Official Series Description


Lab Data Summary

Aggregate lab data for the COULTERVILLE soil series. This aggregation is based on all pedons with a current taxon name of COULTERVILLE, 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 COULTERVILLE 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
11380IL0490301980IL049030Coulterville1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1461237,-88.75323
11389IL0271821989IL027182Coulterville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5638056,-89.2651056
11389IL0271861989IL027186Coulterville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7274194,-89.3597194
11391P016690IL189082Coulterville7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3736111,-89.4194444
11391P016790IL189083Coulterville7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3744444,-89.4186111
11391P0294S1990IL189038COULTERVILLE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4680557,-89.3249969
11391P0296S1990IL189041COULTERVILLE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4680557,-89.3249969
11391P0301S1990IL189046COULTERVILLE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3805542,-89.4375
11391P0305S1990IL189050COULTERVILLE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3819427,-89.4388885
11391P0306S1990IL189051COULTERVILLE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3819427,-89.4402771
11302N0146S2002IL145002Coulterville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9789734,-89.2206116
11302N0149S2002IL145005Coulterville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9778061,-89.2204971
114B77IL1570171977IL157017Coulterville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2095976,-89.6628195
114B77IL1570181977IL157018Coulterville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0739885,-89.7289992
114B77IL1570231977IL157023Coulterville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2088641,-89.9788962
114B79IL1330101979IL133010Coulterville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.300271,-90.0034943
114B79IL1330411979IL133041Coulterville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2303803,-90.0485846
114B79IL1570591979IL157059Coulterville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0452529,-89.6343156
114B80IL1330411980IL133041Coulterville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2951266,-89.9968386
114B80IL1570921980IL157092Coulterville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1935365,-89.9811241
114B80IL1571061980IL157106Coulterville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2033115,-89.8447197
114B81IL1330181981IL133018Coulterville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2117251,-90.0458011
114B89IL0271841989IL027184Coulterville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.539375,-89.4531611
114B89IL0271871989IL027187Coulterville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7373667,-89.4271556
114B89IL0271881989IL027188Coulterville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7279667,-89.6148083
114B89IL1890041989IL189004Coulterville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2544667,-89.6652111
114B89IL1890111989IL189011Coulterville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2375694,-89.6565972
114B89IL1890121989IL189012Coulterville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2388694,-89.6652028
114B40A2797S1974IL163005Coulterville6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3806076,-89.9853668
114B81P0038S1980IL157127COULTERVILLE6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0908318,-89.8494415
114B94P0272S1993IL163014Coulterville6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4113884,-90.0041656
115B94P0271S1993IL163013Coulterville7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4805565,-90.0519409

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COULTERVILLE 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 COULTERVILLE 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 COULTERVILLE 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 COULTERVILLE 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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Click the image to view it full size.

Competing Series

Soil series competing with COULTERVILLE 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 COULTERVILLE 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 COULTERVILLE 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.

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

Click the image to view it full size.

Soil series sharing subgroup-level classification with COULTERVILLE, 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-2010-08-31-10 | Cumberland County - 2002

    Typical pattern of soils and parent material in the Wynoose-Bluford association (Soil Survey of Cumberland County, Illinois; 2002).

  2. IL-2010-08-31-13 | Cumberland County - 2002

    Typical pattern of soils and parent material in the Bluford-Wynoose-Darmstadt association (Soil Survey of Cumberland County, Illinois; 2002).

  3. IL-2010-09-01-78 | Washington County - 1998

    Typical pattern of soils and parent material in the Marine-Rushville-Muren association (Soil Survey of Washington County, Illinois; 1998).

  4. IL-2010-09-01-79 | Washington County - 1998

    Typical pattern of soils and parent material in the Oconee-Darmstadt-Coulterville association (Soil Survey of Washington County, Illinois; 1998).

  5. IL-2011-08-04-98 | Randolph County - 1988

    Pattern of soils and parent material in the Coulterville-Oconee association (Soil Survey of Randolph County, Illinois; 1988).

  6. IL-2011-08-05-02 | Washington County - 1998

    Typical pattern of soils and parent material in the Marine-Rushville-Muren association (Soil Survey of Washington County, Illinois; 1998).

  7. IL-2011-08-05-04 | Washington County - 1998

    Typical pattern of soils and parent material in the Oconee-Darmstadt-Coulterville association (Soil Survey of Washington County, Illinois; 1998).

Map Units

Map units containing COULTERVILLE 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
Oconee-Darmstadt-Coulterville silt loams, 0 to 2 percent slopes882A54692617722ytt1il02119991:12000
Coulterville silt loam, 2 to 5 percent slopes, eroded621B213511748495vy9il03519921:15840
Coulterville-Darmstadt silt loams, 2 to 5 percent slopes, eroded880B29811992356p9yil11719991:12000
Oconee-Darmstadt-Coulterville silt loams, 2 to 5 percent slopes882B531992366p9zil11719991:12000
Oconee-Darmstadt-Coulterville silt loams, 2 to 5 percent slopes882B95111989746p1jil11920011:12000
Coulterville-Darmstadt silt loams, 2 to 5 percent slopes, eroded880B245151989726p1gil11920011:12000
Coulterville-Grantfork silty clay loams, 5 to 10 percent slopes, severely eroded878C342381989736p1hil11920011:12000
Bunkum-Coulterville silt loams, 2 to 5 percent slopes, eroded884B2128618415265mdil13319981:12000
Bunkum-Coulterville silty clay loams, 5 to 10 percent slopes, severely eroded884C3128218415365mfil13319981:12000
Oconee-Darmstadt-Coulterville silt loams, 0 to 2 percent slopes882A751841502ytt1il13319981:12000
Coulterville-Grantfork silty clay loams, 5 to 10 percent slopes, severely eroded878C34418414765m7il13319981:12000
Coulterville-Darmstadt silt loams, 2 to 5 percent slopes, eroded880B24218414865m8il13319981:12000
Oconee-Darmstadt-Coulterville silt loams, 2 to 5 percent slopes882B1618415165mcil13319981:12000
Oconee-Darmstadt-Coulterville silt loams, 2 to 5 percent slopes, eroded882B22149917215471vsdsil13520071:12000
Oconee-Darmstadt-Coulterville silt loams, 0 to 2 percent slopes882A457017213842ytt1il13520071:12000
Oconee-Darmstadt-Coulterville silt loams, 2 to 5 percent slopes882B74717213861vs7lil13520071:12000
Oconee-Darmstadt-Coulterville silt loams, 0 to 2 percent slopes882A208916005972ytt1il14520051:12000
Bunkum-Coulterville silt loams, 2 to 5 percent slopes, eroded884B21614592571kzgtil14520051:12000
Bunkum-Coulterville silt loams, 2 to 5 percent slopes, eroded884B284892005376qnyil15720011:12000
Coulterville-Oconee silt loams, 0 to 2 percent slopes909A82762005386qnzil15720011:12000
Coulterville-Oconee silt loams, 2 to 5 percent slopes909B49062005396qp0il15720011:12000
Bunkum-Coulterville silty clay loams, 5 to 10 percent slopes, severely eroded884C325792005366qnxil15720011:12000
Bunkum-Coulterville silty clay loams, 10 to 18 percent slopes, severely eroded884D323232005356qnwil15720011:12000
Bunkum-Coulterville silty clay loams, 5 to 10 percent slopes, severely eroded884C31198818317364ltil16319971:12000
Coulterville-Grantfork silty clay loams, 5 to 10 percent slopes, severely eroded878C3906518316764lmil16319971:12000
Coulterville-Darmstadt silt loams, 2 to 5 percent slopes, eroded880B2778118316964lpil16319971:12000
Oconee-Darmstadt-Coulterville silt loams, 0 to 2 percent slopes882A65521831712ytt1il16319971:12000
Oconee-Darmstadt-Coulterville silt loams, 2 to 5 percent slopes882B443618317264lsil16319971:12000
Oconee-Darmstadt-Coulterville silt loams, 0 to 2 percent slopes882A3534215424942ytt1il18920061:12000
Darmstadt-Coulterville silt loams, 2 to 5 percent slopes, eroded880B21950815289621nb0cil18920061:12000
Oconee-Darmstadt-Coulterville silt loams, 2 to 5 percent slopes882B357315424961ns2yil18920061:12000
Coulterville-Grantfork silty clay loams, 5 to 10 percent slopes, severely eroded878C3257715425031ns35il18920061:12000
Coulterville-Grantfork silt loams, 5 to 10 percent slopes, eroded878C2123516004961qqfxil18920061:12000
Bunkum-Coulterville silt loams, 2 to 5 percent slopes, eroded884B27815425071ns39il18920061:12000

Map of Series Extent

Approximate geographic distribution of the COULTERVILLE 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 .