Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

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

Competing Series

Soil series competing with SHINDLER 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 SHINDLER 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 SHINDLER 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 SHINDLER, 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. SD-2012-03-15-84 | Moody County - April 1989

    Pattern of soils and parent material in the Kranzburg-Houdek association (Soil Survey of Moody County, SD; 1989).

  2. SD-2012-03-15-86 | Moody County - April 1989

    Pattern of soils and parent material in the Dempster-Flandreau-Lamo association (Soil Survey of Moody County, SD; 1989).

Map Units

Map units containing SHINDLER 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
Shindler clay loam, 15 to 45 percent slopesP44E16194768323cqhmn10120081:12000
Shindler clay loam, 15 to 45 percent slopesP44E442725508sbyhmn11720051:12000
Shindler clay loam, 15 to 45 percent slopesP44E358399566fds7mn13320021:12000
Egan-Shindler complex, 2 to 6 percent slopesEsB12312416640fzk0sd08319711:20000
Egan-Shindler complex, 6 to 9 percent slopesEsC7766416641fzk1sd08319711:20000
Steinauer-Shindler clay loams, 24 to 40 percent slopesSuF2902416659fzkmsd08319711:20000
Shindler-Egan complex, 9 to 15 percent slopes, erodedSkD22834416656fzkjsd08319711:20000
Shindler-Renner complex, 15 to 40 percent slopesSmF2361416657fzkksd08319711:20000
Shindler clay loam, 25 to 40 percent slopesShF1831416655fzkhsd08319711:20000
Shindler clay loam, 9 to 15 percent slopesShD689416654fzkgsd08319711:20000
Shindler and Talmo soils, 6 to 30 percent slopesStD574416658fzklsd08319711:20000
Crofton-Shindler complex, 9 to 15 percent slopesCsD3463446016gz3msd09919951:24000
Shindler-Houdek clay loams, 15 to 40 percent slopesSdE2736446074gz5hsd09919951:24000
Steinauer-Shindler clay loams, 25 to 60 percent slopesSsF2374446078gz5msd09919951:24000
Houdek-Shindler clay loams, 6 to 9 percent slopesHsC2240446050gz4qsd09919951:24000
Shindler-Talmo complex, 15 to 40 percent slopesSnE1256446075gz5jsd09919951:24000
Houdek-Shindler clay loams, 9 to 15 percent slopesHsD831446051gz4rsd09919951:24000
Houdek-Shindler clay loams, 6 to 25 percent slopesHsD4895418337g19rsd10119851:20000
Houdek-Shindler clay loams, 5 to 9 percent slopesHsC4411418336g19qsd10119851:20000
Shindler-Houdek clay loams, 15 to 40 percent slopesShE2156418353g1b8sd10119851:20000
Egan-Shindler complex, 2 to 6 percent slopesEaB3908453689h734sd12719741:20000
Egan-Shindler complex, 6 to 9 percent slopesEaC1233453690h735sd12719741:20000
Shindler clay loam, 9 to 15 percent slopesShD1199453721h745sd12719741:20000
Shindler clay loam, 15 to 30 percent slopesShE1171453722h746sd12719741:20000

Map of Series Extent

Approximate geographic distribution of the SHINDLER 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 .