Official Series Description


Lab Data Summary

Aggregate lab data for the ELTREE soil series. This aggregation is based on all pedons with a current taxon name of ELTREE, 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 ELTREE 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
7370KS05101270KS051012Eltree2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.706974,-99.2881317
7310N0480S10KS167001Eltree7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9501953,-98.663002
7302N0487S2001KS163001Eltree7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4438896,-99.2291641

Water Balance

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

Soil series sharing subgroup-level classification with ELTREE, 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-2012-03-14-06 | Bon Homme County - January 1983

    Pattern of soils and underlying material in the Eltree-Yankton-Alcester association (Soil Survey of Bon Homme County, SD; 1983).

Map Units

Map units containing ELTREE 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
Eltree silt loam, 1 to 3 percent slopes2605633026056312xmlwks05119701:24000
Eltree silt loam, 3 to 7 percent slopes2606522211501232xmlxks05119701:24000
Eltree silt loam, 0 to 1 percent slopes2604210726056302xmlvks05119701:24000
Eltree silt loam, 7 to 15 percent slopes260770411501242xmlyks05119701:24000
Eltree silt loam, 1 to 3 percent slopes2605408626056342xmlwks06519851:24000
Eltree silt loam, 1 to 3 percent slopes2605214126056332xmlwks16319801:24000
Eltree silt loam, 3 to 7 percent slopes2606511502342xmlxks16319801:24000
Eltree silt loam, 1 to 3 percent slopes2605392526056352xmlwks16719801:24000
Eltree silt loam, 3 to 7 percent slopes26061011509542xmlxks16719801:24000
Eltree silt loam, 1 to 3 percent slopes26056626056322xmlwks19519861:24000
Eltree silt loam, 3 to 7 percent slopes26065511508462xmlxks19519861:24000
Eltree silt loam, 0 to 2 percent slopes256120093576242y22vne01519761:20000
Eltree silt loam, 2 to 6 percent slopes256325434270992y22wne02719821:20000
Eltree silt loam, 6 to 11 percent slopes2564841427100gbffne02719821:20000
Eltree silt loam, 0 to 2 percent slopes25615644270982y22vne02719821:20000
Eltree silt loam, 0 to 2 percent slopes25617324343942y22vne10719891:20000
Eltree silt loam, 2 to 6 percent slopes256363011442392y22wne10719891:20000
Eltree silt loam, 2 to 6 percent slopesEaB33654182602y22wsd00919811:20000
Eltree silt loam, 0 to 2 percent slopesEaA29034182592y22vsd00919811:20000
Eltree-Crofton silt loams, 9 to 15 percent slopesEcD999418263g17csd00919811:20000
Eltree-Ethan complex, 6 to 9 percent slopesEbC653418261g179sd00919811:20000
Eltree-Ethan complex, 9 to 40 percent slopesEbE577418262g17bsd00919811:20000

Map of Series Extent

Approximate geographic distribution of the ELTREE 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 .