Update inst/extdata/ JSON files

ncss-tech · Aug 12, 2024 · a5954cc · a5954cc
1 parent f8ffbe7
commit a5954cc
Showing 1 changed file with 3 additions and 3 deletions.
diff --git a/inst/extdata/OSD/S/ST._CHARLES.json b/inst/extdata/OSD/S/ST._CHARLES.json
@@ -2,7 +2,7 @@
   "SERIES": "ST. CHARLES",
   "STATUS": "Established Series",
   "BYREV": "Rev. GVB-SLE-AAC",
-  "REVDATE": "02/2011",
+  "REVDATE": "08/2024",
   "STATES": "IL,IN,WI",
   "OVERVIEW": "The St. Charles series consists of very deep, well drained soils on outwash plains, till plains, or stream terraces. They formed in 40 to 60 inches of loess and in the underlying loamy outwash or sandy loam till. Slope commonly is 0 to 15 percent but ranges from 0 to 30 percent. Mean annual temperature is about 11.1 degrees C (52 degrees F)., and mean annual precipitation is about 889 mm (35 inches).",
   "TAXONOMIC CLASS": {
@@ -31,7 +31,7 @@
   },
   "GEOGRAPHICALLY ASSOCIATED SOILS": {
     "section": "GEOGRAPHICALLY ASSOCIATED SOILS",
-    "content": "GEOGRAPHICALLY ASSOCIATED SOILS: These are the Batavia, Camden, Kendall, Kidder, McHenry, Sexton, Starks, and Thorp soils. Batavia soils have a dark-colored surface layer and commonly are upslope from St. Charles soils and farther from the drainageways. Camden soils are nearby on similar landscapes that have a mantle of loess 51 to 102 cm (20 to 40 inches) in thickness. Kendall soils are the somewhat poorly drained member of a hydro-sequence with St. Charles soils. Kidder and McHenry soils formed in sandy loam till on similar topographic positions as some St. Charles soils, but average more than 15 percent fine sand and coarser in the control section. The poorly drained Sexton and somewhat poorly drained Starks soils are on outwash plains and stream terraces nearby, and have chroma of 2 in the upper part of the sola. The nearly level, poorly drained Thorp soils have a thinner mantle of loess and are Argiaquic Argialbolls."
+    "content": "GEOGRAPHICALLY ASSOCIATED SOILS: These are the Batavia, Camden, Kendall, Kidder, McHenry, Sexton, Starks, and Thorp soils. Batavia soils have a dark-colored surface layer and commonly are upslope and farther from the drainageways. Camden soils are nearby on similar landscapes that have a mantle of loess 51 to 102 cm (20 to 40 inches) in thickness. Kendall soils are the somewhat poorly drained member of a hydro-sequence with St. Charles soils. Kidder and McHenry soils formed in sandy loam till on similar topographic positions as some St. Charles soils, but average more than 15 percent fine sand and coarser in the control section. The poorly drained Sexton and somewhat poorly drained Starks soils are on outwash plains and stream terraces nearby, and have chroma of 2 in the upper part of the sola. The nearly level, poorly drained Thorp soils have a thinner mantle of loess and are Argiaquic Argialbolls."
   },
   "DRAINAGE AND PERMEABILITY": {
     "section": "DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY",
@@ -47,7 +47,7 @@
   },
   "REGIONAL OFFICE": {
     "section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE",
-    "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Indianapolis, Indiana"
+    "content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Salina, Kansas"
   },
   "ORIGIN": {
     "section": "SERIES ESTABLISHED",