Official Series Description


Lab Data Summary

Aggregate lab data for the STOY soil series. This aggregation is based on all pedons with a current taxon name of STOY, 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 STOY 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
114B78IL1570381978IL157038Stoy3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1976172,-89.69819
114B78IL1570391978IL157039Stoy3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2185642,-89.5969257
114B79IL1450111979IL145011Stoy1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9653765,-89.4201782
114B80IL1330081980IL133008Stoy1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2281221,-89.9394644
114B81P0041S1980IL157126STOY6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1175003,-89.769722
120CJN81101981IN071010Stoy2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9283972,-86.2202389
n/a40A5285S1954IN173001Stoy4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the STOY 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 STOY 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 STOY 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 STOY 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 STOY 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 STOY series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the STOY 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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

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

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with STOY, 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-2010-09-01-06 | Edgar County - 2002

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

  2. IL-2011-08-04-85 | Perry County - 1988

    Typical pattern of soils and parent material in the Stoy-Hosmer association (Soil Survey of Perry County, Illinois; 1988).

  3. IL-2011-08-04-88 | Perry County - 1988

    Typical pattern of soils and parent material in the Hosmer-Hickory-Blair association (Soil Survey of Perry County, Illinois; 1988).

  4. 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).

  5. IL-2011-08-05-01 | Wabash County - 1964

    General relationship of some Wabash County soils to physiographic position, relief, parent material, and native vegetation (Soil Survey of Wabash County, Illinois; 1964).

Map Units

Map units containing STOY 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
Stoy silt loam, 2 to 5 percent slopes164B22602020n6g0il00320021:12000
Stoy silt loam, 2 to 5 percent slopes, eroded164B230041738482tp16il00519811:12000
Stoy silt loam, 0 to 2 percent slopes164A25891738462tp12il00519811:12000
Stoy silt loam, 2 to 5 percent slopes164B23891738472tp14il00519811:12000
Stoy silt loam, 2 to 5 percent slopes164B223746386312tp14il02320061:12000
Stoy silt loam, 0 to 2 percent slopes164A139256386302tp12il02320061:12000
Stoy silt loam, 0 to 2 percent slopes164A89921957162tp12il03320041:12000
Stoy silt loam, 2 to 5 percent slopes164B14322000352tp14il03320041:12000
Stoy silt loam, 0 to 2 percent slopes164A2785843550x9s9il04519971:12000
Stoy silt loam, 2 to 5 percent slopes164B1980843551x9sbil04519971:12000
Stoy silt loam, 2 to 5 percent slopes164B21261754322tp14il04719671:15840
Stoy silt loam, 5 to 10 percent slopes, eroded164C28341754332tp19il04719671:15840
Stoy silt loam, 0 to 2 percent slopes164A2081754312tp12il04719671:15840
Stoy silt loam, 0 to 2 percent slopes164A10081733832tp12il05119911:15840
Stoy silt loam, 2 to 5 percent slopes164B4712116062tp14il05919661:20000
Stoy silt loam, 0 to 2 percent slopes164A1872116052tp12il05919661:20000
Stoy silt loam, 2 to 5 percent slopes164B53713881ryvfil06920031:12000
Stoy silt loam, 0 to 2 percent slopes164A7713880ryvdil06920031:12000
Stoy silt loam, 5 to 10 percent slopes, eroded164C26713882ryvgil06920031:12000
Stoy silt loam, 2 to 5 percent slopes164B377215378232tp14il07720061:12000
Stoy silt loam, 0 to 2 percent slopes164A142715378222tp12il07720061:12000
Stoy silt loam, 2 to 5 percent slopes, eroded164B21115387942tp16il07720061:12000
Stoy silt loam, 2 to 5 percent slopes164B86818254wgg9il08720051:12000
Stoy silt loam, 0 to 2 percent slopes164A36818253wgg8il08720051:12000
Stoy silt loam, 2 to 5 percent slopes164B48341766722tp14il10119521:42240
Stoy silt loam, 0 to 2 percent slopes164A5131766712tp12il10119521:42240
Stoy silt loam, 2 to 5 percent slopes, eroded164B21191766732tp16il10119521:42240
Stoy silt loam, 2 to 5 percent slopes164B3126807977w3rsil12720041:12000
Stoy silt loam, 0 to 2 percent slopes164A1589807976w3rril12720041:12000
Stoy silt loam, 5 to 10 percent slopes, eroded164C2550807978w3rtil12720041:12000
Stoy silt loam, 2 to 5 percent slopes164B916614054432tp14il14520051:12000
Stoy silt loam, 0 to 2 percent slopes164A680614054422tp12il14520051:12000
Stoy silt loam, 2 to 5 percent slopes, eroded164B2421514054442tp16il14520051:12000
Stoy silt loam, 2 to 5 percent slopes164B178606830ncg5il15120031:12000
Stoy silt loam, 5 to 10 percent slopes, eroded164C241606831ncg6il15120031:12000
Stoy silt loam, 0 to 2 percent slopes164A14606829ncg4il15120031:12000
Stoy silt loam, 2 to 5 percent slopes164B1512748895t48xil15320041:12000
Stoy silt loam, 0 to 2 percent slopes164A725749044t4fqil15320041:12000
Stoy silt loam, 2 to 5 percent slopes164B14611788632tp14il16519741:15840
Stoy silt loam, 0 to 2 percent slopes164A4291788622tp12il16519741:15840
Stoy silt loam, 2 to 5 percent slopes164B25501995416pmtil18120011:12000
Stoy silt loam, 0 to 2 percent slopes164A3421995336pmkil18120011:12000
Stoy silt loam, 2 to 5 percent slopes164B57831796262tp14il18519621:20000
Stoy silt loam, 0 to 2 percent slopes164A39331796252tp12il18519621:20000
Stoy silt loam, 2 to 5 percent slopes, eroded164B210711796272tp16il18519621:20000
Stoy silt loam, 5 to 10 percent slopes, eroded164C24961796292tp19il18519621:20000
Stoy silt loam, 5 to 10 percent slopes164C2781796282tp1bil18519621:20000
Stoy silty clay loam, 4 to 7 percent slopes, severely eroded164C36317963060xjil18519621:20000
Stoy silt loam, 2 to 5 percent slopes164B4715289362tp14il18920061:12000
Stoy silt loam, 0 to 2 percent slopes164A2315289312tp12il18920061:12000
Stoy silt loam, 2 to 5 percent slopes164B130315438782tp14il19320061:12000
Stoy silt loam, 0 to 2 percent slopes164A103415438772tp12il19320061:12000
Stoy silt loam, 2 to 5 percent slopes164B64014780932tp14il19920071:12000
Stoy silt loam, 2 to 5 percent slopes, eroded164B232314780942tp16il19920071:12000
Stoy silt loam, 0 to 2 percent slopes164A9114780922tp12il19920071:12000
Stoy silt loam, 0 to 2 percent slopesSvgA18971907355220rlin07119851:15840
Bedford-Stoy silt loams, 1 to 4 percent slopes complexBdyB145816515291sfk4in09319821:15840
Stoy silt loam, 0 to 2 percent slopesSvgA78116515481sfkrin09319821:15840

Map of Series Extent

Approximate geographic distribution of the STOY 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 .