MLRA(s): 153C, 153D", "TAXONOMIC CLASS": { - "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Fine-loamy, mixed, active, mesic Aquic Hapludults\nDepth Class: Very deep\nDrainage Class (Agricultural): Moderately well drained\nInternal Free Water Occurrence: Moderately deep (20 to 40 inches) and common (3 to 6 months)\nIndex Surface Runoff: Very low\nPermeability: Moderate in the solum and rapid in the underlying material\nLandscape: Coastal plain, upland\nLandform: Interfluves, broad upstream divides, and flats\nHillslope Profile Position:\nGeomorphic Component: Dip, rise and talf\nElevation: 5 to 20 feet\nParent Material: Silty eolian deposits over fluviomarine sediments\nSlope: 0 to 5 percent\nMean Annual Air Temperature (type location near Princess Anne, MD): 57 degrees F.\nMean Annual Precipitation (type location near Princess Anne, MD): 46 inches\nTAXONOMIC CLASS: Fine-loamy, mixed, active, mesic Aquic Hapludults" + "section": "TAXONOMIC CLASS & TAXONOMIC CLASS", + "content": "TAXONOMIC CLASS: Fine-loamy, mixed, active, mesic Aquic Hapludults\nDepth Class: Very deep\nDrainage Class (Agricultural): Moderately well drained\nInternal Free Water Occurrence: Moderately deep (20 to 40 inches) and common (3 to 6 months)\nIndex Surface Runoff: Very low\nPermeability: Moderate in the solum and rapid in the underlying material\nLandscape: Coastal plain, upland\nLandform: Interfluves, broad upstream divides, and flats\nHillslope Profile Position:\nGeomorphic Component: Dip, rise and talf\nElevation: 5 to 20 feet\nParent Material: Silty eolian deposits over fluviomarine sediments\nSlope: 0 to 5 percent\nMean Annual Air Temperature (type location near Princess Anne, MD): 57 degrees F.\nMean Annual Precipitation (type location near Princess Anne, MD): 46 inches & TAXONOMIC CLASS: Fine-loamy, mixed, active, mesic Aquic Hapludults" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", diff --git a/inst/extdata/OSD/M/MATUNUCK.json b/inst/extdata/OSD/M/MATUNUCK.json index 4772435098..c8c641e4e0 100644 --- a/inst/extdata/OSD/M/MATUNUCK.json +++ b/inst/extdata/OSD/M/MATUNUCK.json @@ -10,8 +10,8 @@ "content": "TAXONOMIC CLASS: Sandy, mixed, mesic Histic Sulfaquents" }, "TYPICAL PEDON": { - "section": "TYPICAL PEDON & The lab and/or field method for total salts in the Typical Pedon is not known but is retained for historical purposes. Total salt content was previously reported in the RIC is generally more than 10,000 ppm, but ranges from 1,000 through 40,000 ppm.", - "content": "TYPICAL PEDON: Matunuck mucky peat - salt grass tidal marsh, undrained. (Colors are for moist soil unless otherwise noted.)\nOe--0 to 30 cm; very dark gray (10YR 3/1) mucky peat, gray (10YR 6/1) dry; 65 percent fiber, 25 percent rubbed; dense mat of roots, stems, and leaves; massive; many very fine, fine, and medium roots; fibers herbaceous; admixtures of fine and medium sand; 55 percent organic matter; total salts 25,000 ppm; slightly acid; abrupt smooth boundary. (20 to 40 cm thick)\nCg1--30 to 45 cm; gray (10YR 5/1) sand, gray (5Y 6/1) dry; thin lenses of very dark grayish brown organic materials; single grain; loose; common fine and medium roots; total salts 20,000 ppm; neutral; clear wavy boundary. (0 to 25 cm thick)\nCg2--45 to 182 cm; gray (2.5Y 5/1) sand, gray (5Y 6/1) dry; single grain; loose; total salts 20,000 ppm; neutral. & The lab and/or field method for total salts in the Typical Pedon is not known but is retained for historical purposes. Total salt content was previously reported in the RIC is generally more than 10,000 ppm, but ranges from 1,000 through 40,000 ppm." + "section": "TYPICAL PEDON", + "content": "TYPICAL PEDON: Matunuck mucky peat - salt grass tidal marsh, undrained. (Colors are for moist soil unless otherwise noted.)\nOe--0 to 30 cm; very dark gray (10YR 3/1) mucky peat, gray (10YR 6/1) dry; 65 percent fiber, 25 percent rubbed; dense mat of roots, stems, and leaves; massive; many very fine, fine, and medium roots; fibers herbaceous; admixtures of fine and medium sand; 55 percent organic matter; total salts 25,000 ppm; slightly acid; abrupt smooth boundary. (20 to 40 cm thick)\nCg1--30 to 45 cm; gray (10YR 5/1) sand, gray (5Y 6/1) dry; thin lenses of very dark grayish brown organic materials; single grain; loose; common fine and medium roots; total salts 20,000 ppm; neutral; clear wavy boundary. (0 to 25 cm thick)\nCg2--45 to 182 cm; gray (2.5Y 5/1) sand, gray (5Y 6/1) dry; single grain; loose; total salts 20,000 ppm; neutral." }, "TYPE LOCATION": { "section": "TYPE LOCATION", @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon include:\n1. Histic epipedon - the zone from 0 to 30 cm (Oe horizon).\n2. Sandy particle-size class - the control section is from 30 to 106 cm (C horizon).\n3. Sulfaquents feature - sulfidic materials are within (50 cm of the mineral soil surface). New pedons should include incubation pH measurements to determine if horizons should receive a 'se' subordinate distinction due to sulfate content.\n4. Reaction (pH value) is more than 4.5 throughout the control section." + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon include:\n1. Histic epipedon - the zone from 0 to 30 cm (Oe horizon).\n2. Sandy particle-size class - the control section is from 30 to 106 cm (C horizon).\n3. Sulfaquents feature - sulfidic materials are within (50 cm of the mineral soil surface). New pedons should include incubation pH measurements to determine if horizons should receive a 'se' subordinate distinction due to sulfate content.\n4. Reaction (pH value) is more than 4.5 throughout the control section.\nThe lab and/or field method for total salts in the Typical Pedon is not known but is retained for historical purposes. Total salt content was previously reported in the RIC is generally more than 10,000 ppm, but ranges from 1,000 through 40,000 ppm." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", @@ -138,7 +138,7 @@ "eff_class": "NA", "distinctness": "NA", "topography": "NA", - "narrative": "Cg2--45 to 182 cm; gray (2.5Y 5/1) sand, gray (5Y 6/1) dry; single grain; loose; total salts 20,000 ppm; neutral. & The lab and/or field method for total salts in the Typical Pedon is not known but is retained for historical purposes. Total salt content was previously reported in the RIC is generally more than 10,000 ppm, but ranges from 1,000 through 40,000 ppm." + "narrative": "Cg2--45 to 182 cm; gray (2.5Y 5/1) sand, gray (5Y 6/1) dry; single grain; loose; total salts 20,000 ppm; neutral." } ] ] diff --git a/inst/extdata/OSD/N/NARROW_CAPE.json b/inst/extdata/OSD/N/NARROW_CAPE.json index 96802cb944..2f9810dbd8 100644 --- a/inst/extdata/OSD/N/NARROW_CAPE.json +++ b/inst/extdata/OSD/N/NARROW_CAPE.json @@ -26,8 +26,8 @@ "content": "COMPETING SERIES: These is the Koniag competing series.\nKoniag soils lack recent volcanic ashy surface horizons and occur on similar landform positions." }, "GEOGRAPHIC SETTING": { - "section": "GEOGRAPHIC SETTING", - "content": "GEOGRAPHIC SETTING:\nElevation: 5 to 365 meters (15 to 1200 feet)\nParent material: moderately decomposed herbaceous organic material over medial silty volcanic ash over gravelly loamy till\nLandform: plains and hills\nSlope: 15 to 60 percent\nMean annual temperature: 0 to 6 degrees C. (32 to 43 degrees F.)\nMean annual precipitation: 600 to 2000 mm (23 to 79 in)\nFrost free period: 20 to 50 days\nGEOGRAPHIC SETTING:\nDepth class: very deep\nDrainage class: well drained\nParent material: volcanic ash over coarse-loamy eolian deposits\nLandform: hills and plains\nSlopes: 3 to 15 percent\nMean annual precipitation: 600 to 3000 mm (23 to 118 in)\nMean annual temperature: 0 to 6 degrees C. (32 to 43 degrees F.)\nFrost-free season: 20 to 50 days" + "section": "GEOGRAPHIC SETTING & GEOGRAPHIC SETTING", + "content": "GEOGRAPHIC SETTING:\nElevation: 5 to 365 meters (15 to 1200 feet)\nParent material: moderately decomposed herbaceous organic material over medial silty volcanic ash over gravelly loamy till\nLandform: plains and hills\nSlope: 15 to 60 percent\nMean annual temperature: 0 to 6 degrees C. (32 to 43 degrees F.)\nMean annual precipitation: 600 to 2000 mm (23 to 79 in)\nFrost free period: 20 to 50 days & GEOGRAPHIC SETTING:\nDepth class: very deep\nDrainage class: well drained\nParent material: volcanic ash over coarse-loamy eolian deposits\nLandform: hills and plains\nSlopes: 3 to 15 percent\nMean annual precipitation: 600 to 3000 mm (23 to 118 in)\nMean annual temperature: 0 to 6 degrees C. (32 to 43 degrees F.)\nFrost-free season: 20 to 50 days" }, "GEOGRAPHICALLY ASSOCIATED SOILS": { "section": "GEOGRAPHICALLY ASSOCIATED SOILS", diff --git a/inst/extdata/OSD/O/OMRO.json b/inst/extdata/OSD/O/OMRO.json index 50e986d9bd..a7949cad71 100644 --- a/inst/extdata/OSD/O/OMRO.json +++ b/inst/extdata/OSD/O/OMRO.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: This soil was mapped as inclusions of the Kewaunee series in adjacent counties to Winnebago County." + "content": "REMARKS: This soil was mapped as inclusions of the Kewaunee series in adjacent counties to Winnebago County.\n11/04 4700 acres with a well drained typical pedon were correlated as a temperature taxadjunct in Door County, WI because they are in the frigid temperature zone. A new series is needed.\n11/04 3020 acres are correlated in Kewaunee County, WI where the well drained typical pedon has a glossic horizon (Haplic Glossudalf). A new series is needed.\nDiagnostic horizons and features recognized in this pedon are: ochric epipedon - 0 to 20 cm (0 to 8 inches) (Ap); argillic horizon - 20 to 71 cm (8 to 28 inches) (Bt1, Bt2, Bt3); Oxyaquic feature redox accumulations and saturation within 102 cm (40 inches)." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/O/OTTOKEE.json b/inst/extdata/OSD/O/OTTOKEE.json index e6b61da520..01268792a3 100644 --- a/inst/extdata/OSD/O/OTTOKEE.json +++ b/inst/extdata/OSD/O/OTTOKEE.json @@ -10,8 +10,8 @@ "content": "TAXONOMIC CLASS: Mixed, mesic Aquic Udipsamments" }, "TYPICAL PEDON": { - "section": "TYPICAL PEDON & Evaluation of Type Location site and additional Typical Pedon sites throughout MLRA 99 in Ohio supports the absence of lamellae within the series control section. The banding that occurs in these soils have increased concentrations of iron and magnetite but not clay. Further investigation is needed in areas mapped as Ottokee soils in Michigan to determine if lamellae are present.", - "content": "TYPICAL PEDON: Ottokee fine sand, on a north-facing, convex, 2 percent slope in a cultivated field at an elevation of 680 feet above m.s.l. (Colors are for moist soil unless otherwise stated.)\nAp--0 to 8 inches; very dark grayish brown (10YR 3/2) fine sand, dark grayish brown (10YR 4/2) rubbed, light brownish gray (10YR 6/2) dry; weak fine granular structure; very friable; slightly acid; abrupt smooth boundary. (7 to 10 inches thick)\nBw1--8 to 22 inches; yellowish brown (10YR 5/4) fine sand; single grain; loose; slightly acid; clear wavy boundary.\nBw2--22 to 27 inches; light yellowish brown (10YR 6/4) fine sand; single grain; loose; common fine faint pale brown (10YR 6/3) iron depletions in the matrix; many fine prominent yellowish red (5YR 5/8 and 4/6) masses of iron accumulation in the matrix; many dark iron and manganese oxide concretions in the matrix; slightly acid; gradual wavy boundary.\nBw3--27 to 33 inches; pale brown (10YR 6/3) fine sand; single grain; loose; few fine distinct gray (10YR 6/1) iron depletions in the matrix; few to many, fine and medium prominent strong brown (7.5YR 5/8) masses of iron accumulation in the matrix; slightly acid; clear wavy boundary.\nBg1--33 to 39 inches; light brownish gray (10YR 6/2) fine sand; single grain; loose; few to many, fine and medium prominent yellowish brown (10YR 5/8) and brownish yellow (10YR 6/8) masses of iron accumulation in the matrix; neutral; abrupt irregular boundary with tongues extending into the horizon below.\nBg2--39 to 60 inches; light brownish gray (10YR 6/2) loamy fine sand in the upper part and pale brown (10YR 6/3) loamy fine sand in the lower part; single grain; loose; weak fine subangular blocky structure; massive in places; very friable; neutral; clear wavy boundary. (Combined thickness of the Bw or Bg horizon is 30 to 55 inches.)\nCg--60 to 80 inches; gray (10YR 5/1) fine sand; single grain; loose; many medium prominent light olive brown (2.5Y 5/6) masses of iron accumulation in the matrix; strongly effervescent; moderately alkaline. & Evaluation of Type Location site and additional Typical Pedon sites throughout MLRA 99 in Ohio supports the absence of lamellae within the series control section. The banding that occurs in these soils have increased concentrations of iron and magnetite but not clay. Further investigation is needed in areas mapped as Ottokee soils in Michigan to determine if lamellae are present." + "section": "TYPICAL PEDON", + "content": "TYPICAL PEDON: Ottokee fine sand, on a north-facing, convex, 2 percent slope in a cultivated field at an elevation of 680 feet above m.s.l. (Colors are for moist soil unless otherwise stated.)\nAp--0 to 8 inches; very dark grayish brown (10YR 3/2) fine sand, dark grayish brown (10YR 4/2) rubbed, light brownish gray (10YR 6/2) dry; weak fine granular structure; very friable; slightly acid; abrupt smooth boundary. (7 to 10 inches thick)\nBw1--8 to 22 inches; yellowish brown (10YR 5/4) fine sand; single grain; loose; slightly acid; clear wavy boundary.\nBw2--22 to 27 inches; light yellowish brown (10YR 6/4) fine sand; single grain; loose; common fine faint pale brown (10YR 6/3) iron depletions in the matrix; many fine prominent yellowish red (5YR 5/8 and 4/6) masses of iron accumulation in the matrix; many dark iron and manganese oxide concretions in the matrix; slightly acid; gradual wavy boundary.\nBw3--27 to 33 inches; pale brown (10YR 6/3) fine sand; single grain; loose; few fine distinct gray (10YR 6/1) iron depletions in the matrix; few to many, fine and medium prominent strong brown (7.5YR 5/8) masses of iron accumulation in the matrix; slightly acid; clear wavy boundary.\nBg1--33 to 39 inches; light brownish gray (10YR 6/2) fine sand; single grain; loose; few to many, fine and medium prominent yellowish brown (10YR 5/8) and brownish yellow (10YR 6/8) masses of iron accumulation in the matrix; neutral; abrupt irregular boundary with tongues extending into the horizon below.\nBg2--39 to 60 inches; light brownish gray (10YR 6/2) loamy fine sand in the upper part and pale brown (10YR 6/3) loamy fine sand in the lower part; single grain; loose; weak fine subangular blocky structure; massive in places; very friable; neutral; clear wavy boundary. (Combined thickness of the Bw or Bg horizon is 30 to 55 inches.)\nCg--60 to 80 inches; gray (10YR 5/1) fine sand; single grain; loose; many medium prominent light olive brown (2.5Y 5/6) masses of iron accumulation in the matrix; strongly effervescent; moderately alkaline." }, "TYPE LOCATION": { "section": "TYPE LOCATION", @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are: ochric epipedon - the zone from 0 to 8 inches (Ap); aquic conditions chroma of 2 or less in the zone from 27 to 80 inches; udic moisture regime." + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are: ochric epipedon - the zone from 0 to 8 inches (Ap); aquic conditions chroma of 2 or less in the zone from 27 to 80 inches; udic moisture regime.\nEvaluation of Type Location site and additional Typical Pedon sites throughout MLRA 99 in Ohio supports the absence of lamellae within the series control section. The banding that occurs in these soils have increased concentrations of iron and magnetite but not clay. Further investigation is needed in areas mapped as Ottokee soils in Michigan to determine if lamellae are present." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", @@ -230,7 +230,7 @@ "eff_class": "strongly effervescent", "distinctness": "NA", "topography": "NA", - "narrative": "Cg--60 to 80 inches; gray (10YR 5/1) fine sand; single grain; loose; many medium prominent light olive brown (2.5Y 5/6) masses of iron accumulation in the matrix; strongly effervescent; moderately alkaline. & Evaluation of Type Location site and additional Typical Pedon sites throughout MLRA 99 in Ohio supports the absence of lamellae within the series control section. The banding that occurs in these soils have increased concentrations of iron and magnetite but not clay. Further investigation is needed in areas mapped as Ottokee soils in Michigan to determine if lamellae are present." + "narrative": "Cg--60 to 80 inches; gray (10YR 5/1) fine sand; single grain; loose; many medium prominent light olive brown (2.5Y 5/6) masses of iron accumulation in the matrix; strongly effervescent; moderately alkaline." } ] ] diff --git a/inst/extdata/OSD/P/PAMLICO.json b/inst/extdata/OSD/P/PAMLICO.json index 71e6c272e1..cc08e2c6a8 100644 --- a/inst/extdata/OSD/P/PAMLICO.json +++ b/inst/extdata/OSD/P/PAMLICO.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Pamlico muck, as mapped in the past, included a very wide range of conditions. The concept expressed in this description is restricted in thickness, degree of decomposition and nature of underlying materials.\nDiagnostic horizons and features recognized in the typical pedon are:\nOrganic materials (terric) - the zone from the surface to a depth of 30 inches (the Oi, Oa1, and Oa2 horizons)\nSandy particle-size class - mineral material within a depth of 51 inches that has weighted average of the sandy particle-size class in the upper 12 inches of the mineral material or within the control section (51 inches), whichever is thicker (the Cg horizon)\nMLRA(S): 152A, 153A, 153B, 133A" + "content": "REMARKS: Pamlico muck, as mapped in the past, included a very wide range of conditions. The concept expressed in this description is restricted in thickness, degree of decomposition and nature of underlying materials.\nDiagnostic horizons and features recognized in the typical pedon are:\nOrganic materials (terric) - the zone from the surface to a depth of 30 inches (the Oi, Oa1, and Oa2 horizons)\nSandy particle-size class - mineral material within a depth of 51 inches that has weighted average of the sandy particle-size class in the upper 12 inches of the mineral material or within the control section (51 inches), whichever is thicker (the Cg horizon)\nMLRA(S): 152A, 153A, 153B, 133A\nSIR(S): NC0050, NC0154 (LOAMY SUBSTRATUM), NC0155 (PONDED),\nNC0159 (FLOODED), NC0270 (PONDED, LOAMY SUBSTRATUM)\nREVISED=6/10/96, MHC" }, "ADDITIONAL DATA": { "section": "TABULAR SERIES DATA", diff --git a/inst/extdata/OSD/P/PAWCATUCK.json b/inst/extdata/OSD/P/PAWCATUCK.json index 4e605e49a7..56e4b3e085 100644 --- a/inst/extdata/OSD/P/PAWCATUCK.json +++ b/inst/extdata/OSD/P/PAWCATUCK.json @@ -10,8 +10,8 @@ "content": "TAXONOMIC CLASS: Sandy or sandy-skeletal, mixed, euic, mesic Terric Sulfihemists" }, "TYPICAL PEDON": { - "section": "TYPICAL PEDON & The lab and/or field method for total salts in the Typical Pedon is not known but is retained for historical purposes. Total salt content previously reported in the RIC is generally more than 10,000 ppm, but total salt content ranges from 1,000 to 40,000 ppm.", - "content": "TYPICAL PEDON: Pawcatuck mucky peat - salt grass tidal marsh, undrained. (Colors are for moist soil, unless otherwise noted.)\nOese1--0 to 30 centimeters; very dark gray (10YR 3/1) mucky peat, dark grayish brown (10YR 4/2) dry; 65 percent fiber, 30 percent rubbed; H5 von Post humification; dense mat of roots, stems and leaves; slightly sticky; many very fine, fine and medium roots; fibers herbaceous; thin lenses and coatings of silt; 57 percent organic matter; total salts 19,500 ppm; slightly acid (pH 6.3), extremely acid (pH 3.9) oxidized pH; clear wavy boundary.\nOese2--30 to 102 centimeters; black (10YR 2/1) mucky peat, very dark gray (10YR 3/1) dry; 50 percent fiber, 25 percent rubbed; H5 von Post humification; slightly sticky; few very fine, fine and medium roots; fibers herbaceous; 54 percent organic matter; total salts 22,900 ppm; slightly acid (pH 6.3), very strongly acid (pH 4.8) oxidized pH; gradual wavy boundary.\nOese3--102 to 117 centimeters; black (10YR 2/1) moist and dry mucky peat; 40 percent fiber, 25 percent rubbed; H5 von Post humification; slightly sticky; fibers herbaceous; 27 percent organic matter; total salts 18,850 ppm; slightly acid (pH 6.3), extremely acid (pH 3.7) oxidized pH; clear wavy boundary. (Combined thickness of Oese horizons in 40 to 125 centimeters).\nCseg1--117 to 127 centimeters; gray (N 5/) very fine sandy loam, gray (10YR 5/1) dry; massive; friable; slightly sticky; 10 percent organic matter; total salts 20,000 ppm; slightly acid (pH 6.3), extremely acid (pH 4.0) oxidized pH; clear wavy boundary.\nCseg2--127 to 200 centimeters; black (10YR 2/1) loamy sand, dark gray (10YR 4/1) dry; single grain; loose; 10 percent gravel; total salts 20,000 ppm; slightly acid (pH 6.3), ultra acid (pH 2.8) oxidized pH. (Combined thickness of Cseg horizons is 20 to 75 centimeters). & The lab and/or field method for total salts in the Typical Pedon is not known but is retained for historical purposes. Total salt content previously reported in the RIC is generally more than 10,000 ppm, but total salt content ranges from 1,000 to 40,000 ppm.\nDiagnostic horizons and features in this pedon include:\n1. Histosols--have organic materials that total 40 centimeters or more between the soil surface and a depth of 50 centimeters - the zone from a depth of 0 to 117 centimeters (Oese horizons).\n2. Hypersulfidic materials--the zone from 0 to 200 centimeters;\n3. Reaction (pH value) is more than 4.5 throughout the control section." + "section": "TYPICAL PEDON", + "content": "TYPICAL PEDON: Pawcatuck mucky peat - salt grass tidal marsh, undrained. (Colors are for moist soil, unless otherwise noted.)\nOese1--0 to 30 centimeters; very dark gray (10YR 3/1) mucky peat, dark grayish brown (10YR 4/2) dry; 65 percent fiber, 30 percent rubbed; H5 von Post humification; dense mat of roots, stems and leaves; slightly sticky; many very fine, fine and medium roots; fibers herbaceous; thin lenses and coatings of silt; 57 percent organic matter; total salts 19,500 ppm; slightly acid (pH 6.3), extremely acid (pH 3.9) oxidized pH; clear wavy boundary.\nOese2--30 to 102 centimeters; black (10YR 2/1) mucky peat, very dark gray (10YR 3/1) dry; 50 percent fiber, 25 percent rubbed; H5 von Post humification; slightly sticky; few very fine, fine and medium roots; fibers herbaceous; 54 percent organic matter; total salts 22,900 ppm; slightly acid (pH 6.3), very strongly acid (pH 4.8) oxidized pH; gradual wavy boundary.\nOese3--102 to 117 centimeters; black (10YR 2/1) moist and dry mucky peat; 40 percent fiber, 25 percent rubbed; H5 von Post humification; slightly sticky; fibers herbaceous; 27 percent organic matter; total salts 18,850 ppm; slightly acid (pH 6.3), extremely acid (pH 3.7) oxidized pH; clear wavy boundary. (Combined thickness of Oese horizons in 40 to 125 centimeters).\nCseg1--117 to 127 centimeters; gray (N 5/) very fine sandy loam, gray (10YR 5/1) dry; massive; friable; slightly sticky; 10 percent organic matter; total salts 20,000 ppm; slightly acid (pH 6.3), extremely acid (pH 4.0) oxidized pH; clear wavy boundary.\nCseg2--127 to 200 centimeters; black (10YR 2/1) loamy sand, dark gray (10YR 4/1) dry; single grain; loose; 10 percent gravel; total salts 20,000 ppm; slightly acid (pH 6.3), ultra acid (pH 2.8) oxidized pH. (Combined thickness of Cseg horizons is 20 to 75 centimeters)." }, "TYPE LOCATION": { "section": "TYPE LOCATION", @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: This revision reflects general updating, reformatting, and inclusion of blue carbon data. Pawcatuck soils have been mapped as Tidal marsh, undifferentiated. Some of the Pawcatuck soils were classified and mapped at the Great Group or Subgroup level. Pawcatuck series was originally described as consisting of fibric organic materials. Current procedures for estimating fibers indicate that the materials are dominantly hemic. These soils become extremely acid when drained." + "content": "REMARKS: This revision reflects general updating, reformatting, and inclusion of blue carbon data. Pawcatuck soils have been mapped as Tidal marsh, undifferentiated. Some of the Pawcatuck soils were classified and mapped at the Great Group or Subgroup level. Pawcatuck series was originally described as consisting of fibric organic materials. Current procedures for estimating fibers indicate that the materials are dominantly hemic. These soils become extremely acid when drained.\nThe lab and/or field method for total salts in the Typical Pedon is not known but is retained for historical purposes. Total salt content previously reported in the RIC is generally more than 10,000 ppm, but total salt content ranges from 1,000 to 40,000 ppm.\nDiagnostic horizons and features in this pedon include:\n1. Histosols--have organic materials that total 40 centimeters or more between the soil surface and a depth of 50 centimeters - the zone from a depth of 0 to 117 centimeters (Oese horizons).\n2. Hypersulfidic materials--the zone from 0 to 200 centimeters;\n3. Reaction (pH value) is more than 4.5 throughout the control section." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", @@ -184,30 +184,7 @@ "eff_class": "NA", "distinctness": "NA", "topography": "NA", - "narrative": "Cseg2--127 to 200 centimeters; black (10YR 2/1) loamy sand, dark gray (10YR 4/1) dry; single grain; loose; 10 percent gravel; total salts 20,000 ppm; slightly acid (pH 6.3), ultra acid (pH 2.8) oxidized pH. (Combined thickness of Cseg horizons is 20 to 75 centimeters). & The lab and/or field method for total salts in the Typical Pedon is not known but is retained for historical purposes. Total salt content previously reported in the RIC is generally more than 10,000 ppm, but total salt content ranges from 1,000 to 40,000 ppm. Diagnostic horizons and features in this pedon include:" - }, - { - "name": "centimeters", - "top": "NA", - "bottom": "NA", - "dry_hue": "NA", - "dry_value": "NA", - "dry_chroma": "NA", - "moist_hue": "NA", - "moist_value": "NA", - "moist_chroma": "NA", - "texture_class": "NA", - "structure": "NA", - "dry_rupture": "NA", - "moist_rupture": "NA", - "coherence": "NA", - "cf_class": "NA", - "pH": "NA", - "pH_class": "NA", - "eff_class": "NA", - "distinctness": "NA", - "topography": "NA", - "narrative": "1. Histosols--have organic materials that total 40 centimeters or more between the soil surface and a depth of 50 centimeters - the zone from a depth of 0 to 117 centimeters (Oese horizons)." + "narrative": "Cseg2--127 to 200 centimeters; black (10YR 2/1) loamy sand, dark gray (10YR 4/1) dry; single grain; loose; 10 percent gravel; total salts 20,000 ppm; slightly acid (pH 6.3), ultra acid (pH 2.8) oxidized pH. (Combined thickness of Cseg horizons is 20 to 75 centimeters)." } ] ] diff --git a/inst/extdata/OSD/P/PIERRE.json b/inst/extdata/OSD/P/PIERRE.json index af33e1dfd8..1dab4c29af 100644 --- a/inst/extdata/OSD/P/PIERRE.json +++ b/inst/extdata/OSD/P/PIERRE.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nOchric epipedon - 0 to 13 cm (0 to 5 inches); (A horizon)\nCambic horizon - 13 to 66 cm (5 to 26 inches); (Bw and Bk horizons)\nIdentifiable secondary carbonates - 49 to 66 cm (19 to 26 inches); (Bk and BCk horizons)\nParalithic contact - at 79 cm (31 inches); (upper boundary of Cr horizon)\nParalithic materials- 79 to 200 cm (31 to 80 inches); (Cr horizon)\nThe series taxonomic class is changed to Torrertic Haplustepts. Field observations of Pierre soils failed to reveal the presence of slickensides or wedge-shaped aggregates associated with Vertisols." + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nOchric epipedon - 0 to 13 cm (0 to 5 inches); (A horizon)\nCambic horizon - 13 to 66 cm (5 to 26 inches); (Bw and Bk horizons)\nIdentifiable secondary carbonates - 49 to 66 cm (19 to 26 inches); (Bk and BCk horizons)\nParalithic contact - at 79 cm (31 inches); (upper boundary of Cr horizon)\nParalithic materials- 79 to 200 cm (31 to 80 inches); (Cr horizon)\nThe series taxonomic class is changed to Torrertic Haplustepts. Field observations of Pierre soils failed to reveal the presence of slickensides or wedge-shaped aggregates associated with Vertisols.\nThe typical pedon for the series is moved from Haakon County, South Dakota (MLRA 63A) to Custer County (MLRA 60A) with this update. MLRA 63A is typic-ustic.\nTaxonomic Version: Keys to Soil Taxonomy, Twelvth Edition, 2013" }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/P/PINEKNOT.json b/inst/extdata/OSD/P/PINEKNOT.json index ff97ab4fab..088b3b5dd5 100644 --- a/inst/extdata/OSD/P/PINEKNOT.json +++ b/inst/extdata/OSD/P/PINEKNOT.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nParticle-size control section - the zone from a depth of 10 to 100 centimeters.\nSeries control section - 0 to 200 centimeters.\nDiagnostic horizons and features recognized in this pedon include:\nOchric epipedon - the zone from the surface of the soil to a depth of 5 to 33 centimeters (A, E, EA, AE, AB, BA, BE horizons).\nAlbic horizon, where present the zone from 10 to 41 centimeters.\nArgillic horizon - the zone from 15 to 200 centimeters (Bt and 2Bt and 3Bt horizons).\nStrongly contrasting particle size class (lithologic discontinuity) occurs at a depth of 39 centimeters for the typical pedon. The range is from 28 to 76 centimeters and the average is 45 centimeters.\nThe typical pedon has a base saturation of 17 percent at the critical depth. The base saturation for this series ranges from 6 to 20 percent with an average of 12 percent." + "content": "REMARKS:\nParticle-size control section - the zone from a depth of 10 to 100 centimeters.\nSeries control section - 0 to 200 centimeters.\nDiagnostic horizons and features recognized in this pedon include:\nOchric epipedon - the zone from the surface of the soil to a depth of 5 to 33 centimeters (A, E, EA, AE, AB, BA, BE horizons).\nAlbic horizon, where present the zone from 10 to 41 centimeters.\nArgillic horizon - the zone from 15 to 200 centimeters (Bt and 2Bt and 3Bt horizons).\nStrongly contrasting particle size class (lithologic discontinuity) occurs at a depth of 39 centimeters for the typical pedon. The range is from 28 to 76 centimeters and the average is 45 centimeters.\nThe typical pedon has a base saturation of 17 percent at the critical depth. The base saturation for this series ranges from 6 to 20 percent with an average of 12 percent.\nPineknot soils were previously mapped as Macedonia, Fanchon and Poynor series. Site and pedon ID 2017MO203204 represents the typical pedon." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/P/PLEVNA.json b/inst/extdata/OSD/P/PLEVNA.json index 1569b78134..a8a1614deb 100644 --- a/inst/extdata/OSD/P/PLEVNA.json +++ b/inst/extdata/OSD/P/PLEVNA.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nMollic epipedon: the zone from 0 to 43 centimeters (0 to 17 inches) (A1, A2)\nCambic horizon: the zone from 43 to 102 centimeters (17 to 40 inches) (Bg)\nAquic conditions: redoximorphic features in the zone from about 25 to 152 centimeters (10 to 60 inches) (A2, Bg, 2C)\nEndo: Apparent water table from the surface to 2 feet\nSeries Interpretation Record: KS0092\nKeys to Soil Taxonomy: Twelfth edition, 2014" + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nMollic epipedon: the zone from 0 to 43 centimeters (0 to 17 inches) (A1, A2)\nCambic horizon: the zone from 43 to 102 centimeters (17 to 40 inches) (Bg)\nAquic conditions: redoximorphic features in the zone from about 25 to 152 centimeters (10 to 60 inches) (A2, Bg, 2C)\nEndo: Apparent water table from the surface to 2 feet\nSeries Interpretation Record: KS0092\nKeys to Soil Taxonomy: Twelfth edition, 2014\n3/2017 BKN Updated intro to current standards. Added elevation and slope to typical pedon. Changed to tabular format. Added in metric units. Added clay content, sand content, and reaction to RIC. Added latitude, longitude, and datum to type location. Updated MAAT and MAP in geographic setting and added in precipitation pattern and FFD. Updated geographically associated soils by removing Cohoctah and adding Ninnescah, Ralsen, and Suckercreek. Changed permeability to Ksat. Added LRR and MLRA to distribution and extent. Added lab data to additional data." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/P/PRATT.json b/inst/extdata/OSD/P/PRATT.json index cc2cf6209a..448b6d3a7e 100644 --- a/inst/extdata/OSD/P/PRATT.json +++ b/inst/extdata/OSD/P/PRATT.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nOchric epipedon: The zone from 0 to 20 centimeters (0 to 8 inches). (Ap)\nArgillic horizon: The zone from 20 to 61 centimeters (8 to 24 inches) and containing lamellae. (Bt)\nKeys to Soil Taxonomy: Twelfth edition, 2014\n2/08/95: Update series for Oklahoma" + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nOchric epipedon: The zone from 0 to 20 centimeters (0 to 8 inches). (Ap)\nArgillic horizon: The zone from 20 to 61 centimeters (8 to 24 inches) and containing lamellae. (Bt)\nKeys to Soil Taxonomy: Twelfth edition, 2014\n2/08/95: Update series for Oklahoma\n1/2017 BKN Added slope range to intro. Added on a north facing, convex, 1 percent slope and at an elevation of 547 meters (1,794 feet) to typical pedon. Added clay and sand content to RIC. Added precipitation pattern to geographic setting. Removed Carway, Carwile, Hayes, Langdon, Shellabarger, Tivoli, Turon, and Warnut soils from geographically associated soils. Changed permeability to saturated hydraulic conductivity." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/Q/QUEPONCO.json b/inst/extdata/OSD/Q/QUEPONCO.json index acedecb031..cb4a2b00e4 100644 --- a/inst/extdata/OSD/Q/QUEPONCO.json +++ b/inst/extdata/OSD/Q/QUEPONCO.json @@ -6,8 +6,8 @@ "STATES": "MD", "OVERVIEW": "MLRA(s): 153C, 153D", "TAXONOMIC CLASS": { - "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Fine-loamy, mixed, semiactive, mesic Typic Hapludults\nDepth Class: Very Deep\nDrainage Class (Agricultural): Well drained\nInternal Free Water Occurrence: Deep (40 to 72 inches)and common (3 to 6 months)\nPermeability: Moderate\nIndex Surface Runoff: Low\nLandscape: Peninsula\nLandform: Interfluves and broad interstream divides\nHillslope Profile Position: Summits, shoulders, and backslope\nGeomorphic Component: Rise and talfs\nParent Material: Loamy fluvial and eolian deposits underlain by sandy and loamy fluvial and marine (fluviomarine) deposits\nSlope: 0 to 5 percent\nElevation (type location): 5 feet\nMean Annual Air Temperature (type location near Princess Anne, MD): 57 degrees F.\nMean Annual Precipitation (type location near Princess Anne, MD): 46 inches\nTAXONOMIC CLASS: Fine-loamy, mixed, semiactive, mesic Typic Hapludults" + "section": "TAXONOMIC CLASS & TAXONOMIC CLASS", + "content": "TAXONOMIC CLASS: Fine-loamy, mixed, semiactive, mesic Typic Hapludults\nDepth Class: Very Deep\nDrainage Class (Agricultural): Well drained\nInternal Free Water Occurrence: Deep (40 to 72 inches)and common (3 to 6 months)\nPermeability: Moderate\nIndex Surface Runoff: Low\nLandscape: Peninsula\nLandform: Interfluves and broad interstream divides\nHillslope Profile Position: Summits, shoulders, and backslope\nGeomorphic Component: Rise and talfs\nParent Material: Loamy fluvial and eolian deposits underlain by sandy and loamy fluvial and marine (fluviomarine) deposits\nSlope: 0 to 5 percent\nElevation (type location): 5 feet\nMean Annual Air Temperature (type location near Princess Anne, MD): 57 degrees F.\nMean Annual Precipitation (type location near Princess Anne, MD): 46 inches & TAXONOMIC CLASS: Fine-loamy, mixed, semiactive, mesic Typic Hapludults" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", diff --git a/inst/extdata/OSD/Q/QUINDOCQUA.json b/inst/extdata/OSD/Q/QUINDOCQUA.json index aeb94196dd..88eca734b6 100644 --- a/inst/extdata/OSD/Q/QUINDOCQUA.json +++ b/inst/extdata/OSD/Q/QUINDOCQUA.json @@ -6,8 +6,8 @@ "STATES": "MD", "OVERVIEW": "MLRA(s): 153C, 153D", "TAXONOMIC CLASS": { - "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Fine-loamy, mixed, active, mesic Typic Endoaquults\nDepth Class: Very Deep\nDrainage Class (Agricultural): Poorly drained\nInternal Free Water Occurrence: Very shallow (0 to 10 inches) and common (3 to 6 months)\nIndex Surface Runoff: Negligible where concave (depressional), to low where nearly level.\nSaturated Hydraulic Conductivity: Moderately high in the subsoil, high and very high in the substratum\nPermeability(obsolete): Moderate in the solum and rapid in the underlying material\nPhysiographic Region: Coastal Plain\nLandscape: Lowlands\nLandform: Interfluves, broad interstream divides, and flats, swales, drainageways\nElevation: 5 to 40 feet (6 feet at type location)\nParent Material: Loamy fluvial and eolian deposits underlain by sandy fluviomarine sediments\nSlope: 0 to 2 percent\nMean Annual Air Temperature (type location near Princess Anne, MD): 57 degrees F.\nMean Annual Precipitation (type location near Princess Anne, MD): 46 inches\nTAXONOMIC CLASS: Fine-loamy, mixed, active, mesic Typic Endoaquults" + "section": "TAXONOMIC CLASS & TAXONOMIC CLASS", + "content": "TAXONOMIC CLASS: Fine-loamy, mixed, active, mesic Typic Endoaquults\nDepth Class: Very Deep\nDrainage Class (Agricultural): Poorly drained\nInternal Free Water Occurrence: Very shallow (0 to 10 inches) and common (3 to 6 months)\nIndex Surface Runoff: Negligible where concave (depressional), to low where nearly level.\nSaturated Hydraulic Conductivity: Moderately high in the subsoil, high and very high in the substratum\nPermeability(obsolete): Moderate in the solum and rapid in the underlying material\nPhysiographic Region: Coastal Plain\nLandscape: Lowlands\nLandform: Interfluves, broad interstream divides, and flats, swales, drainageways\nElevation: 5 to 40 feet (6 feet at type location)\nParent Material: Loamy fluvial and eolian deposits underlain by sandy fluviomarine sediments\nSlope: 0 to 2 percent\nMean Annual Air Temperature (type location near Princess Anne, MD): 57 degrees F.\nMean Annual Precipitation (type location near Princess Anne, MD): 46 inches & TAXONOMIC CLASS: Fine-loamy, mixed, active, mesic Typic Endoaquults" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", diff --git a/inst/extdata/OSD/R/RAUB.json b/inst/extdata/OSD/R/RAUB.json index ba08eae2d1..83d5ad0116 100644 --- a/inst/extdata/OSD/R/RAUB.json +++ b/inst/extdata/OSD/R/RAUB.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nMollic epipedon: from the surface to a depth of 33 cm (Ap, A horizons).\nArgillic horizon: from a depth of 33 to 152 cm (Bt, 2Bt horizons).\nDepth to densic contact: at 152 cm (top of 2Cd horizon).\nAquic conditions: redoximorphic features in all horizons below a depth of 33 cm.\nThis soil is prime farmland where drained." + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nMollic epipedon: from the surface to a depth of 33 cm (Ap, A horizons).\nArgillic horizon: from a depth of 33 to 152 cm (Bt, 2Bt horizons).\nDepth to densic contact: at 152 cm (top of 2Cd horizon).\nAquic conditions: redoximorphic features in all horizons below a depth of 33 cm.\nThis soil is prime farmland where drained.\nRepresentative NASIS data mapunit for the typical pedon is DMU ID 153116 in MO 11." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/R/REZANOF.json b/inst/extdata/OSD/R/REZANOF.json index a3edc94b0c..996e2a032a 100644 --- a/inst/extdata/OSD/R/REZANOF.json +++ b/inst/extdata/OSD/R/REZANOF.json @@ -26,8 +26,8 @@ "content": "COMPETING SERIES: There are no competing series." }, "GEOGRAPHIC SETTING": { - "section": "GEOGRAPHIC SETTING", - "content": "GEOGRAPHIC SETTING:\nElevation: 5 to 365 meters (15 to 1200 feet)\nParent material: moderately decomposed herbaceous organic material over medial silty volcanic ash over gravelly loamy till\nLandform: plains and hills\nSlope: 0 to 20 percent\nMean annual temperature: 0 to 6 degrees C. (32 to 43 degrees F.)\nMean annual precipitation: 600 to 2000 mm (23 to 79 in)\nFrost free period: 20 to 50 days\nGEOGRAPHIC SETTING:\nDepth class: very deep\nDrainage class: well drained\nParent material: moderately decomposed herbaceous organic material over medial silty volcanic ash over gravelly loamy subglacial till\nLandform: plains and hills\nSlopes: 0 to 30 percent\nMean annual precipitation: 700 to 2000 mm (27 to 79 in)\nMean annual temperature: 0 to 6 degrees C. (32 to 43 degrees F.)\nFrost-free season: 20 to 50 days" + "section": "GEOGRAPHIC SETTING & GEOGRAPHIC SETTING", + "content": "GEOGRAPHIC SETTING:\nElevation: 5 to 365 meters (15 to 1200 feet)\nParent material: moderately decomposed herbaceous organic material over medial silty volcanic ash over gravelly loamy till\nLandform: plains and hills\nSlope: 0 to 20 percent\nMean annual temperature: 0 to 6 degrees C. (32 to 43 degrees F.)\nMean annual precipitation: 600 to 2000 mm (23 to 79 in)\nFrost free period: 20 to 50 days & GEOGRAPHIC SETTING:\nDepth class: very deep\nDrainage class: well drained\nParent material: moderately decomposed herbaceous organic material over medial silty volcanic ash over gravelly loamy subglacial till\nLandform: plains and hills\nSlopes: 0 to 30 percent\nMean annual precipitation: 700 to 2000 mm (27 to 79 in)\nMean annual temperature: 0 to 6 degrees C. (32 to 43 degrees F.)\nFrost-free season: 20 to 50 days" }, "GEOGRAPHICALLY ASSOCIATED SOILS": { "section": "GEOGRAPHICALLY ASSOCIATED SOILS", diff --git a/inst/extdata/OSD/S/SHARONDALE.json b/inst/extdata/OSD/S/SHARONDALE.json index 8a047a5a2d..1d0d4bbc77 100644 --- a/inst/extdata/OSD/S/SHARONDALE.json +++ b/inst/extdata/OSD/S/SHARONDALE.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: The Sharondale soils were mostly mapped as Cutshin soils in the past.\nDiagnostic horizons and features recognized in this pedon are:\nMollic epipedon: 0 to 18 inches A, AB\nCambic subsurface horizon: 18 to 34 inches Bw1, 34 to 49 inches Bw2, 49 to 63 inches Bw3, 63 to 75 inches BC" + "content": "REMARKS: The Sharondale soils were mostly mapped as Cutshin soils in the past.\nDiagnostic horizons and features recognized in this pedon are:\nMollic epipedon: 0 to 18 inches A, AB\nCambic subsurface horizon: 18 to 34 inches Bw1, 34 to 49 inches Bw2, 49 to 63 inches Bw3, 63 to 75 inches BC\n12/2021 revision - Oi had 2 to 0 inch depths, corrected to be 0 to 2 in horizon depths then added 2 inches to all horizon depths throughout the typical pedon. WJN" }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/S/SHERANDO.json b/inst/extdata/OSD/S/SHERANDO.json index ae114a31e8..ff7ddf6cf6 100644 --- a/inst/extdata/OSD/S/SHERANDO.json +++ b/inst/extdata/OSD/S/SHERANDO.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: The major diagnostic horizons recognized in this pedon are the alluvial E horizon from 3 to 7 inches and the cambic horizon from 16 to 46 inches.\nCEC class based on similar soils and laboratory data.\nThe 1/2006 revision updates this soil to the 9th Edition of the Keys to Soil Taxonomy (2003). The CEC activity class placement is based on similar soils. Class placement may be revised in the future when additional laboratory data becomes available.\nCompeting series, pedon descriptions (including horizon nomenclature and/or descriptive terms), and other sections on the OSD were not revised.\nPrevious revision date: 3/85" + "content": "REMARKS: The major diagnostic horizons recognized in this pedon are the alluvial E horizon from 3 to 7 inches and the cambic horizon from 16 to 46 inches.\nCEC class based on similar soils and laboratory data.\nThe 1/2006 revision updates this soil to the 9th Edition of the Keys to Soil Taxonomy (2003). The CEC activity class placement is based on similar soils. Class placement may be revised in the future when additional laboratory data becomes available.\nCompeting series, pedon descriptions (including horizon nomenclature and/or descriptive terms), and other sections on the OSD were not revised.\nPrevious revision date: 3/85\n2/2022 revision: O had 1 to 0 inch depths, corrected to be 0 to 1 in horizon depths then added 1 inch to all horizon depths throughout the typical pedon. WJN" }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/S/SINKIN.json b/inst/extdata/OSD/S/SINKIN.json index b5d474ddcb..61bf28b4a3 100644 --- a/inst/extdata/OSD/S/SINKIN.json +++ b/inst/extdata/OSD/S/SINKIN.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nParticle-size control section--the zone from a depth of 25 to 75 centimeters (Bt1 and Bt2 horizons)\nSeries control section--the zone from the surface to a depth of 163 centimeters (A, BA, Bt1, Bt2, 2Bt3, and 2Bt4 horizons).\nDiagnostic horizons and features recognized in this pedon include:\nochric epipedon--the zone from the surface to a depth of 25 centimeters (Ap and BA horizons)\nargillic horizon--the zone from a depth of 25 to 163 centimeters (Bt and 2Bt horizons)\nudic moisture regime.\nThe Sinkin soils were previously mapped as the Midco, Relfe, Tilk and Waben soil series." + "content": "REMARKS:\nParticle-size control section--the zone from a depth of 25 to 75 centimeters (Bt1 and Bt2 horizons)\nSeries control section--the zone from the surface to a depth of 163 centimeters (A, BA, Bt1, Bt2, 2Bt3, and 2Bt4 horizons).\nDiagnostic horizons and features recognized in this pedon include:\nochric epipedon--the zone from the surface to a depth of 25 centimeters (Ap and BA horizons)\nargillic horizon--the zone from a depth of 25 to 163 centimeters (Bt and 2Bt horizons)\nudic moisture regime.\nThe Sinkin soils were previously mapped as the Midco, Relfe, Tilk and Waben soil series.\nSite and pedon ID 1999MO203005M represents the typical pedon.\nTaxonomy version--Keys to Soil Taxonomy, thirteenth edition, 2022." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/S/SNOWLAKE.json b/inst/extdata/OSD/S/SNOWLAKE.json index 3a4f11f9bb..02c4849f58 100644 --- a/inst/extdata/OSD/S/SNOWLAKE.json +++ b/inst/extdata/OSD/S/SNOWLAKE.json @@ -19,7 +19,7 @@ }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nAverage annual soil temperature - 44 to 46 degrees F.\nAverage summer soil temperature - 54 to 56 degrees F. without an O horizon\nMoisture control section - dry 30 to 45 days (August to September), moist October through July\nDepth to sandy material - 10 to 20 inches\nBase saturation - 30 to 60 percent in the upper 30 inches\nVolcanic glass content in A and Bw horizons - 5 to 20 percent\nAcid-oxalate extr. Al + 1/2 Fe - 0.4 to 1.0 percent\nMoist bulk density - 1.0 to 1.2 g/cc\nPhosphate retention - 25 to 55 percent\nA horizon\nValue - 4 or 5 dry, 2 or 3 moist\nChroma - 1 to 3 dry or moist\nTexture - ASHY-SL, GR-ASHY-SL\nClay content - 3 to 10 percent\nGravel content - 0 to 15 percent (0 to 10 percent fine gravel)\nBw horizons\nHue - 10YR or 7.5YR\nValue - 5 or 6 dry, 3 or 4 moist\nChroma - 4 or 6 dry or moist\nTexture - ASHY-SL, GR-ASHY-SL\nClay content - 3 to 10 percent\nGravel content - 0 to 20 percent (0 to 10 percent fine gravel)\nReaction - slightly acid or neutral\nBC horizon\nHue - 10YR or 2.5Y\nValue - 6 to 8 dry, 4 to 6 moist\nChroma - 4 or 6 dry or moist\nTexture - LS, GR-LS\nClay content - 2 to 5 percent\nGravel content - 0 to 15 percent (0 to 10 percent fine gravel)\nReaction - slightly acid or neutral\nC horizons\nHue - 10YR, 2.5Y, or variegated\nValue - 6 to 8 dry, 4 to 6 moist\nChroma - 2 to 6 dry or moist\nTexture - GRF-LCOS, GRF-COS, GR-COS, LCOS, GR-LS," + "content": "RANGE IN CHARACTERISTICS:\nAverage annual soil temperature - 44 to 46 degrees F.\nAverage summer soil temperature - 54 to 56 degrees F. without an O horizon\nMoisture control section - dry 30 to 45 days (August to September), moist October through July\nDepth to sandy material - 10 to 20 inches\nBase saturation - 30 to 60 percent in the upper 30 inches\nVolcanic glass content in A and Bw horizons - 5 to 20 percent\nAcid-oxalate extr. Al + 1/2 Fe - 0.4 to 1.0 percent\nMoist bulk density - 1.0 to 1.2 g/cc\nPhosphate retention - 25 to 55 percent\nA horizon\nValue - 4 or 5 dry, 2 or 3 moist\nChroma - 1 to 3 dry or moist\nTexture - ASHY-SL, GR-ASHY-SL\nClay content - 3 to 10 percent\nGravel content - 0 to 15 percent (0 to 10 percent fine gravel)\nBw horizons\nHue - 10YR or 7.5YR\nValue - 5 or 6 dry, 3 or 4 moist\nChroma - 4 or 6 dry or moist\nTexture - ASHY-SL, GR-ASHY-SL\nClay content - 3 to 10 percent\nGravel content - 0 to 20 percent (0 to 10 percent fine gravel)\nReaction - slightly acid or neutral\nBC horizon\nHue - 10YR or 2.5Y\nValue - 6 to 8 dry, 4 to 6 moist\nChroma - 4 or 6 dry or moist\nTexture - LS, GR-LS\nClay content - 2 to 5 percent\nGravel content - 0 to 15 percent (0 to 10 percent fine gravel)\nReaction - slightly acid or neutral\nC horizons\nHue - 10YR, 2.5Y, or variegated\nValue - 6 to 8 dry, 4 to 6 moist\nChroma - 2 to 6 dry or moist\nTexture - GRF-LCOS, GRF-COS, GR-COS, LCOS, GR-LS,\nGR-LCOS, COS\nClay content - 0 to 3 percent\nGravel content - 5 to 30 percent (5 to 20 percent fine gravel)\nReaction - moderately acid to neutral" }, "COMPETING SERIES": { "section": "COMPETING SERIES", diff --git a/inst/extdata/OSD/S/SOLOMON.json b/inst/extdata/OSD/S/SOLOMON.json index a08d01a16d..01f7fb8c9f 100644 --- a/inst/extdata/OSD/S/SOLOMON.json +++ b/inst/extdata/OSD/S/SOLOMON.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nMollic epipedon: The zone from 0 to 81 centimeters (0 to 32 inches) (Ap, A, and Bg horizons)\nCambic horizon: The zone from 81 to 127 centimeters (32 to 50 inches) (BCg horizon)\nRedoximorphic concentrations: In the zone from 41 to 165 centimeters (16 to 65 inches) (Bg, BCg, and Cg horizons)\nMoisture conditions: Aquic\nEpisaturation: A seasonal, perched water table ranges from 30 centimeters (12 inches) above the surface to 61 centimeters (24 inches) below (Ap, A, and Bg horizons)\nVertic features: The presence of linear extensibility of 6.0 cm or more between 0 and 100 cm (0 to 40 inches). There is no lab data available to support this, but it is assumed that it would meet this criteria due to the amount and type (smectitic) of clay.\nSolomon soils will likely classify as a Vertisol if intersecting slickensides are found to occur.\n07/2003 WAW Changed format to semi-tabular from narrative.\nChanged runoff: from very slow to negligible\nRange in characteristics: Added clay and sand content to control section\nModified format by LRM in 3/2006 to include metric conversion and change permeability to saturated hydraulic conductivity." + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nMollic epipedon: The zone from 0 to 81 centimeters (0 to 32 inches) (Ap, A, and Bg horizons)\nCambic horizon: The zone from 81 to 127 centimeters (32 to 50 inches) (BCg horizon)\nRedoximorphic concentrations: In the zone from 41 to 165 centimeters (16 to 65 inches) (Bg, BCg, and Cg horizons)\nMoisture conditions: Aquic\nEpisaturation: A seasonal, perched water table ranges from 30 centimeters (12 inches) above the surface to 61 centimeters (24 inches) below (Ap, A, and Bg horizons)\nVertic features: The presence of linear extensibility of 6.0 cm or more between 0 and 100 cm (0 to 40 inches). There is no lab data available to support this, but it is assumed that it would meet this criteria due to the amount and type (smectitic) of clay.\nSolomon soils will likely classify as a Vertisol if intersecting slickensides are found to occur.\n07/2003 WAW Changed format to semi-tabular from narrative.\nChanged runoff: from very slow to negligible\nRange in characteristics: Added clay and sand content to control section\nModified format by LRM in 3/2006 to include metric conversion and change permeability to saturated hydraulic conductivity.\n09/2015 DJK Updated opening paragraph to current SSRO5 standards. Added quad and lat/long to type location. Added elevation to typical pedon. Added clay content, sand content, CCE, and redoximorphic features to RIC. Added elevation, precipitation pattern, and FFD to geographic setting. Added flooding, ponding, and saturation statement to drainage and Ksat section. Updated use and vegetation section to include wildlife habitat and wetland vegetation. Edited depths of mollic and cambic in remarks. Added Vertic features. Added statement about being a Vertisol if have slickensides. Added available lab data to additional data.\n07/2020 BKN Updated intro paragraph. Updated Distribution and Extent paragraph to include LRR and MLRA names. Removed South Dakota (SD) from the state list at the top as this soils does not occur in SD at all.\nKeys to Soil Taxonomy: Twelfth Edition, 2014" }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/S/STINGAL.json b/inst/extdata/OSD/S/STINGAL.json index 2006353004..d39cdccde0 100644 --- a/inst/extdata/OSD/S/STINGAL.json +++ b/inst/extdata/OSD/S/STINGAL.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nOchric epipedon - The zone from the soil surface to 6 inches (Ap1 and Ap2 horizons).\nCambic horizon - The zone from 6 to 25 inches (Bw1 and Bw2 horizons).\nCalcic horizon - The zone from 25 to 48 inches (Bkn1 and Bkn2 horizons).\nParticle-size control section - The zone from 10 to 40 inches (Bw2 and Bkn1 horizons and part of the Bw1 and Bkn2 horizons)." + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nOchric epipedon - The zone from the soil surface to 6 inches (Ap1 and Ap2 horizons).\nCambic horizon - The zone from 6 to 25 inches (Bw1 and Bw2 horizons).\nCalcic horizon - The zone from 25 to 48 inches (Bkn1 and Bkn2 horizons).\nParticle-size control section - The zone from 10 to 40 inches (Bw2 and Bkn1 horizons and part of the Bw1 and Bkn2 horizons).\nThis revision of April 2005 updates the taxonomic class from Coarse-silty, mixed, superactive, mesic Xeric Haplocambids based on estimated soil properties for cation exchange capacity and sodium adsorption ratio in the NASIS database, field observation at the typical pedon for the series that recognized a calcic horizon, use as dry cropland, and correlation to an Upland rangeland ecological site." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/T/TINE.json b/inst/extdata/OSD/T/TINE.json index 15bb52b37a..652a23074f 100644 --- a/inst/extdata/OSD/T/TINE.json +++ b/inst/extdata/OSD/T/TINE.json @@ -38,12 +38,12 @@ "content": "DRAINAGE AND PERMEABILITY: Well to somewhat excessively drained; slow runoff; rapid permeability." }, "USE AND VEGETATION": { - "section": "USE AND VEGETATION", - "content": "USE AND VEGETATION: These soils are used as native pastureland and recreational purposes." + "section": "USE AND VEGETATION & USE AND VEGETATION", + "content": "USE AND VEGETATION: These soils are used as native pastureland and recreational purposes. & USE AND VEGETATION: These soils are used as native pastureland and fro recreational purposes. Principal native vegetation is sagebrush, ring muhly, and Idaho fescue." }, "DISTRIBUTION AND EXTENT": { "section": "DISTRIBUTION AND EXTENT", - "content": "DISTRIBUTION AND EXTENT: High mountain valleys of central Colorado and adjacent parts of Wyoming. The series is of moderate extent.\nUSE AND VEGETATION: These soils are used as native pastureland and fro recreational purposes. Principal native vegetation is sagebrush, ring muhly, and Idaho fescue." + "content": "DISTRIBUTION AND EXTENT: High mountain valleys of central Colorado and adjacent parts of Wyoming. The series is of moderate extent." }, "REGIONAL OFFICE": { "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", diff --git a/inst/extdata/OSD/T/TIZZARD.json b/inst/extdata/OSD/T/TIZZARD.json index 15613af6a3..34ced26410 100644 --- a/inst/extdata/OSD/T/TIZZARD.json +++ b/inst/extdata/OSD/T/TIZZARD.json @@ -6,8 +6,8 @@ "STATES": "MD", "OVERVIEW": "MLRA(s): 153C, 153D", "TAXONOMIC CLASS": { - "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Sandy over loamy, aniso, siliceous, subactive, nonacid, mesic Sulfic Fluvaquents\nDepth Class: Very deep\nDrainage Class: Very poorly drained (permanently submersed)\nPermeability: Moderate to very rapid\nIndex Surface Runoff: Negligible\nParent Material: Barrier island washover sediments overlying loamy paleo-terrestrial tidal marsh deposits\nSlope: 0 to 1 percent\nMean Annual Air Temperature: 56 degrees F.\nMean Annual Water Temperature: 57 degrees F.\nTAXONOMIC CLASS: Sandy over loamy, aniso, siliceous, subactive, nonacid, mesic Sulfic Fluvaquents" + "section": "TAXONOMIC CLASS & TAXONOMIC CLASS", + "content": "TAXONOMIC CLASS: Sandy over loamy, aniso, siliceous, subactive, nonacid, mesic Sulfic Fluvaquents\nDepth Class: Very deep\nDrainage Class: Very poorly drained (permanently submersed)\nPermeability: Moderate to very rapid\nIndex Surface Runoff: Negligible\nParent Material: Barrier island washover sediments overlying loamy paleo-terrestrial tidal marsh deposits\nSlope: 0 to 1 percent\nMean Annual Air Temperature: 56 degrees F.\nMean Annual Water Temperature: 57 degrees F. & TAXONOMIC CLASS: Sandy over loamy, aniso, siliceous, subactive, nonacid, mesic Sulfic Fluvaquents" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", diff --git a/inst/extdata/OSD/T/TOGHOTTHELE.json b/inst/extdata/OSD/T/TOGHOTTHELE.json index 9968bd4698..92b03511f7 100644 --- a/inst/extdata/OSD/T/TOGHOTTHELE.json +++ b/inst/extdata/OSD/T/TOGHOTTHELE.json @@ -58,8 +58,8 @@ "content": "REMARKS: Diagnostic features and horizons recognized in this profile include:\nOchric epipedon: from 2 to 7 inches, 6 to 18 cm.\nCambic horizon: from 7 to 28 inches, 12 to 59 cm.\nEffervescence with dilute hydrochloric acid: from 51 to 72 inches, 130 to 183 cm.\nTemperature regime: cryic 25 F., -4 C.\nMoisture regime: udic" }, "ADDITIONAL DATA": { - "section": "ADDITIONAL DATA", - "content": "ADDITIONAL DATA:\nADDITIONAL DATA: National Soil Survey Laboratory data S06AK-240-00? from Southeast Fairbanks Borough, Alaska, samples by SSL Lincoln, NE, 07/2006" + "section": "ADDITIONAL DATA & ADDITIONAL DATA", + "content": "ADDITIONAL DATA:\nADDITIONAL DATA: National Soil Survey Laboratory data S06AK-240-00? from Southeast Fairbanks Borough, Alaska, samples by SSL Lincoln, NE, 07/2006 & ADDITIONAL DATA: National Soil Survey Laboratory data S06AK-240-00? from Southeast Fairbanks Borough, Alaska, samples by SSL Lincoln, NE, 07/2006" }, "SITE": [ [ diff --git a/inst/extdata/OSD/T/TREVLAC.json b/inst/extdata/OSD/T/TREVLAC.json index df90cde618..9674c242bf 100644 --- a/inst/extdata/OSD/T/TREVLAC.json +++ b/inst/extdata/OSD/T/TREVLAC.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are: ochric epipedon - 0 to 13 inches (A, E, BE horizons); argillic horizon - 13 to 31 inches (Bt1, Bt2, Bt3 horizons)." + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are: ochric epipedon - 0 to 13 inches (A, E, BE horizons); argillic horizon - 13 to 31 inches (Bt1, Bt2, Bt3 horizons).\n2/2022 revision: Oi had 1 to 0 inch depths, corrected to be 0 to 1 in horizon depths then added 1 inch to all horizon depths throughout the typical pedon. WJN" }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/V/VASQUEZ.json b/inst/extdata/OSD/V/VASQUEZ.json index f2353a2808..b3a16f7995 100644 --- a/inst/extdata/OSD/V/VASQUEZ.json +++ b/inst/extdata/OSD/V/VASQUEZ.json @@ -34,12 +34,12 @@ "content": "GEOGRAPHICALLY ASSOCIATED SOILS: These are the Naverly, Nystrom, and Ptarmigan soils. Naverly soils lack an aquic moisture regime. Nystrom soils are Nistisols. Ptarmigan soils lack an aquic moisture regime." }, "DRAINAGE AND PERMEABILITY": { - "section": "DRAINAGE AND PERMEABILITY", - "content": "DRAINAGE AND PERMEABILITY: Poorly drained; very slow runoff or ponded; moderate permeability. These soils have a fluctuating high water table." + "section": "DRAINAGE AND PERMEABILITY & DRAINAGE AND PERMEABILITY", + "content": "DRAINAGE AND PERMEABILITY: Poorly drained; very slow runoff or ponded; moderate permeability. These soils have a fluctuating high water table. & DRAINAGE AND PERMEABILITY: Poorly drained; very slow runoff or ponded; moderate permeability. These soils have a fluctuating high water table." }, "USE AND VEGETATION": { - "section": "USE AND VEGETATION", - "content": "USE AND VEGETATION: These soils are used as native pastureland, and for recreational purposes. They have considerable importance for wildlife, and they are very influential in controlling the late summer stream flow from the mountainous areas. Principal native vegetation is water tolerant alpine grasses, sedges, and willows.\nDRAINAGE AND PERMEABILITY: Poorly drained; very slow runoff or ponded; moderate permeability. These soils have a fluctuating high water table.\nUSE AND VEGETATION: These soils are used as native pastureland, and for recreational purposes. They have considerable importance for wildlife, and they are very influential in controlling the late summer stream flow for the mountainous areas. Principal native vegetation is water tolerant alpine grasses, sedges, and willows." + "section": "USE AND VEGETATION & USE AND VEGETATION", + "content": "USE AND VEGETATION: These soils are used as native pastureland, and for recreational purposes. They have considerable importance for wildlife, and they are very influential in controlling the late summer stream flow from the mountainous areas. Principal native vegetation is water tolerant alpine grasses, sedges, and willows. & USE AND VEGETATION: These soils are used as native pastureland, and for recreational purposes. They have considerable importance for wildlife, and they are very influential in controlling the late summer stream flow for the mountainous areas. Principal native vegetation is water tolerant alpine grasses, sedges, and willows." }, "DISTRIBUTION AND EXTENT": { "section": "DISTRIBUTION AND EXTENT", diff --git a/inst/extdata/OSD/W/WABEDO.json b/inst/extdata/OSD/W/WABEDO.json index d0abde4348..cfd067db13 100644 --- a/inst/extdata/OSD/W/WABEDO.json +++ b/inst/extdata/OSD/W/WABEDO.json @@ -46,12 +46,12 @@ "content": "DISTRIBUTION AND EXTENT: Central Minnesota - the soil is of moderate extent. Source of name is that of a lake in Cass County." }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: St. Paul, Minnesota" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: St. Paul, Minnesota & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: St. Paul, Minnesota" }, "ORIGIN": { "section": "SERIES PROPOSED & SERIES ESTABLISHED", - "content": "SERIES PROPOSED: Cass County, Minnesota, December, 1986.\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: St. Paul, Minnesota & SERIES ESTABLISHED: Cass County, Minnesota, 1992." + "content": "SERIES PROPOSED: Cass County, Minnesota, December, 1986. & SERIES ESTABLISHED: Cass County, Minnesota, 1992." }, "REMARKS": { "section": "REMARKS", diff --git a/inst/extdata/OSD/W/WASSOOKEAG.json b/inst/extdata/OSD/W/WASSOOKEAG.json index e00d93eb73..4989c89e70 100644 --- a/inst/extdata/OSD/W/WASSOOKEAG.json +++ b/inst/extdata/OSD/W/WASSOOKEAG.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: The series name (pronounced WAH suh keg) is taken from one of the larger lakes of Southern Penobscot County, Maine. This soil is part of a proposed catena of soils that include Sebasticook, Penobscot, and Corinna. They developed in till that is shallow to deep to calcareous metamorphic bedrock of the Waterville and Sangerville Formations in Central Maine. In comparison to other soils of the region they have a higher base saturation, water-holding capacity, and saturated hydraulic conductivity. They are considered agriculturally productive, particularly for potatoes.\nThe subgroup is revised from Aquic Dystric to Oxyaquic, and the mineralogy class to mixed with this revision. It is recognized that some pedons characterized for series development have isotic mineralogy.\nFeatures similar to those described as remnants of highly weathered pelitic limestone, were historically described as \"limestone ghosts\" in some places." + "content": "REMARKS: The series name (pronounced WAH suh keg) is taken from one of the larger lakes of Southern Penobscot County, Maine. This soil is part of a proposed catena of soils that include Sebasticook, Penobscot, and Corinna. They developed in till that is shallow to deep to calcareous metamorphic bedrock of the Waterville and Sangerville Formations in Central Maine. In comparison to other soils of the region they have a higher base saturation, water-holding capacity, and saturated hydraulic conductivity. They are considered agriculturally productive, particularly for potatoes.\nThe subgroup is revised from Aquic Dystric to Oxyaquic, and the mineralogy class to mixed with this revision. It is recognized that some pedons characterized for series development have isotic mineralogy.\nFeatures similar to those described as remnants of highly weathered pelitic limestone, were historically described as \"limestone ghosts\" in some places.\nReaction updated based on KSSL data for the Bw1, Bw2, and BC horizons only; others were field measured using Cornell field kit. Measured field values for the Bw1, Bw2, and BC were 6.7, 6.0. and 6.5, respectively. Field texture of the Bw1 was loam. KSSL data placed this horizon in the sandy loam class but near the boundary with loam. It is not the typical range for this series and the typical pedon is maintained as a loam.\nDiagnostic horizons and features recognized in this pedon include:\n1. Ochric epipedon--the zone from 0 to 30 cm (Ap horizon).\n2. Evidence of oxyaquic conditions--redox depletions and concentrations from 74 to 119 cm.\nCambic horizon--from a depth of 30 to 74 cm (Bw horizon).\n3. Lithic contact--at 147 cm (2R horizon)" }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/W/WELLS.json b/inst/extdata/OSD/W/WELLS.json index 72a41ae27b..2d69dd4fd1 100644 --- a/inst/extdata/OSD/W/WELLS.json +++ b/inst/extdata/OSD/W/WELLS.json @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nParticle-size control section: The zone from 41 to 91 cm (16 to 36 inches). (upper 50 cm of Bt1 and Bt2 horizons)\nMollic epipedon: The zone from 0 to 41 centimeters (0 to 16 inches). (A, BA horizons)\nArgillic horizon: The zone from 41 to 127 centimeters (16 to 50 inches). (Bt1, Bt2, and Bt3 horizons)\nThe assignment of the CEC activity class is supported by KSSL sample number 79P0320 (pedon 79KS143001).\nIn some pedons, sandstone or sandy shale bedrock occurs at depths between 100 and 150 cm.\n07/2003 WAW CEC activity class added, change format to semi-tablular, updated competing series, added ADDITIONAL DATA, updated reaction classes in horizon description to new terminology.\nModified format by LRM in 2/2006 to include metric conversion and change permeability to saturated hydraulic conductivity." + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nParticle-size control section: The zone from 41 to 91 cm (16 to 36 inches). (upper 50 cm of Bt1 and Bt2 horizons)\nMollic epipedon: The zone from 0 to 41 centimeters (0 to 16 inches). (A, BA horizons)\nArgillic horizon: The zone from 41 to 127 centimeters (16 to 50 inches). (Bt1, Bt2, and Bt3 horizons)\nThe assignment of the CEC activity class is supported by KSSL sample number 79P0320 (pedon 79KS143001).\nIn some pedons, sandstone or sandy shale bedrock occurs at depths between 100 and 150 cm." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", diff --git a/inst/extdata/OSD/W/WHARTON.json b/inst/extdata/OSD/W/WHARTON.json index ffb48f3aab..a250fad452 100644 --- a/inst/extdata/OSD/W/WHARTON.json +++ b/inst/extdata/OSD/W/WHARTON.json @@ -10,8 +10,8 @@ "content": "TAXONOMIC CLASS: Fine-loamy, mixed, active, mesic Aquic Hapludults" }, "TYPICAL PEDON": { - "section": "TYPICAL PEDON & This edit updates the format to the MO6 semitabular format; adds fragment kind and updates redoximorphic features in horizon descriptions of TYPICAL PEDON; revises COMPETING SERIES section; expands the description of GEOGRAPHICALLY ASSOCIATED SOILS; updates the DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY section; adds states to the DISTRIBUTION AND EXTENT section; adds diagnostic features to the REMARKS section; and adds other sampled pedons to the ADDITIONAL DATA section.", - "content": "TYPICAL PEDON: Wharton silt loam, cultivated on a 3 to 8 percent east facing slope. (Colors are for moist soil unless otherwise indicated.)\nAp--0 to 23 cm (0 to 9 inches); dark grayish brown (10YR 4/2) silt loam, light brownish gray (10YR 6/2) dry; moderate fine and medium granular structure; friable, slightly sticky and slightly plastic; 1 percent shale fragments; strongly acid; abrupt smooth boundary. (18 to 30 cm thick)\nBt1--23 to 41 cm (9 to 16 inches); yellowish brown (10YR 5/4) silt loam; moderate fine subangular and angular blocky structure; friable, moderately sticky and moderately plastic; common faint clay films on some faces of peds and lining some pores; 1 percent shale fragments; very strongly acid; clear wavy boundary.\nBt2--41 to 56 cm (16 to 22 inches); yellowish brown (10YR 5/4) silt loam; moderate medium angular blocky structure; friable, moderately sticky and moderately plastic; many distinct clay films on faces of peds and lining pores; common medium distinct yellowish brown (10YR 5/6) and strong brown (7.5YR 5/6) iron-manganese masses; common medium distinct grayish brown (10YR 5/2) iron depletions; 1 percent shale fragments; very strongly acid; clear wavy boundary.\nBt3--56 to 79 cm (22 to 31 inches); brown (10YR 5/3) silt loam; moderate coarse prismatic structure parting to moderate medium angular blocky; friable, moderately sticky and moderately plastic; continuous prominent clay films on the faces of peds and lining pores; many medium prominent strong brown (7.5YR 5/6) iron-manganese masses; many medium distinct gray (10YR 6/1) iron depletions and many coarse faint light brownish gray (10YR 6/2) iron depletions on prism faces; 2 percent shale fragments; extremely acid; gradual wavy boundary. (Combined thickness of the Bt horizon is 51 to 107 cm)\nBC--79 to 117 cm (31 to 46 inches); dark yellowish brown (10YR 4/4) silty clay loam; moderate coarse prismatic structure parting to weak coarse angular blocky; firm, moderately sticky and moderately plastic; few faint clay films on faces of peds and lining pores; common coarse prominent strong brown (7.5YR 5/8) and common coarse distinct yellowish brown (10YR 5/6) iron-manganese masses; many coarse distinct gray (10YR 6/1) iron depletions on prism faces; 10 percent shale fragments; extremely acid; gradual wavy boundary. (0 to 51 cm thick)\nC--117 to 175 cm (46 to 69 inches); brown (10YR 5/3) channery silty clay loam; massive; very firm, moderately sticky and moderately plastic; common medium distinct yellowish brown (10YR 5/6) iron-manganese masses; common medium distinct gray (N 6/0) iron depletions and few medium distinct gray (10YR 6/1) iron depletions on prism faces; 20 percent shale fragments; extremely acid; abrupt wavy boundary. (25 to 64 cm thick)\nCr--175 to 200 cm (69 to 79 inches); brown (10YR 5/3) rippable shale. & This edit updates the format to the MO6 semitabular format; adds fragment kind and updates redoximorphic features in horizon descriptions of TYPICAL PEDON; revises COMPETING SERIES section; expands the description of GEOGRAPHICALLY ASSOCIATED SOILS; updates the DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY section; adds states to the DISTRIBUTION AND EXTENT section; adds diagnostic features to the REMARKS section; and adds other sampled pedons to the ADDITIONAL DATA section.\nPrevious version: 07/2004-AWD, WRK, ART" + "section": "TYPICAL PEDON", + "content": "TYPICAL PEDON: Wharton silt loam, cultivated on a 3 to 8 percent east facing slope. (Colors are for moist soil unless otherwise indicated.)\nAp--0 to 23 cm (0 to 9 inches); dark grayish brown (10YR 4/2) silt loam, light brownish gray (10YR 6/2) dry; moderate fine and medium granular structure; friable, slightly sticky and slightly plastic; 1 percent shale fragments; strongly acid; abrupt smooth boundary. (18 to 30 cm thick)\nBt1--23 to 41 cm (9 to 16 inches); yellowish brown (10YR 5/4) silt loam; moderate fine subangular and angular blocky structure; friable, moderately sticky and moderately plastic; common faint clay films on some faces of peds and lining some pores; 1 percent shale fragments; very strongly acid; clear wavy boundary.\nBt2--41 to 56 cm (16 to 22 inches); yellowish brown (10YR 5/4) silt loam; moderate medium angular blocky structure; friable, moderately sticky and moderately plastic; many distinct clay films on faces of peds and lining pores; common medium distinct yellowish brown (10YR 5/6) and strong brown (7.5YR 5/6) iron-manganese masses; common medium distinct grayish brown (10YR 5/2) iron depletions; 1 percent shale fragments; very strongly acid; clear wavy boundary.\nBt3--56 to 79 cm (22 to 31 inches); brown (10YR 5/3) silt loam; moderate coarse prismatic structure parting to moderate medium angular blocky; friable, moderately sticky and moderately plastic; continuous prominent clay films on the faces of peds and lining pores; many medium prominent strong brown (7.5YR 5/6) iron-manganese masses; many medium distinct gray (10YR 6/1) iron depletions and many coarse faint light brownish gray (10YR 6/2) iron depletions on prism faces; 2 percent shale fragments; extremely acid; gradual wavy boundary. (Combined thickness of the Bt horizon is 51 to 107 cm)\nBC--79 to 117 cm (31 to 46 inches); dark yellowish brown (10YR 4/4) silty clay loam; moderate coarse prismatic structure parting to weak coarse angular blocky; firm, moderately sticky and moderately plastic; few faint clay films on faces of peds and lining pores; common coarse prominent strong brown (7.5YR 5/8) and common coarse distinct yellowish brown (10YR 5/6) iron-manganese masses; many coarse distinct gray (10YR 6/1) iron depletions on prism faces; 10 percent shale fragments; extremely acid; gradual wavy boundary. (0 to 51 cm thick)\nC--117 to 175 cm (46 to 69 inches); brown (10YR 5/3) channery silty clay loam; massive; very firm, moderately sticky and moderately plastic; common medium distinct yellowish brown (10YR 5/6) iron-manganese masses; common medium distinct gray (N 6/0) iron depletions and few medium distinct gray (10YR 6/1) iron depletions on prism faces; 20 percent shale fragments; extremely acid; abrupt wavy boundary. (25 to 64 cm thick)\nCr--175 to 200 cm (69 to 79 inches); brown (10YR 5/3) rippable shale." }, "TYPE LOCATION": { "section": "TYPE LOCATION", @@ -22,28 +22,28 @@ "content": "RANGE IN CHARACTERISTICS:\nDepth to the top of the Argillic horizon: 13 to 28 cm (5 to 11 inches)\nDepth to the base of the Argillic horizon: 64 to 138 cm (25 to 54 inches)\nSolum Thickness: 75 to 153 cm (30 to 60 inches)\nDepth to Bedrock: 102 to 183 cm (40 to 72 inches)\nDepth Class: Deep and Very Deep\nDepth to Seasonal High Water Table: 40 to 71 cm (16 to 28 inches), January through April\nRock Fragment content: 0 to 20 percent, by volume, in the A, E, BE, and Bt horizons, 5 to 50 percent, by volume, in the BC horizon, and 10 to 90 percent, by volume, in the C horizon\nFine-Earth Fraction: 25 to 35 percent clay in the particle control section\nSoil Reaction: Strongly acid through extremely acid throughout, except where limed\nRange of Individual Horizons:\nA or Ap horizon:\nColor--hue of 7.5YR or 10YR, value of 2 through 6, and chroma of 0 through 4\nTexture (fine-earth fraction)--silt loam or silty clay loam\nE horizon (if it occurs):\nColor--hue of 7.5YR or 10YR, value of 5 through 8, and chroma of 1 through 4\nTexture (fine earth fraction)--silt loam or silty clay loam\nBt and BC horizons:\nColor--hue of 7.5YR through 2.5Y, value of 4 through 6, and chroma of 1 through 8\nTexture (fine-earth fraction)--silt loam, loam, silty clay loam, clay loam, silty clay, or clay\nRedoximorphic features--iron-manganese masses in shades of brown, yellow, and olive and iron depletions in shades of gray, brown, yellow, and olive\nC horizon:\nColor--hue of 7.5YR through 2.5Y, value of 4 through 6, and chroma of 2 through 6\nTexture (fine-earth fraction)--silt loam, silty clay loam, silty clay, or clay\nRedoximorphic features--iron-manganese masses in shades of brown, yellow, and olive and iron depletions in shades of gray, brown, yellow, and olive\nCr horizon:\nTypically shale or siltstone bedrock but in some places it is interbedded with fine-grained sandstone." }, "COMPETING SERIES": { - "section": "COMPETING SERIES & This edit updates the format to the MO6 semitabular format; adds fragment kind and updates redoximorphic features in horizon descriptions of TYPICAL PEDON; revises COMPETING SERIES section; expands the description of GEOGRAPHICALLY ASSOCIATED SOILS; updates the DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY section; adds states to the DISTRIBUTION AND EXTENT section; adds diagnostic features to the REMARKS section; and adds other sampled pedons to the ADDITIONAL DATA section.", - "content": "COMPETING SERIES:\nAdelphia soil--formed in fluvio-marine sediments which contain glauconite in the series control section\nCotaco soils--formed in alluvial sediments which have sandy clay loam Bt horizons or less than 75 percent of the fine-earth passing the No. 2 sieve\nHolmdel soils--formed in loamy marine or fluvio-marine sediments which contain glauconite in the series control section\nKensington soils--formed in loess, till, and residuum, and have a 2Bt horizon\nTrackler soils--formed from fine-grained igneous rocks, and have a 2Bt horizon\nWoodstown soils--formed from sandy marine and old alluvial sediments & This edit updates the format to the MO6 semitabular format; adds fragment kind and updates redoximorphic features in horizon descriptions of TYPICAL PEDON; revises COMPETING SERIES section; expands the description of GEOGRAPHICALLY ASSOCIATED SOILS; updates the DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY section; adds states to the DISTRIBUTION AND EXTENT section; adds diagnostic features to the REMARKS section; and adds other sampled pedons to the ADDITIONAL DATA section.\nPrevious version: 07/2004-AWD, WRK, ART" + "section": "COMPETING SERIES", + "content": "COMPETING SERIES:\nAdelphia soil--formed in fluvio-marine sediments which contain glauconite in the series control section\nCotaco soils--formed in alluvial sediments which have sandy clay loam Bt horizons or less than 75 percent of the fine-earth passing the No. 2 sieve\nHolmdel soils--formed in loamy marine or fluvio-marine sediments which contain glauconite in the series control section\nKensington soils--formed in loess, till, and residuum, and have a 2Bt horizon\nTrackler soils--formed from fine-grained igneous rocks, and have a 2Bt horizon\nWoodstown soils--formed from sandy marine and old alluvial sediments" }, "GEOGRAPHIC SETTING": { "section": "GEOGRAPHIC SETTING", "content": "GEOGRAPHIC SETTING:\nMLRA(s) using this series: 124 (Western Allegheny Plateau), 125 (Cumberland Plateau and Mountains), 126 (Central Allegheny Plateau), 127 (Eastern Allegheny Plateau and Mountains), and 128 (Southern Appalachian Ridges and Valleys)\nLandscape: Uplands\nLandform: Hills\nGeomorphic Component: side slope, nose slope, head slope, or crest\nHillslope Profile Position: backslope, shoulder, or summit\nParent Material Origin: Pennsylvanian interbedded clay shale, siltstone, and fine-grained sandstone\nParent Material Kind: Residuum\nSlope: 0 to 35 percent\nElevation: 207 to 610 meters (679 to 2001 feet)\nFrost-free period: 162 to 205 days\nMean Annual Air Temperature: 5.0 to 14.0 degrees C. (41 to 57 degrees F.)\nMean Annual Precipitation: 813 to 1854 millimeters (32 to 73 inches)" }, "GEOGRAPHICALLY ASSOCIATED SOILS": { - "section": "GEOGRAPHICALLY ASSOCIATED SOILS & This edit updates the format to the MO6 semitabular format; adds fragment kind and updates redoximorphic features in horizon descriptions of TYPICAL PEDON; revises COMPETING SERIES section; expands the description of GEOGRAPHICALLY ASSOCIATED SOILS; updates the DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY section; adds states to the DISTRIBUTION AND EXTENT section; adds diagnostic features to the REMARKS section; and adds other sampled pedons to the ADDITIONAL DATA section.", - "content": "GEOGRAPHICALLY ASSOCIATED SOILS:\nArmagh soils--occur on broad ridgetops and benches that are poorly drained and have a fine particle size class\nBerks soils--occur on well drained summits and upper shoulders that are loamy-skeletal and have a lithic contact that is less than 102 centimeters deep\nBlairton soils--occur on upland flats, depressions, and in drainage heads that are moderately well drained and have a lithic contact that is less than 102 centimeters deep\nBrinkerton soils--occur on poorly drained footslopes of uplands that have a fragipan\nCavode soils--occur on somewhat poorly drained upland ridgetops, side slopes, and benches and have a fine particle size class\nErnest soils--occur on footslopes of uplands that have a fragipan\nGilpin soils--occur on well drained uplands that have a lithic contact that is less than 102 centimeters deep\nWeikert soils--occur on well drained uplands that have a lithic contact that is less than 51 centimeters deep & This edit updates the format to the MO6 semitabular format; adds fragment kind and updates redoximorphic features in horizon descriptions of TYPICAL PEDON; revises COMPETING SERIES section; expands the description of GEOGRAPHICALLY ASSOCIATED SOILS; updates the DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY section; adds states to the DISTRIBUTION AND EXTENT section; adds diagnostic features to the REMARKS section; and adds other sampled pedons to the ADDITIONAL DATA section.\nPrevious version: 07/2004-AWD, WRK, ART" + "section": "GEOGRAPHICALLY ASSOCIATED SOILS", + "content": "GEOGRAPHICALLY ASSOCIATED SOILS:\nArmagh soils--occur on broad ridgetops and benches that are poorly drained and have a fine particle size class\nBerks soils--occur on well drained summits and upper shoulders that are loamy-skeletal and have a lithic contact that is less than 102 centimeters deep\nBlairton soils--occur on upland flats, depressions, and in drainage heads that are moderately well drained and have a lithic contact that is less than 102 centimeters deep\nBrinkerton soils--occur on poorly drained footslopes of uplands that have a fragipan\nCavode soils--occur on somewhat poorly drained upland ridgetops, side slopes, and benches and have a fine particle size class\nErnest soils--occur on footslopes of uplands that have a fragipan\nGilpin soils--occur on well drained uplands that have a lithic contact that is less than 102 centimeters deep\nWeikert soils--occur on well drained uplands that have a lithic contact that is less than 51 centimeters deep" }, "DRAINAGE AND PERMEABILITY": { - "section": "DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY & This edit updates the format to the MO6 semitabular format; adds fragment kind and updates redoximorphic features in horizon descriptions of TYPICAL PEDON; revises COMPETING SERIES section; expands the description of GEOGRAPHICALLY ASSOCIATED SOILS; updates the DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY section; adds states to the DISTRIBUTION AND EXTENT section; adds diagnostic features to the REMARKS section; and adds other sampled pedons to the ADDITIONAL DATA section.", - "content": "DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY:\nDrainage Class (Agricultural): Moderately well drained\nInternal Free Water Occurrence: Shallow (25-50 cm) and Common (present 3-6 months)\nIndex Surface Runoff: Low through High\nSaturated Hydraulic Conductivity Class: Moderately low and moderately high\nShrink-Swell Class: Low\nFlooding frequency and Duration: None\nPonding frequency and Duration: None & This edit updates the format to the MO6 semitabular format; adds fragment kind and updates redoximorphic features in horizon descriptions of TYPICAL PEDON; revises COMPETING SERIES section; expands the description of GEOGRAPHICALLY ASSOCIATED SOILS; updates the DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY section; adds states to the DISTRIBUTION AND EXTENT section; adds diagnostic features to the REMARKS section; and adds other sampled pedons to the ADDITIONAL DATA section.\nPrevious version: 07/2004-AWD, WRK, ART" + "section": "DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY", + "content": "DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY:\nDrainage Class (Agricultural): Moderately well drained\nInternal Free Water Occurrence: Shallow (25-50 cm) and Common (present 3-6 months)\nIndex Surface Runoff: Low through High\nSaturated Hydraulic Conductivity Class: Moderately low and moderately high\nShrink-Swell Class: Low\nFlooding frequency and Duration: None\nPonding frequency and Duration: None" }, "USE AND VEGETATION": { "section": "USE AND VEGETATION", "content": "USE AND VEGETATION:\nMajor uses: Hayland, pasture, cropland, and woodland\nDominant Vegetation: Where cultivated--Grass-legume hay, corn, wheat, oats. Where wooded--Mixed hardwood trees." }, "DISTRIBUTION AND EXTENT": { - "section": "DISTRIBUTION AND EXTENT & This edit updates the format to the MO6 semitabular format; adds fragment kind and updates redoximorphic features in horizon descriptions of TYPICAL PEDON; revises COMPETING SERIES section; expands the description of GEOGRAPHICALLY ASSOCIATED SOILS; updates the DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY section; adds states to the DISTRIBUTION AND EXTENT section; adds diagnostic features to the REMARKS section; and adds other sampled pedons to the ADDITIONAL DATA section.", - "content": "DISTRIBUTION AND EXTENT:\nDistribution: Pennsylvania, Kentucky, Maryland, New York, Ohio, Virginia, and West Virginia; mainly MLRA's 124, 125, 126, 127, and 128\nExtent: Large, about 600,000 acres at the time of this revision & This edit updates the format to the MO6 semitabular format; adds fragment kind and updates redoximorphic features in horizon descriptions of TYPICAL PEDON; revises COMPETING SERIES section; expands the description of GEOGRAPHICALLY ASSOCIATED SOILS; updates the DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY section; adds states to the DISTRIBUTION AND EXTENT section; adds diagnostic features to the REMARKS section; and adds other sampled pedons to the ADDITIONAL DATA section.\nPrevious version: 07/2004-AWD, WRK, ART" + "section": "DISTRIBUTION AND EXTENT", + "content": "DISTRIBUTION AND EXTENT:\nDistribution: Pennsylvania, Kentucky, Maryland, New York, Ohio, Virginia, and West Virginia; mainly MLRA's 124, 125, 126, 127, and 128\nExtent: Large, about 600,000 acres at the time of this revision" }, "REGIONAL OFFICE": { "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", @@ -54,12 +54,12 @@ "content": "SERIES ESTABLISHED: Fayette County, Pennsylvania, 1943." }, "REMARKS": { - "section": "REMARKS & This edit updates the format to the MO6 semitabular format; adds fragment kind and updates redoximorphic features in horizon descriptions of TYPICAL PEDON; revises COMPETING SERIES section; expands the description of GEOGRAPHICALLY ASSOCIATED SOILS; updates the DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY section; adds states to the DISTRIBUTION AND EXTENT section; adds diagnostic features to the REMARKS section; and adds other sampled pedons to the ADDITIONAL DATA section.", - "content": "REMARKS:\nDiagnostic horizons and soil characteristics recognized in this pedon are:\nOchric epipedon--the zone from 0 to 23 cm (Ap horizon)\nArgillic horizon--the zone from 23 to 79 cm (Bt horizon)\nRedoximorphic depletions with chroma of 2 or less--the zone from 41 to 175 cm\nParalithic contact--175 cm\nSeries control section--the zone from 23 to 73 cm & This edit updates the format to the MO6 semitabular format; adds fragment kind and updates redoximorphic features in horizon descriptions of TYPICAL PEDON; revises COMPETING SERIES section; expands the description of GEOGRAPHICALLY ASSOCIATED SOILS; updates the DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY section; adds states to the DISTRIBUTION AND EXTENT section; adds diagnostic features to the REMARKS section; and adds other sampled pedons to the ADDITIONAL DATA section.\nPrevious version: 07/2004-AWD, WRK, ART" + "section": "REMARKS", + "content": "REMARKS:\nDiagnostic horizons and soil characteristics recognized in this pedon are:\nOchric epipedon--the zone from 0 to 23 cm (Ap horizon)\nArgillic horizon--the zone from 23 to 79 cm (Bt horizon)\nRedoximorphic depletions with chroma of 2 or less--the zone from 41 to 175 cm\nParalithic contact--175 cm\nSeries control section--the zone from 23 to 73 cm" }, "ADDITIONAL DATA": { - "section": "This edit updates the format to the MO6 semitabular format; adds fragment kind and updates redoximorphic features in horizon descriptions of TYPICAL PEDON; revises COMPETING SERIES section; expands the description of GEOGRAPHICALLY ASSOCIATED SOILS; updates the DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY section; adds states to the DISTRIBUTION AND EXTENT section; adds diagnostic features to the REMARKS section; and adds other sampled pedons to the ADDITIONAL DATA section. & ADDITIONAL DATA", - "content": "This edit updates the format to the MO6 semitabular format; adds fragment kind and updates redoximorphic features in horizon descriptions of TYPICAL PEDON; revises COMPETING SERIES section; expands the description of GEOGRAPHICALLY ASSOCIATED SOILS; updates the DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY section; adds states to the DISTRIBUTION AND EXTENT section; adds diagnostic features to the REMARKS section; and adds other sampled pedons to the ADDITIONAL DATA section.\nPrevious version: 07/2004-AWD, WRK, ART\nADDITIONAL DATA:\nPrevious revision used Pennsylvania characterization sample number PA-017-016 as a basis for placing this series in the active CEC activity class. Other sampled pedons include 61PA063053, 72PA129020, and 73PA033017. These samples were analyzed by Pennsylvania State University, University Park, Pennsylvania.\n________________________________________ & ADDITIONAL DATA:\nPrevious revision used Pennsylvania characterization sample number PA-017-016 as a basis for placing this series in the active CEC activity class. Other sampled pedons include 61PA063053, 72PA129020, and 73PA033017. These samples were analyzed by Pennsylvania State University, University Park, Pennsylvania.\n________________________________________" + "section": "ADDITIONAL DATA", + "content": "This edit updates the format to the MO6 semitabular format; adds fragment kind and updates redoximorphic features in horizon descriptions of TYPICAL PEDON; revises COMPETING SERIES section; expands the description of GEOGRAPHICALLY ASSOCIATED SOILS; updates the DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY section; adds states to the DISTRIBUTION AND EXTENT section; adds diagnostic features to the REMARKS section; and adds other sampled pedons to the ADDITIONAL DATA section.\nPrevious version: 07/2004-AWD, WRK, ART\nADDITIONAL DATA:\nPrevious revision used Pennsylvania characterization sample number PA-017-016 as a basis for placing this series in the active CEC activity class. Other sampled pedons include 61PA063053, 72PA129020, and 73PA033017. These samples were analyzed by Pennsylvania State University, University Park, Pennsylvania.\n________________________________________" }, "SITE": [ [ @@ -230,7 +230,7 @@ "eff_class": "NA", "distinctness": "NA", "topography": "NA", - "narrative": "Cr--175 to 200 cm (69 to 79 inches); brown (10YR 5/3) rippable shale. & This edit updates the format to the MO6 semitabular format; adds fragment kind and updates redoximorphic features in horizon descriptions of TYPICAL PEDON; revises COMPETING SERIES section; expands the description of GEOGRAPHICALLY ASSOCIATED SOILS; updates the DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY section; adds states to the DISTRIBUTION AND EXTENT section; adds diagnostic features to the REMARKS section; and adds other sampled pedons to the ADDITIONAL DATA section." + "narrative": "Cr--175 to 200 cm (69 to 79 inches); brown (10YR 5/3) rippable shale." } ] ] diff --git a/inst/extdata/OSD/W/WIDEWATER.json b/inst/extdata/OSD/W/WIDEWATER.json index 51a160038e..7cd6b7128f 100644 --- a/inst/extdata/OSD/W/WIDEWATER.json +++ b/inst/extdata/OSD/W/WIDEWATER.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Floodplains of the inner Northern Coastal Plain of Maryland\nExtent: Small\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Floodplains of the inner Northern Coastal Plain of Maryland\nExtent: Small & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES ESTABLISHED", diff --git a/inst/extdata/OSD/W/WILLAKENZIE.json b/inst/extdata/OSD/W/WILLAKENZIE.json index dbf86877eb..e10ed4265c 100644 --- a/inst/extdata/OSD/W/WILLAKENZIE.json +++ b/inst/extdata/OSD/W/WILLAKENZIE.json @@ -10,8 +10,8 @@ "content": "TAXONOMIC CLASS: Fine-loamy, mixed, active, mesic Ultic Haploxeralfs" }, "TYPICAL PEDON": { - "section": "TYPICAL PEDON & Typical pedon relocated based on field observations and documentation from several counties in the MLRA 2 Willamette Valley update area to reflect a modal concept for this soil which has brown hues, active cation exchange activity class, medium to moderately fine textures in the argillic horizon, and dominantly occurs on the Eugene and Spencer Formation geology along the margins of the Willamette. Willakenzie soils occur on the Brateng (low hills) and Dolph (foothills) geomorphic surfaces.", - "content": "TYPICAL PEDON: Willakenzie loam, cultivated field, on a 10 percent east-facing slope at an elevation of 380 feet. (When described on August 20, 1997 the soil was moist to a depth of 1 inch and dry below this depth. (Colors are for moist soil unless otherwise stated.)\nAp--0 to 5 inches; dark brown (7.5YR 3/3) loam, brown (10YR 5/3) dry; strong fine subangular blocky structure; slightly hard, very friable, slightly sticky and nonplastic; common very fine roots; many very fine tubular pores; moderately acid (pH 5.9); clear smooth boundary.\nA--5 to 11 inches; dark brown (7.5YR 3/4) loam, light yellowish brown (10YR 6/4) dry; moderate fine and medium subangular blocky structure; slightly hard, friable, slightly sticky and nonplastic; common very fine roots; many very fine tubular pores; moderately acid (pH 5.6); abrupt smooth boundary. (Combined thickness of the A horizon is 5 to 12 inches)\nBt1--11 to 19 inches; brown (7.5YR 4/4) clay loam, strong brown (7.5YR 5/6) dry; moderate medium and coarse subangular blocky structure; hard, firm, slightly sticky and slightly plastic; common very fine roots; many very fine, fine, and medium tubular pores; many distinct clay films on faces of peds and along pores; 5 percent paragravel; strongly acid (pH 5.4); clear wavy boundary.\nBt2--19 to 32 inches; strong brown (7.5YR 4/6) paragravelly clay loam, reddish yellow (7.5YR 6/6) dry; moderate medium and coarse subangular blocky structure; slightly hard, friable, slightly sticky and slightly plastic; few very fine roots; many very fine, fine, and medium tubular pores; common distinct clay films on faces of peds and along pores; 25 percent paragravel; strongly acid (pH 5.4); clear irregular boundary. (Combined thickness of the 2Bt horizon is 12 to 28 inches)\nCr---32 inches; weakly cemented tuffaceous sandstone. & Typical pedon relocated based on field observations and documentation from several counties in the MLRA 2 Willamette Valley update area to reflect a modal concept for this soil which has brown hues, active cation exchange activity class, medium to moderately fine textures in the argillic horizon, and dominantly occurs on the Eugene and Spencer Formation geology along the margins of the Willamette. Willakenzie soils occur on the Brateng (low hills) and Dolph (foothills) geomorphic surfaces.\nDepths to diagnostic horizons and features as noted in the range of characteristics start from the mineral soil surface.\nClassification revised 2/02 to reflect active mineralogy and fine-loamy family. This revision is based on extensive lab data." + "section": "TYPICAL PEDON", + "content": "TYPICAL PEDON: Willakenzie loam, cultivated field, on a 10 percent east-facing slope at an elevation of 380 feet. (When described on August 20, 1997 the soil was moist to a depth of 1 inch and dry below this depth. (Colors are for moist soil unless otherwise stated.)\nAp--0 to 5 inches; dark brown (7.5YR 3/3) loam, brown (10YR 5/3) dry; strong fine subangular blocky structure; slightly hard, very friable, slightly sticky and nonplastic; common very fine roots; many very fine tubular pores; moderately acid (pH 5.9); clear smooth boundary.\nA--5 to 11 inches; dark brown (7.5YR 3/4) loam, light yellowish brown (10YR 6/4) dry; moderate fine and medium subangular blocky structure; slightly hard, friable, slightly sticky and nonplastic; common very fine roots; many very fine tubular pores; moderately acid (pH 5.6); abrupt smooth boundary. (Combined thickness of the A horizon is 5 to 12 inches)\nBt1--11 to 19 inches; brown (7.5YR 4/4) clay loam, strong brown (7.5YR 5/6) dry; moderate medium and coarse subangular blocky structure; hard, firm, slightly sticky and slightly plastic; common very fine roots; many very fine, fine, and medium tubular pores; many distinct clay films on faces of peds and along pores; 5 percent paragravel; strongly acid (pH 5.4); clear wavy boundary.\nBt2--19 to 32 inches; strong brown (7.5YR 4/6) paragravelly clay loam, reddish yellow (7.5YR 6/6) dry; moderate medium and coarse subangular blocky structure; slightly hard, friable, slightly sticky and slightly plastic; few very fine roots; many very fine, fine, and medium tubular pores; common distinct clay films on faces of peds and along pores; 25 percent paragravel; strongly acid (pH 5.4); clear irregular boundary. (Combined thickness of the 2Bt horizon is 12 to 28 inches)\nCr---32 inches; weakly cemented tuffaceous sandstone." }, "TYPE LOCATION": { "section": "TYPE LOCATION", @@ -55,7 +55,7 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nOchric epipedon - from the soil surface to a depth of 11 inches (Ap and A horizons). Dark colors in the modal Ap horizon do not meet umbric epipedon criteria for thickness.\nArgillic horizon - from a depth of 11 to 32 inches (Bt1and Bt2 horizons)\nParticle-size control section - from a depth of 11 to 31 inches (Bt1 and nearly the entire Bt2 horizon)" + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nOchric epipedon - from the soil surface to a depth of 11 inches (Ap and A horizons). Dark colors in the modal Ap horizon do not meet umbric epipedon criteria for thickness.\nArgillic horizon - from a depth of 11 to 32 inches (Bt1and Bt2 horizons)\nParticle-size control section - from a depth of 11 to 31 inches (Bt1 and nearly the entire Bt2 horizon)\nTypical pedon relocated based on field observations and documentation from several counties in the MLRA 2 Willamette Valley update area to reflect a modal concept for this soil which has brown hues, active cation exchange activity class, medium to moderately fine textures in the argillic horizon, and dominantly occurs on the Eugene and Spencer Formation geology along the margins of the Willamette. Willakenzie soils occur on the Brateng (low hills) and Dolph (foothills) geomorphic surfaces.\nDepths to diagnostic horizons and features as noted in the range of characteristics start from the mineral soil surface.\nClassification revised 2/02 to reflect active mineralogy and fine-loamy family. This revision is based on extensive lab data." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA", @@ -184,7 +184,7 @@ "eff_class": "NA", "distinctness": "NA", "topography": "NA", - "narrative": "Cr---32 inches; weakly cemented tuffaceous sandstone. & Typical pedon relocated based on field observations and documentation from several counties in the MLRA 2 Willamette Valley update area to reflect a modal concept for this soil which has brown hues, active cation exchange activity class, medium to moderately fine textures in the argillic horizon, and dominantly occurs on the Eugene and Spencer Formation geology along the margins of the Willamette. Willakenzie soils occur on the Brateng (low hills) and Dolph (foothills) geomorphic surfaces. Depths to diagnostic horizons and features as noted in the range of characteristics start from the mineral soil surface." + "narrative": "Cr---32 inches; weakly cemented tuffaceous sandstone." } ] ] diff --git a/inst/extdata/OSD/W/WIST.json b/inst/extdata/OSD/W/WIST.json index a787fe87f2..1b14931b99 100644 --- a/inst/extdata/OSD/W/WIST.json +++ b/inst/extdata/OSD/W/WIST.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Northern Coastal Plain of Maryland and possibly New Jersey.\nExtent: Moderate\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Northern Coastal Plain of Maryland and possibly New Jersey.\nExtent: Moderate & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES ESTABLISHED", diff --git a/inst/extdata/OSD/Z/ZEKIAH.json b/inst/extdata/OSD/Z/ZEKIAH.json index 5aabb97de8..1144195ec6 100644 --- a/inst/extdata/OSD/Z/ZEKIAH.json +++ b/inst/extdata/OSD/Z/ZEKIAH.json @@ -46,8 +46,8 @@ "content": "NA" }, "REGIONAL OFFICE": { - "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", - "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Flood plains of the mid-Atlantic Coastal Plain of Maryland, Delaware, and New Jersey\nExtent: Moderate\nMLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" + "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE", + "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: RALEIGH, NORTH CAROLINA\nDistribution: Flood plains of the mid-Atlantic Coastal Plain of Maryland, Delaware, and New Jersey\nExtent: Moderate & MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia" }, "ORIGIN": { "section": "SERIES ESTABLISHED", diff --git a/inst/extdata/OSD/Z/ZENKER.json b/inst/extdata/OSD/Z/ZENKER.json index 5046c0aeed..0acc7f7877 100644 --- a/inst/extdata/OSD/Z/ZENKER.json +++ b/inst/extdata/OSD/Z/ZENKER.json @@ -54,8 +54,8 @@ "content": "SERIES ESTABLISHED: Wahkiakum County, Washington, 1976." }, "REMARKS": { - "section": "REMARKS", - "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are an umbric epipedon from the mineral surface to 17 inches and a cambic horizon from 17 to 60 inches. This description reflects a change in classification based on amendment 16. The particle-size control section has an estimated moist bulk density of less than 0.90 g/cc, volcanic glass content of 30 to 60 percent, acid-oxalate extractable aluminum plus one-half iron of more than 1 percent." + "section": "REMARKS & REMARKS", + "content": "REMARKS: Diagnostic horizons and features recognized in this pedon are an umbric epipedon from the mineral surface to 17 inches and a cambic horizon from 17 to 60 inches. This description reflects a change in classification based on amendment 16. The particle-size control section has an estimated moist bulk density of less than 0.90 g/cc, volcanic glass content of 30 to 60 percent, acid-oxalate extractable aluminum plus one-half iron of more than 1 percent. & REMARKS: Classification only changed 4/94 because of recent amendments to Soil Taxonomy." }, "ADDITIONAL DATA": { "section": "ADDITIONAL DATA",