Official Series Description


Lab Data Summary

Aggregate lab data for the WILDHORSE soil series. This aggregation is based on all pedons with a current taxon name of WILDHORSE, 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 WILDHORSE 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
6581P012480NE161002Wildhorse7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0461121,-102.398056
6581P012580NE161003Wildhorse7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0305557,-102.3897247
6581P012780NE161005Wildhorse7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.2391663,-102.4427795
6581P013080NE161008Wildhorse7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.1844444,-102.4377747
6581P013180NE161009Wildhorse7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.185833,-102.4380569
6581P013480NE161012Wildhorse7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.2913895,-102.4613876

Water Balance

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

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

Competing Series

Soil series competing with WILDHORSE 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 WILDHORSE 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 WILDHORSE 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 WILDHORSE, 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. NE-2010-09-09-03 | Garden County - 1999

    Typical pattern of the soils and underlying material in the Valent-Wildhorse-Ipage calcareous association (Soil Survey of Garden County, Nebraska; 1999).

  2. NE-2012-02-13-02 | Garden County - 1999

    Typical pattern of the soils and underlying material in the Valent-Wildhorse-Ipage calcareous association (Soil Survey of Garden County, Nebraska; 1999).

  3. NE-2012-02-13-60 | Morrill County - August 1985

    A generalized cross section of Morrill County that shows the relationship of parent material, soil associations, and elevation (Soil Survey of Morrill County, Nebraska; August 1985).

  4. NE-2012-02-13-96 | Sheridan County - 2002

    Typical pattern of soils and parent material in the Valent-Wildhorse association (Soil Survey of Sheridan County, Nebraska; 2002).

Map Units

Map units containing WILDHORSE 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
Wildhorse-Hoffland complex, 0 to 3 percent slopes489761824347362v9wkne00519731:24000
Wildhorse fine sand, 0 to 3 percent slopes48943922174512vzryne01319801:20000
Wildhorse-Hoffland complex, 0 to 3 percent slopes48971122174702v9wkne01319801:20000
Wildhorse-Ipage, calcareous complex, 0 to 3 percent slopes4898322174712v9wjne01319801:20000
Wildhorse fine sand, 0 to 3 percent slopes489437441004602vzryne03119951:24000
Wildhorse-Ipage, calcareous complex, 0 to 3 percent slopes48982308616987882v9wjne06919951:20000
Wildhorse fine sand, 0 to 3 percent slopes4894916116987862vzryne06919951:20000
Wildhorse-Hoffland complex, 0 to 3 percent slopes4897853016987872v9wkne06919951:20000
Wildhorse fine sand, 0 to 3 percent slopes4894266322192912vzryne07519731:24000
Wildhorse-Ipage, calcareous complex, 0 to 3 percent slopes489811322192982v9wjne07519731:24000
Wildhorse-Hoffland complex, 0 to 3 percent slopes48974026686712v9wkne07519731:24000
Wildhorse-Hoffland complex, 0 to 3 percent slopes489720726687052v9wkne09119611:24000
Wildhorse fine sand, 0 to 3 percent slopes48941090522203602vzryne12319811:20000
Wildhorse-Ipage, calcareous complex, 0 to 3 percent slopes48982622203612v9wjne12319811:20000
Wildhorse loamy fine sand, 0 to 3 percent slopes489587416536861shsqne15719651:20000
Wildhorse-Ipage, calcareous complex, 0 to 3 percent slopes4898291921006642v9wjne16119921:20000
Wildhorse-Hoffland complex, 0 to 3 percent slopes4897226161006632v9wkne16119921:20000
Wildhorse fine sand, 0 to 3 percent slopes489472311006622vzryne16119921:20000
Wildhorse loamy fine sand, 0 to 3 percent slopes48951194358062d0ldne16519931:20000

Map of Series Extent

Approximate geographic distribution of the WILDHORSE 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 .