Official Series Description


Lab Data Summary

Aggregate lab data for the STOOKEY soil series. This aggregation is based on all pedons with a current taxon name of STOOKEY, 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 STOOKEY 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
115C84IL0130091984IL013009Stookey2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9537694,-90.623125
131A95P019493IL003016EStookey6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2467383,-89.2931235

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the STOOKEY 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 STOOKEY 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 STOOKEY 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 STOOKEY 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.

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

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

Competing Series

Soil series competing with STOOKEY 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 STOOKEY 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 STOOKEY 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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There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with STOOKEY, 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

No block diagrams are available.

Map Units

Map units containing STOOKEY 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
Stookey silt loam, 2 to 5 percent slopes216B597723785912kv3ril00119971:12000
Stookey silt loam, 5 to 10 percent slopes, eroded216C2490323785922kv3sil00119971:12000
Stookey and Timula soils, 18 to 35 percent slopes856F352023786672kv66il00119971:12000
Stookey-Timula-Orthents complex, 1 to 7 percent slopes816B217723786622kv61il00119971:12000
Stookey silt loam, 10 to 18 percent slopes, eroded216D2203923785942kv3vil00119971:12000
Stookey and Timula soils, 35 to 60 percent slopes856G140223786682kv67il00119971:12000
Stookey-Timula-Orthents complex, 7 to 15 percent slopes816D39923786632kv62il00119971:12000
Stookey silt loam, 5 to 10 percent slopes, severely eroded216C317023785932kv3til00119971:12000
Stookey silt loam, 10 to 18 percent slopes, severely eroded216D314823785952kv3wil00119971:12000
Stookey-Clarksville complex, 18 to 35 percent slopes717F10610603211n7pfil00320021:12000
Stookey silt loam, 25 to 35 percent slopes216F6352602055n6h4il00320021:12000
Clarksville-Stookey complex, 35 to 70 percent slopes717G3258603212n7pgil00320021:12000
Stookey silt loam, 35 to 70 percent slopes216G1801602141n6kxil00320021:12000
Stookey silt loam, 18 to 25 percent slopes216E1629602047n6gwil00320021:12000
Stookey silt loam, 18 to 25 percent slopes, severely eroded216E3985602054n6h3il00320021:12000
Stookey silt loam, 10 to 18 percent slopes, eroded216D2740602051n6h0il00320021:12000
Stookey silt loam, 10 to 18 percent slopes216D473602050n6gzil00320021:12000
Stookey silt loam, 18 to 25 percent slopes, eroded216E2412602053n6h2il00320021:12000
Stookey silt, 35 to 60 percent slopes216G2670525186122qj69il01319861:15840
Stookey silt, 18 to 35 percent slopes216F2084325189392r21cil01319861:15840
Stookey silt loam, 5 to 10 percent slopes, eroded216C298341755045wmfil01319861:15840
Stookey silt loam, 10 to 18 percent slopes, eroded216D289691755055wmgil01319861:15840
Stookey silt loam, 18 to 35 percent slopes, severely eroded216F3321025423582qj66il01319861:15840
Stookey silt loam, 2 to 5 percent slopes216B9391755035wmdil01319861:15840
Stookey silt loam, terrace, 10 to 18 percent slopes, eroded9216D265225423762qzktil01319861:15840
Stookey and Timula soils, 35 to 60 percent slopes856G16825423642qzkcil01319861:15840
Stookey and Timula soils, 18 to 35 percent slopes856F1271755065wmhil01319861:15840
Stookey silt loam, terrace, 5 to 10 percent slopes, eroded9216C212425186082qj5xil01319861:15840
Stookey and Timula soils, 18 to 25 percent slopes, eroded856E27625186142qj62il01319861:15840
Stookey silt, terrace, 18 to 35 percent slopes9216F2225186132qj64il01319861:15840
Stookey silt loam, 2 to 5 percent slopes216B21821751695w8mil06719931:15840
Stookey silt loam, 5 to 10 percent slopes, eroded216C217331751705w8nil06719931:15840
Stookey silt loam, 10 to 18 percent slopes, severely eroded216D37761751715w8pil06719931:15840
Stookey silt loam, 0 to 2 percent slopes216A2831751685w8lil06719931:15840
Stookey silt loam, 35 to 70 percent slopes216G806018406665jmil13319981:12000
Stookey and Timula soils, 18 to 25 percent slopes, eroded856E2162302011406r9dil14920011:12000
Stookey and Timula soils, 35 to 60 percent slopes856G97212012846rg1il14920011:12000
Stookey silt loam, 5 to 10 percent slopes, eroded216C267292012766rfsil14920011:12000
Stookey silt loam, 10 to 18 percent slopes, eroded216D237112012786rfvil14920011:12000
Stookey silt loam, 2 to 5 percent slopes216B22962012756rfril14920011:12000
Stookey silt loam, 5 to 10 percent slopes, severely eroded216C38392012776rftil14920011:12000
Stookey silt loam, 10 to 18 percent slopes, severely eroded216D38162012796rfwil14920011:12000
Stookey and Timula soils, 18 to 35 percent slopes856F2882012806rfxil14920011:12000
Stookey-Clarksville complex, 18 to 35 percent slopes717F382748926t49xil15320041:12000
Stookey silt loam, 25 to 35 percent slopes216F265748911t49fil15320041:12000
Stookey silt loam, 18 to 25 percent slopes, eroded216E2107748909t49cil15320041:12000
Stookey silt loam, 10 to 18 percent slopes, eroded216D282748907t499il15320041:12000
Clarksville-Stookey complex, 35 to 70 percent slopes717G29748927t49yil15320041:12000
Stookey silt loam, 35 to 70 percent slopes216G27748912t49gil15320041:12000
Stookey silt loam, 18 to 25 percent slopes, severely eroded216E325748910t49dil15320041:12000
Stookey silt loam, 18 to 25 percent slopes216E9748908t49bil15320041:12000
Stookey silt loam, 35 to 70 percent slopes216G17182004716qltil15720011:12000

Map of Series Extent

Approximate geographic distribution of the STOOKEY 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 .