Official Series Description


Lab Data Summary

Aggregate lab data for the HIDEWOOD soil series. This aggregation is based on all pedons with a current taxon name of HIDEWOOD, 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 HIDEWOOD 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 HIDEWOOD 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 HIDEWOOD 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 HIDEWOOD 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 HIDEWOOD 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 hills figure.

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

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

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Competing Series

Soil series competing with HIDEWOOD 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 HIDEWOOD 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 HIDEWOOD 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 hills figure.

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 HIDEWOOD, 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-2012-03-15-02 | Codington County - December 1966

    Diagram showing the relative position of the major soils in association 3 (Soil Survey of Codington County, SD; 1966).

  2. SD-2012-03-15-80 | Minnehaha County - June 1964

    Block diagram showing the geographical association of the soils in association 4. Here, the soils formed in a mantle of loess which lies over glacial till (Soil Survey of Minnehaha County, SD; 1964).

  3. SD-2012-03-15-81 | Minnehaha County - June 1964

    Block diagram showing the geographical association of the soils in association 9. Here, the soils formed in loess and till (Soil Survey of Minnehaha County, SD; 1964).

Map Units

Map units containing HIDEWOOD 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
Hidewood-Badger complex, 0 to 2 percent slopesJ93A3942991430128nmmn08120071:12000
Hidewood-Badger complex, 0 to 2 percent slopesJ93A28839888851260jmn10120081:12000
Hidewood-Badger complex, 0 to 2 percent slopesJ93A26869780042v5pnmn11720051:12000
Hidewood silty clay loamHw2338428349gcqqmn14919661:15840
McKranz-Hidewood, frequently flooded, silty clay loams, 0 to 2 percent slopesZ116A306427130062qjmrsd02920061:12000
Hidewood silty clay loam, 0 to 2 percent slopes, frequently floodedZ252A74727652582qkmgsd02920061:12000
McKranz-Hidewood, frequently flooded, silty clay loams, 0 to 2 percent slopesZ116A1027653962qjmrsd03719921:20000
McKranz-Hidewood, frequently flooded, silty clay loams, 0 to 2 percent slopesZ116A1427129522qjmrsd03919921:20000
McKranz-Hidewood, frequently flooded, silty clay loams, 0 to 2 percent slopesZ116A29627128622qjmrsd05119771:20000
Hidewood silty clay loam, 0 to 2 percent slopes, frequently floodedZ252A5427129142qkmgsd05119771:20000
McKranz-Hidewood, frequently flooded, silty clay loams, 0 to 2 percent slopesZ116A10227127762qjmrsd10919771:20000

Map of Series Extent

Approximate geographic distribution of the HIDEWOOD 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 .