Official Series Description


Lab Data Summary

Aggregate lab data for the ELPASO soil series. This aggregation is based on all pedons with a current taxon name of ELPASO, 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 ELPASO 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
108A03N0301S2002IL099021ElPaso7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1976624,-89.0780411
108A13N0531S2012IL147001Elpaso6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9051333,-88.6269556

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ELPASO 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 ELPASO 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 ELPASO 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 ELPASO 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 ELPASO 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 ELPASO 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 ELPASO 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 mountains figure.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with ELPASO, 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. IL-2010-09-01-41 | Marshall County - 2002

    Typical pattern of soils and parent material in the Flanagan-Graymont-Elpaso association (Soil Survey of Marshall County, Illinois; 2002).

Map Units

Map units containing ELPASO 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
Elpaso silty clay loam, 0 to 2 percent slopes356A518968962t6zsil01120071:12000
Elpaso silty clay loam, 0 to 2 percent slopes356A650471838942t6zsil03719981:12000
Elpaso silty clay loam, 0 to 2 percent slopes356A152215474672t6zsil06320051:12000
Elpaso silty clay loam, 0 to 2 percent slopes356A117642714452t6zsil08920001:12000
Elpaso silty clay loam, 0 to 2 percent slopes356A1031317156152t6zsil09320071:12000
Elpaso silty clay loam, 0 to 2 percent slopes356A2530410299332t6zsil09920061:12000
Elpaso silty clay loam, 0 to 2 percent slopes356A1266211451152t6zsil10320041:12000
Drummer and Elpaso silty clay loams, 0 to 2 percent slopes721A38426488802ytpzil10519911:15840
Drummer and Elpaso silty clay loams, 0 to 2 percent slopes721A690016209602ytpzil11320001:12000
Elpaso silty clay loam, 0 to 2 percent slopes356A34071821692t6zsil12319971:15840
Elpaso silty clay loam, 0 to 2 percent slopes356A195214787952t6zsil14120051:12000
Drummer and Elpaso silty clay loams, 0 to 2 percent slopes721A113019129542ytpzil14720091:12000
Elpaso silty clay loam, 0 to 2 percent slopes356A9961728422t6zsil15519871:15840
Elpaso silty clay loam, 0 to 2 percent slopes356A100425423262t6zsil17519921:15840
Elpaso silty clay loam, 0 to 2 percent slopes356A147661983822t6zsil19720021:12000
Elpaso silty clay loam, 0 to 2 percent slopes356A322338692112t6zsil20320081:12000
Drummer and Elpaso silty clay loams, 0 to 2 percent slopes721A51821089482ytpzil20320081:12000

Map of Series Extent

Approximate geographic distribution of the ELPASO 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 .