Official Series Description


Lab Data Summary

Aggregate lab data for the STOKLY soil series. This aggregation is based on all pedons with a current taxon name of STOKLY, 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 STOKLY were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
12405KY-019-00105KY019 Stokly-OSDStokly3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3118057,-82.7448883
12583P070382KY195005Stokly6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5216675,-82.6108322

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

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

Click the image to view it full size.

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

Click the image to view it full size.

Geomorphic description summaries for the STOKLY 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

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

Click the image to view it full size.

Select annual climate data summaries for the STOKLY 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 STOKLY 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 STOKLY, 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. KY-2012-01-31-25 | Knox County and Eastern Part of Whitley County - May 1988

    Pattern of soils, topography, and underlying material in the Shelocta-Latham-DeKalb map unit (Soil Survey of Knox County and Eastern Part of Whitley County, Kentucky; May 1988).

Map Units

Map units containing STOKLY 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
Stokly fine sandy loamSv3766550264lglgky04319801:20000
Stokly fine sandy loam, occasionally floodedSt902552538ljytky05119941:24000
Stokly sandy loam, occasionally floodedSt315551474lhvhky05719911:20000
Stokly sandy loam, frequently floodedSt43618846562184cky06320071:12000
Hayter-Potomac-Stokly complex, 2 to 15 percent slopesHpC13645550036lgc3ky19519861:24000
Stokly fine sandy loamSn2262550425lgrnky60519751:20000
Stokly fine sandy loam, frequently floodedSv2060552236ljn2ky62719841:20000
Atkins-Stokly complex, 0 to 3 percent slopes, frequently flooded303714612219nk20ky63019661:15840
Shelocta-Grigsby-Stokly complex, 2 to 15 percent slopesShC11774550881lh7cky63919911:24000
Stokly fine sandy loam, occasionally floodedSt895550882lh7dky63919911:24000
Stokly-Philo silt loams, 0 to 3 percent slopes, frequently floodedSkP1AF106424418552myyjoh00919811:15840
Pope-Stokly silt loams, 0 to 3 percent slopes, frequently floodedPpS1AF84024418542myyhoh00919811:15840
Pope-Stokly silt loams, 0 to 3 percent slopes, frequently floodedPpS1AF329124504432n7wkoh05319881:15840
Stokly-Philo silt loams, 0 to 3 percent slopes, frequently floodedSkP1AF220524504552n7wyoh05319881:15840
Pope-Stokly silt loams, 0 to 3 percent slopes, frequently floodedPpS1AF160424506562n83foh07319861:15840
Stokly-Philo silt loams, 0 to 3 percent slopes, frequently floodedSkP1AF20824506272n82hoh07319861:15840
Stokly-Philo silt loams, 0 to 3 percent slopes, frequently floodedSkP1AF310724510242n8h9oh07919811:15840
Pope-Stokly silt loams, 0 to 3 percent slopes, frequently floodedPpS1AF259424511102n8l2oh08719891:15840
Stokly-Philo silt loams, 0 to 3 percent slopes, frequently floodedSkP1AF38424511182n8lboh08719891:15840
Pope-Stokly silt loams, 0 to 3 percent slopes, frequently floodedPpS1AF19024512852n8rqoh10519911:15840
Stokly-Philo silt loams, 0 to 3 percent slopes, frequently floodedSkP1AF7524512872n8rsoh10519911:15840
Stokly-Philo silt loams, 0 to 3 percent slopes, frequently floodedSkP1AF329124533772nby6oh16319981:15840
Pope-Stokly silt loams, 0 to 3 percent slopes, frequently floodedPpS1AF186624533742nby3oh16319981:15840

Map of Series Extent

Approximate geographic distribution of the STOKLY 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 .