Official Series Description


Lab Data Summary

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

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Competing Series

Soil series competing with EVRIDGE 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 EVRIDGE 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 EVRIDGE 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.

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

Soil series sharing subgroup-level classification with EVRIDGE, 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-2012-03-15-10 | Corson County - July 1995

    Pattern of soils and parent material in the Bullock-Parchin association (Soil Survey of Corson County, SD; 1995).

  2. SD-2012-03-16-07 | Ziebach County - March 1990

    Pattern of soils and parent material in the Bullock-Vebar-Parchin association (Soil Survey of Ziebach County, SD; 1990).

Map Units

Map units containing EVRIDGE 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
Evridge-Desart-Telfer fine sandy loams, 0 to 6 percent slopesE1259B59326990491jv3vnd00719981:24000
Evridge-Whitebird fine sandy loams, 6 to 15 percent slopesE1263D13692563550d1x7nd01119691:20000
Evridge-Whitebird fine sandy loams, 6 to 15 percent slopesE1263D116322525867d1x7nd03719851:20000
Evridge-Whitebird fine sandy loams, 6 to 15 percent slopesE1263D482759667d1x7nd05919981:20000
Evridge-Whitebird fine sandy loams, 6 to 15 percent slopesE1263D120552699083d1x7nd08519921:24000
Evridge-Desart-Telfer complex, 6 to 15 percent slopesE1261D72942699082d1x6nd08519921:24000
Evridge-Whitebird fine sandy loams, 6 to 15 percent slopesE1263D2022707395d1x7nd08719741:20000
Evridge-Desart-Telfer fine sandy loams, 0 to 6 percent slopesE1259B20027159891jv3vnd08919651:20000
Evridge-Desart-Telfer complex, 6 to 15 percent slopesE1261D1612715990d1x6nd08919651:20000
Evridge-Parchin fine sandy loams, 0 to 6 percent slopesExB19027356158cylzsd03119861:24000
Evridge-Bullock fine sandy loams, 0 to 6 percent slopesEwB5655356157cylysd03119861:24000
Evridge fine sandy loam, 0 to 6 percent slopesEvB5408356156cylxsd03119861:24000
Evridge loamy fine sand, 0 to 6 percent slopesEvB3124355839cy8psd13719851:24000

Map of Series Extent

Approximate geographic distribution of the EVRIDGE 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 .