Official Series Description


Lab Data Summary

Aggregate lab data for the ELSMERE soil series. This aggregation is based on all pedons with a current taxon name of ELSMERE, 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 ELSMERE 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
6580P018980NE149003Elsmere7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.521946,-99.5363922
6592P034691NE031021Elsmere7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.5086098,-100.9288864
6540A2086S1977NE089004Elsmere6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3272133,-98.8515091

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ELSMERE 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 ELSMERE 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 ELSMERE 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 ELSMERE 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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Click the image to view it full size.

Competing Series

Soil series competing with ELSMERE 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 ELSMERE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the ELSMERE 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 ELSMERE, 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-2012-02-10-24 | Dundy County - February 1963

    Typical area in the Valentine soil association (Soil Survey of Dundy County, Nebraska; February 1963).

  2. NE-2012-02-10-29 | Dundy County - February 1963

    The Bridgeport-Havre soil association, on the right, merges with the Sandy alluvial land-Las association (Soil Survey of Dundy County, Nebraska; February 1963).

  3. NE-2012-02-13-20 | Hall County - January 1962

    Ovina-Elsmere association in the north-central part of Hall County (Soil Survey of Hall County, Nebraska; January 1962).

  4. NE-2012-02-13-27 | Holt County - March 1983

    Typical pattern of soils in the Els-Valentine-Ipage association and their relationship to topography and parent material (Soil Survey of Holt County, Nebraska; March 1983).

  5. NE-2012-02-13-29 | Holt County - March 1983

    Typical pattern of soils in the Elsmere-Ipage-Loup association and their relationship to topography and parent material (Soil Survey of Holt County, Nebraska; March 1983).

  6. NE-2012-02-13-33 | Hooker County - January 1964

    Diagram showing typical topography, soils, and parent materials in Hooker County. Symbols below soil names identify range sites, as follows: CS=Choppy Sands; WL=Wet Land; Sb=Subirrigated; Sv=Sandy; So=Sands; and TB=Thin Breaks (Soil Survey of Hooker County, Nebraska; January 1964).

  7. NE-2012-02-13-54 | Loup County - October 1990

    Typical pattern of soils and parent material in the Ipage-Valentine-Elsmere and Almeria-Calamus-Bolent associations (Soil Survey of Loup County, Nebraska; October 1990).

  8. NE-2012-02-13-77 | Rock County - May 1985

    Typical pattern of soils and parent material in the Els-Valentine-Tryon association (Soil Survey of Rock County, Nebraska; May 1985).

  9. NE-2012-02-13-78 | Rock County - May 1985

    Typical pattern of soils and parent material in the Loup-Elsmere association (Soil Survey of Rock County, Nebraska; May 1985).

  10. NE-2012-02-14-07 | Thomas County - August 1965

    Diagram showing typical soils and parent materials in Thomas County. Symbols below soil names identify range sites as follows: (Sa) Sands; (CS) Choppy Sands; (Sy) Sandy; (Sb) Subirrigated; (WL) Wet Land; (TB) Thin Breaks; (SwG) Shallow to Gravel (Soil Survey of Thomas County, Nebraska; August 1965).

  11. NE-2012-02-14-17 | Wheeler County - September 1988

    Pattern of soils and parent material in the Els-Valentine-Ipage association (Soil Survey of Wheeler County, Nebraska; September 1988).

  12. OK-2012-02-16-30 | Ellis County - April 1966

    Major soils of associations 7, 8, and 10 (Soil Survey of Ellis County, Oklahoma; April 1966).

  13. OK-2012-02-17-60 | Woodward County - November 1963

    Typical pattern of soils of the Port association (Soil Survey of Woodward County, Oklahoma; November 1963).

  14. OK-2012-02-17-61 | Woodward County - November 1963

    Typical pattern of soils of the Lincoln-Las Animas association (Soil Survey of Woodward County, Oklahoma; November 1963).

  15. SD-2010-11-01-16 | Spink County - 2009

    Pattern of soils and underlying materials in the Hand-Carthage-Forestburg association (Soil Survey of Spink County, South Dakota; 2009).

  16. SD-2012-03-14-01 | Bennett County - May 1971

    Typical association of Valentine, Mosher, Minatare, Loup, Keith, Rosebud, Oglala, and Canyon soils in the southern part of Bennett County (Soil Survey of Bennett County, SD; 1971).

  17. SD-2012-03-15-95 | Shannon County - April 1971

    Representative pattern of soils in associations 9 and 14 (Soil Survey of Shannon County, SD; 1971).

  18. SD-2012-03-15-99 | Todd County - April 1974

    Typical pattern of soils in associations 8 and 10. Areas of association 10 are commonly within areas of association 8 (Soil Survey of Todd County, SD; 1974).

Map Units

Map units containing ELSMERE 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
Elsmere loamy fine sandEl2559493435sdco11519691:15840
Elsmere fine sandy loam, rarely flooded373583514545362zt62ks04119771:24000
Elsmere fine sand, 0 to 3 percent slopes45504079426950gb8lne00319751:20000
Elsmere loamy fine sand, 0 to 3 percent slopes455322344269512v9vtne00319751:20000
Elsmere-Ipage loamy fine sands, 0 to 3 percent slopes456069722159462vzsdne00319751:20000
Elsmere fine sandy loam, 0 to 3 percent slopes43522822159412vzs3ne00319751:20000
Elsmere loamy fine sand, calcareous, 0 to 3 percent slopes4556109622190842v9vwne00519731:24000
Elsmere loamy fine sand, 0 to 3 percent slopes455358916989352v9vtne00519731:24000
Elsmere fine sand, 0 to 3 percent slopes45501875427033gbc8ne01119661:20000
Elsmere loamy fine sand, 0 to 3 percent slopes455317324270322v9vtne01119661:20000
Elsmere loamy fine sand, 0 to 3 percent slopes43512716999872vzs2ne01719871:20000
Elsmere-Loup complex, 0 to 3 percent slopes456122322191722v9vyne01719871:20000
Elsmere-Loup complex, 0 to 3 percent slopes4561194751003762v9vyne03119951:24000
Elsmere loamy fine sand, 0 to 3 percent slopes455376141003742v9vtne03119951:24000
Elsmere loamy fine sand, calcareous, 0 to 3 percent slopes455675811003752v9vwne03119951:24000
Selia loamy fine sand, 0 to 3 percent slopes4559113716996761v1n8ne04719751:20000
Elsmere loamy fine sand, loamy substratum, 0 to 3 percent slopes4558103416996751v1n7ne04719751:20000
Elsmere loamy fine sand, calcareous, 0 to 3 percent slopes45561024796402v9vwne06919951:20000
Elsmere-Selia loamy fine sands, 0 to 3 percent slopes4562186016997772vzsfne07119841:20000
Elsmere loamy fine sand, 0 to 3 percent slopes435197416997762vzs2ne07119841:20000
Elsmere loamy fine sand, 0 to 3 percent slopes45531452716988412v9vtne07519731:24000
Elsmere loamy fine sand, calcareous, 0 to 3 percent slopes455626322192812v9vwne07519731:24000
Elsmere-Loup complex, 0 to 3 percent slopes4561526686722v9vyne07519731:24000
Elsmere-Ipage loamy fine sands, 0 to 3 percent slopes4560560961000982vzsdne08919811:20000
Elsmere loamy fine sand, 0 to 3 percent slopes4553443471000952v9vtne08919811:20000
Elsmere fine sandy loam, 0 to 3 percent slopes4352296621000972vzs3ne08919811:20000
Elsmere-Selia loamy fine sands, 0 to 3 percent slopes4562142461000992vzsfne08919811:20000
Elsmere loamy fine sand, clayey substratum, 0 to 3 percent slopes455718711000963c4xne08919811:20000
Elsmere loamy fine sand, 0 to 3 percent slopes435110322196302vzs2ne08919811:20000
Elsmere-Loup complex, 0 to 3 percent slopes456140626686922v9vyne09119611:24000
Elsmere loamy fine sand, calcareous, 0 to 3 percent slopes455630126686912v9vwne09119611:24000
Elsmere loamy fine sand, 0 to 3 percent slopes455312226686822v9vtne09119611:24000
Elsmere loamy fine sand, 0 to 2 percent slopes, rarely flooded45531823997002y22jne09319681:12000
Elsmere loamy fine sand, calcareous, 0 to 3 percent slopes45561522195972v9vwne10119901:20000
Elsmere loamy fine sand, 0 to 3 percent slopes455384083576902v9vtne10319771:20000
Elsmere fine sandy loam, rarely flooded43521047849252xhq7ne10719891:20000
Elsmere loamy fine sand, 0 to 2 percent slopes, rarely flooded455318011442362y22jne10719891:20000
Elsmere fine sandy loam, rarely flooded, wet43544925704662r98hne10719891:20000
Elsmere loamy fine sand, 0 to 3 percent slopes4351763816991632vzs2ne11119711:24000
Elsmere complex, 0 to 6 percent slopes4549118316991641v13rne11119711:24000
Elsmere loamy fine sand, loamy substratum, 0 to 3 percent slopes4558422197882dhw2ne11119711:24000
Els and Elsmere fine sands, 0 to 3 percent slopes4519940616993531v19vne11319691:24000
Elsmere loamy fine sand, 0 to 3 percent slopes455399316995272v9vtne11519861:20000
Elsmere loamy fine sand, calcareous, 0 to 3 percent slopes455641917002192v9vwne11719661:31680
Elsmere loamy fine sand, 0 to 3 percent slopes455317617002182v9vtne11719661:31680
Elsmere loamy fine sand, 0 to 2 percent slopes, rarely flooded4553110004273992y22jne11919811:20000
Elsmere fine sandy loam, rarely flooded4352943427400gbr3ne11919811:20000
Elsmere loamy fine sand, 0 to 2 percent slopes, rarely flooded45536654274502y22jne12519581:20000
Elsmere loamy fine sand, 0 to 2 percent slopes, rarely flooded455395884275632y22jne13919701:20000
Elsmere fine sandy loam, rarely flooded43524522171372df3kne13919701:20000
Elsmere loamy fine sand, 0 to 3 percent slopes4553162071002382v9vtne14919821:20000
Elsmere-Selia loamy fine sands, 0 to 3 percent slopes456229111002392vzsfne14919821:20000
Elsmere loamy fine sand, 0 to 3 percent slopes455314011005862v9vtne16119921:20000
Elsmere loamy fine sand, 0 to 2 percent slopes, rarely flooded455334454268272y22jne16719801:20000
Elsmere-Loup complex, 0 to 3 percent slopes45611140216998362v9vyne18319841:20000
Elsmere loamy fine sand, 0 to 3 percent slopes4553890216998342v9vtne18319841:20000
Elsmere-Ipage loamy fine sands, 0 to 3 percent slopes4560752616998352vzsdne18319841:20000
Elsmere-Selia loamy fine sands, 0 to 3 percent slopes456221616998372vzsfne18319841:20000
Elsmere loamy fine sand, loamy substratumEm2999354569cwyqsd00519761:20000
Elsmere-Loup complex, 0 to 3 percent slopesT059A267113900642v9vysd00720041:20000
Dunday-Elsmere loamy fine sands, 0 to 3 percent slopesDu2446352733cv1hsd00720041:20000
Elsmere loamy fine sand, calcareous, 0 to 3 percent slopesT057A84813900622v9vwsd00720041:20000
Elsmere, calcareous-hoffland complex, 0 to 2 percent slopesT058A71213900631hngrsd00720041:20000
Elsmere loamy fine sand, 0 to 3 percent slopesT056A50013900612v9vtsd00720041:20000
Elsmere loamy fine sand, loamy substratumEa6271354781cx5ksd11119781:20000
Elsmere-Orwet complexEb1474354782cx5lsd11119781:20000
Forestburg-Elsmere loamy sands, 0 to 2 percent slopesFf6077356613cz2nsd11519971:24000
Forestburg-Elsmere-Toko complex, 0 to 2 percent slopesFh2664356614cz2psd11519971:24000
Elsmere loamy sand, 0 to 2 percent slopesEk475356603cz2bsd11519971:24000
Loup-Elsmere loamy fine sandsLe15967353013cvbjsd12119671:31680
Elsmere loamy fine sand, 0 to 3 percent slopesElA9578352988cv9qsd12119671:31680
Elsmere-Loup complex, 0 to 3 percent slopesT059A99713915522v9vysd12119671:31680
Elsmere, calcareous-hoffland complex, 0 to 2 percent slopesT058A32013915511hq0rsd12119671:31680
Elsmere loamy fine sand, 0 to 3 percent slopesT056A15013915492v9vtsd12119671:31680
Elsmere loamy fine sand, calcareous, 0 to 3 percent slopesT057A13913915502v9vwsd12119671:31680
Doger-Elsmere complex, 0 to 3 percent slopesDmA14000354386cwrtsd12319751:20000
Elsmere fine sandy loamEm6696354389cwrxsd12319751:20000
Elsmere-Loup complex, 0 to 3 percent slopesT059A71125827682v9vysd61320111:24000
Lamo-Elsmere complex, 0 to 3 percent slopesLe4792582715cv3xsd61320111:24000
Elsmere loamy fine sand, calcareous, 0 to 3 percent slopesT057A17025827662v9vwsd61320111:24000
Elsmere, calcareous-hoffland complex, 0 to 2 percent slopesT058A16225827671hv2wsd61320111:24000
Elsmere loamy fine sand, 0 to 3 percent slopesT056A13325827652v9vtsd61320111:24000

Map of Series Extent

Approximate geographic distribution of the ELSMERE 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 .