Official Series Description


Lab Data Summary

Aggregate lab data for the ST. CHARLES soil series. This aggregation is based on all pedons with a current taxon name of ST. CHARLES, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to ST. CHARLES were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
108A84IL0410041984IL041004St. Charles2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6956806,-88.0396028
111DMY80141980IN107014St. Charles2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9722861,-87.0073389
114B72IL0770021972IL077002St. Charles4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8285731,-89.3481924
114B77IL1570041977IL157004St. Charles4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2090197,-89.9062189
114B80IL1571071980IL157107St. Charles3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1187822,-89.8863265
114B80IL1571081980IL157108St. Charles3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.129757,-89.8851626
95B40A274353IL111009aSt. Charles2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.4113987,-88.4147656
95B40A1524S1952WI027020St. Charles3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5119438,-88.7583313
95B40A1525S1952WI027027St. Charles3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.4119453,-88.8688889

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ST. CHARLES soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the ST. CHARLES series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the ST. CHARLES series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the ST. CHARLES series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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There are insufficient data to create the 3D mountains figure.

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Competing Series

Soil series competing with ST. CHARLES share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the ST. CHARLES series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the ST. CHARLES series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

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Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with ST. CHARLES, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. IL-2010-09-01-05 | Edgar County - 2002

    Typical pattern of soils and parent material in the Camden-Starks association (Soil Survey of Edgar County, Illinois; 2002).

  2. IL-2010-09-01-73 | Stark County - 1996

    Typical pattern of soils and parent material in the Elburn-Plano and Catlin-Flanagan associations (Soil Survey of Stark County, Illinois; 1996).

  3. IL-2011-08-04-97 | Randolph County - 1988

    Pattern of soils and parent material in the St. Charles-Hurst-Martinsville association (Soil Survey of Randolph County, Illinois; 1988).

Map Units

Map units containing ST. CHARLES as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
St. Charles silt loam, 2 to 5 percent slopes243B443019979930758il00720061:12000
St. Charles silt loam, 0 to 2 percent slopes243A26891997986px3il00720061:12000
St. Charles silt loam, 5 to 10 percent slopes, eroded243C2243139723430759il00720061:12000
St. Charles silt loam, 2 to 5 percent slopes243B1092186272520j9xil01120071:12000
St. Charles silt loam, 5 to 10 percent slopes, eroded243C21067186272620j9yil01120071:12000
St. Charles silt loam, 0 to 2 percent slopes243A299186272420j9wil01120071:12000
St. Charles silt loam, 2 to 5 percent slopes, rarely flooded7243B99115977581qmllil03920051:12000
St. Charles silt loam, 2 to 5 percent slopes243B52215956941qkg0il03920051:12000
St. Charles silt loam, 2 to 5 percent slopes243B370843560x9smil04519971:12000
St. Charles silt loam, 2 to 5 percent slopes243B1478615646nnmkil05719971:12000
St. Charles silt loam, 5 to 10 percent slopes, eroded243C2175186888220qqjil09320071:12000
St. Charles silt loam, 2 to 5 percent slopes243B405113862281hjh1il09920061:12000
St. Charles silt loam, 5 to 10 percent slopes, eroded243C2183713862291hjh2il09920061:12000
St. Charles silt loam, 0 to 2 percent slopes243A8602634548v4jil09920061:12000
St. Charles silt loam, 2 to 5 percent slopes243B438921335zxqhil10320041:12000
St. Charles silt loam, 0 to 2 percent slopes243A214921334zxqgil10320041:12000
St. Charles silt loam, 2 to 5 percent slopes243B120715960511qktjil10720061:12000
St. Charles silt loam, 5 to 10 percent slopes, eroded243C275815960521qktkil10720061:12000
St. Charles silt loam, 0 to 2 percent slopes243A59115960551qktnil10720061:12000
St. Charles silt loam, 0 to 2 percent slopes243A1426488892rlv3il11320001:12000
St. Charles silt loam, 2 to 5 percent slopes243B426488912rlv5il11320001:12000
St. Charles silt loam, 2 to 5 percent slopes243B94918212563j0il12319971:15840
St. Charles silt loam, 2 to 5 percent slopes243B57814063921j6ghil12920051:12000
St. Charles silt loam, 0 to 2 percent slopes243A26614063891j6gdil12920051:12000
St. Charles silt loam, 2 to 5 percent slopes243B318920857430758il14120051:12000
St. Charles silt loam, 5 to 10 percent slopes, eroded243C2182420857530759il14120051:12000
St. Charles silt loam, 0 to 2 percent slopes243A5562085737015il14120051:12000
St. Charles silt loam, 2 to 5 percent slopes243B83820897270g1il14319861:15840
St. Charles silt loam, 5 to 10 percent slopes, eroded243C236620897370g2il14319861:15840
St. Charles silt loam, 2 to 5 percent slopes243B5071914020227plil14720091:12000
St. Charles silt loam, 2 to 5 percent slopes243B8252020696s8cil16920001:12000
St. Charles silt loam, 2 to 5 percent slopes243B141017907860bqil17519921:15840
St. Charles silt loam, 0 to 2 percent slopes243A26817907760bpil17519921:15840
St. Charles silt loam, 2 to 5 percent slopes, rarely flooded7243B12925423892r1zfil17519921:15840
St. Charles silt loam, 5 to 10 percent slopes, eroded243C21495159201030759il17720061:12000
St. Charles silt loam, 2 to 5 percent slopes243B1415159200930758il17720061:12000
St. Charles silt loam, 0 to 2 percent slopes243A30617919460ggil17720061:12000
St. Charles silt loam, 0 to 2 percent slopes243A118417938260njil17919911:15840
St. Charles silt loam, 2 to 5 percent slopes243B104217938360nkil17919911:15840
St. Charles silt loam, 5 to 10 percent slopes, eroded243C298817938460nlil17919911:15840
St. Charles silt loam, 0 to 2 percent slopes, rarely flooded7243A14825097902qgxmil17919911:15840
St. Charles silt loam, 2 to 5 percent slopes243B271617399530758il20119971:12000
St. Charles silt loam, 5 to 10 percent slopes, eroded243C2148817399630759il20119971:12000
St. Charles silt loam, 0 to 2 percent slopes243A9731739945v1qil20119971:12000
St. Charles silt loam, 2 to 5 percent slopes243B345869198y5gnil20320081:12000
St. Charles silt loam, 0 to 2 percent slopes243A284869197y5gmil20320081:12000
St. Charles silt loam, 2 to 6 percent slopes, erodedSseB24024250484bqin04519991:12000
St. Charles silt loam, 2 to 6 percent slopesStB29021630695gp9in10719841:15840
St. Charles silt loam, 2 to 6 percent slopes, erodedSaB2172344233512szfbwi02119721:15840
St. Charles silt loam, 6 to 12 percent slopes, erodedSaC244544233522szdzwi02119721:15840
St. Charles silt loam, 0 to 2 percent slopesSaA18264233502szdxwi02119721:15840
St. Charles silt loam, 12 to 20 percent slopes, erodedSaD212354233532szf0wi02119721:15840
St. Charles silt loam, 20 to 30 percent slopesSaE69542335430756wi02119721:15840
St. Charles silt loam, 2 to 6 percent slopesScB347097535732szdywi02519721:15840
St. Charles silt loam, 0 to 2 percent slopesScA31817535722szdxwi02519721:15840
St. Charles silt loam, 6 to 12 percent slopes, erodedScC229077535742szdzwi02519721:15840
St. Charles silt loam, 12 to 20 percent slopes, erodedScD23047535752szf0wi02519721:15840
St. Charles silt loam, moderately well drained, 0 to 2 percent slopesSdA448394236442szf1wi02719761:15840
St. Charles silt loam, 2 to 6 percent slopesScB80314236422szdywi02719761:15840
St. Charles silt loam, 0 to 2 percent slopesScA59464236412szdxwi02719761:15840
St. Charles silt loam, 6 to 12 percent slopes, erodedScC235374236432szdzwi02719761:15840
St. Charles silt loam, gravelly subtratum, 2 to 6 percent slopesSeB6864236462szf3wi02719761:15840
St. Charles silt loam, gravelly subtratum, 0 to 2 percent slopesSeA4824236452szf2wi02719761:15840
St. Charles silt loam, 2 to 6 percent slopesScB59714255582szdywi03919671:15840
St. Charles silt loam, 0 to 2 percent slopesScA34554255572szdxwi03919671:15840
St. Charles silt loam, gravelly subtratum, 0 to 2 percent slopesSeA10184255592szf2wi03919671:15840
St. Charles silt loam, gravelly subtratum, 2 to 6 percent slopesSeB8594255602szf3wi03919671:15840
St. Charles silt loam, 2 to 6 percent slopesScB34234237552szdywi04719741:20000
St. Charles silt loam, 0 to 2 percent slopesScA14034237542szdxwi04719741:20000
St. Charles silt loam, 6 to 12 percent slopes, erodedScC26974237562szdzwi04719741:20000
St. Charles silt loam, moderately well drained, 2 to 6 percent slopesSbB365942382430753wi05519761:15840
St. Charles silt loam, moderately well drained, gravelly substratum, 2 to 6 percent slopesSfB239542382530754wi05519761:15840
St. Charles silt loam, moderately well drained, 0 to 2 percent slopesSbA14204238232szf1wi05519761:15840
St. Charles silt loam, 2 to 6 percent slopesSaB111444263812szdywi10519701:20000
St. Charles silt loam, gravelly subtratum, 2 to 6 percent slopesSbB46884263852szf3wi10519701:20000
St. Charles silt loam, gravelly subtratum, 0 to 2 percent slopesSbA44924263842szf2wi10519701:20000
St. Charles silt loam, 0 to 2 percent slopesSaA42884263802szdxwi10519701:20000
St. Charles silt loam, 6 to 12 percent slopes, erodedSaC28124263822szdzwi10519701:20000
St. Charles silt loam, gravelly substratum, 6 to 12 percent slopes, erodedSbC219442638630757wi10519701:20000
St. Charles silt loam, 12 to 20 percent slopes, erodedSaD28533810292szf0wi10519701:20000
St. Charles silt loam, 2 to 6 percent slopesScB43394232042szdywi11119771:15840
St. Charles silt loam, 6 to 12 percent slopes, erodedScC229574232052szdzwi11119771:15840
St. Charles silt loam, 12 to 20 percent slopes, erodedScD28004232062szf0wi11119771:15840
St. Charles silt loam, 2 to 6 percent slopesScB12464239262szdywi11719741:15840
St. Charles silt loam, 0 to 2 percent slopesScA9404239252szdxwi11719741:15840
St. Charles silt loam, gravelly subtratum, 0 to 2 percent slopesSeA87964256762szf2wi12719671:15840
St. Charles silt loam, gravelly subtratum, 2 to 6 percent slopesSeB49774256772szf3wi12719671:15840
St. Charles silt loam, 2 to 6 percent slopesScB35394256752szdywi12719671:15840
St. Charles silt loam, 0 to 2 percent slopesScA30974256742szdxwi12719671:15840
St. Charles silt loam, 2 to 6 percent slopesScB29134257702szdywi13119671:15840
St. Charles silt loam, 0 to 2 percent slopesScA14544257692szdxwi13119671:15840
St. Charles silt loam, gravelly subtratum, 2 to 6 percent slopesSeB5154257722szf3wi13119671:15840
St. Charles silt loam, gravelly subtratum, 0 to 2 percent slopesSeA3054257712szf2wi13119671:15840
St. Charles silt loam, 2 to 6 percent slopesScB13224228282szdywi13919771:20000
St. Charles silt loam, gravelly subtratum, 0 to 2 percent slopesSeA4644240972szf2wi60119671:15840
St. Charles silt loam, gravelly subtratum, 2 to 6 percent slopesSeB2344240982szf3wi60119671:15840
St. Charles silt loam, gravelly subtratum, 0 to 2 percent slopesSeA35114259182szf2wi60219671:15840
St. Charles silt loam, gravelly subtratum, 2 to 6 percent slopesSeB8444259192szf3wi60219671:15840
St. Charles silt loam, 2 to 6 percent slopesScB7104259172szdywi60219671:15840
St. Charles sandy loam, gravelly substratum, 1 to 3 percent slopesSaA48342591530755wi60219671:15840
St. Charles silt loam, 0 to 2 percent slopesScA3014259162szdxwi60219671:15840

Map of Series Extent

Approximate geographic distribution of the ST. CHARLES soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .