Official Series Description


Lab Data Summary

Aggregate lab data for the ELS soil series. This aggregation is based on all pedons with a current taxon name of ELS, 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 ELS were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
6587P01671986NE009053Els6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0508224,-99.8595928
6588P003287NE031102Els7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.4527779,-100.9349976
6592P035091NE031025Els7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.6236115,-100.7050018
6540A2083S1977NE089002Els6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.416378,-98.8437271
6540A2084S1977NE149001Els6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3447113,-99.35569

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the ELS series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the ELS series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the ELS 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 .

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with ELS share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the ELS series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the ELS 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 .

Click the image to view it full size.

Click the image to view it full size.

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 ELS, 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-2012-02-08-06 | Blaine County - September 1993

    Typical pattern of soils and parent material in the Valentine-Els-Ipage association (Soil Survey of Blaine County, Nebraska; September 1993).

  2. NE-2012-02-08-09 | Brown County - April 1992

    Typical pattern of soils and parent material in the Valentine association (Soil Survey of Brown County, Nebraska; April 1992).

  3. NE-2012-02-10-19 | Custer County - July 1982

    Typical pattern of soils in the Valentine association, rolling and hilly, and relationship of soils to topography and parent material (Soil Survey of Custer County, Nebraska; July 1982).

  4. NE-2012-02-13-08 | Garfield County - February 1988

    Typical pattern of soils and parent material in the Els-Valentine-Tryon association (Soil Survey of Garfield County, Nebraska; February 1988).

  5. 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).

  6. NE-2012-02-13-28 | Holt County - March 1983

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

  7. 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).

  8. NE-2012-02-13-37 | Kearney County - September 1984

    Typical pattern of soils in the Valentine association (Soil Survey of Kearney County, Nebraska; September 1984).

  9. NE-2012-02-13-52 | Loup County - October 1990

    Typical pattern of soils and parent material in the Valentine-Tryon-Ipage association (Soil Survey of Loup County, Nebraska; October 1990).

  10. NE-2012-02-13-55 | Morrill County - August 1985

    Pattern of soils, topography, and underlying material in the Valentine association (Soil Survey of Morrill County, Nebraska; August 1985).

  11. 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).

  12. NE-2012-02-13-71 | Platte County - September 1988

    Typical landscape pattern of the soils and the underlying material in the Valentine-Thurman association (Soil Survey of Platte County, Nebraska; September 1988).

  13. 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).

  14. NE-2012-02-13-79 | Rock County - May 1985

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

  15. NE-2012-02-13-95 | Sheridan County - 2002

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

  16. NE-2012-02-14-15 | Wheeler County - September 1988

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

  17. 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).

  18. NE-2012-02-14-18 | Wheeler County - September 1988

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

Map Units

Map units containing ELS 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
Els loamy sand269979450635blco07519741:24000
Els loamy sand, rarely flooded3730111713821222zt61ks14319781:24000
Valentine-Els complex, 0 to 9 percent slopes4861395822282422s81lne00519731:24000
Ipage-Els complex, 0 to 3 percent slopes451863626687082v9w0ne00519731:24000
Els, calcareous-Hoffland complex, 0 to 3 percent slopes453629422190832s810ne00519731:24000
Els-Ipage complex, 0 to 3 percent slopes45421622616994812s81hne00919881:20000
Valentine-Els complex, moist, 0 to 9 percent slopes4858915528765782s81mne00919881:20000
Els-Tryon complex, 0 to 3 percent slopes4563449622191532wgdqne00919881:20000
Els loamy sand, 0 to 3 percent slopes4533243016994801v1fyne00919881:20000
Els-Ipage fine sands, 0 to 3 percent slopes454565322191512s81jne00919881:20000
Valentine-Els complex, 0 to 9 percent slopes48616128765772s81lne00919881:20000
Els fine sand, 0 to 3 percent slopes4521322174762s81fne01319801:20000
Valentine-Els complex, moist, 0 to 9 percent slopes48584243028765802s81mne01719871:20000
Els-Ipage fine sands, 0 to 3 percent slopes454519804999862s81jne01719871:20000
Els-Tryon complex, 0 to 3 percent slopes4563851622191732wgdqne01719871:20000
Valentine-Els complex, 0 to 9 percent slopes4861690728765792s81lne01719871:20000
Loup-Els complex, 0 to 3 percent slopes467566471000102zbfdne01719871:20000
Els loamy sand, 0 to 3 percent slopes45334043999851v1fyne01719871:20000
Els fine sand, 0 to 3 percent slopes45213822191712s81fne01719871:20000
Valentine-Els complex, 0 to 9 percent slopes4861480881004542s81lne03119951:24000
Els-Tryon complex, 0 to 3 percent slopes4563475031003712wgdqne03119951:24000
Els-Ipage fine sands, 0 to 3 percent slopes4545290221003702s81jne03119951:24000
Els, calcareous-Hoffland complex, 0 to 3 percent slopes4536137131003722s810ne03119951:24000
Els fine sand, 0 to 3 percent slopes452175191003692s81fne03119951:24000
Els, calcareous-Selia fine sands, 0 to 3 percent slopes454031241003733cfvne03119951:24000
Els-Ipage complex, 0 to 3 percent slopes4542359422281792s81hne04119801:20000
Els fine sand, 0 to 3 percent slopes4521165716995852s81fne04119801:20000
Els fine sand, calcareous, 0 to 3 percent slopes45243122175562dfk2ne04519731:20000
Els fine sand, calcareous, 0 to 3 percent slopes4524468716987392s81kne06919951:20000
Valentine-Els complex, moist, 0 to 9 percent slopes48581783828765742s81mne07119841:20000
Els-Ipage complex, 0 to 3 percent slopes45421325216997752s81hne07119841:20000
Els loamy sand, 0 to 3 percent slopes4533448816997741v1fyne07119841:20000
Els-Ipage fine sands, 0 to 3 percent slopes4545206722192632s81jne07119841:20000
Els fine sand, 0 to 3 percent slopes4521499016988392s81fne07519731:24000
Valentine-Els complex, 0 to 9 percent slopes486116626686672s81lne07519731:24000
Els fine sand, calcareous, 0 to 3 percent slopes45248922192942s81kne07519731:24000
Ipage-Els complex, 0 to 3 percent slopes45187426687092v9w0ne07519731:24000
Els, calcareous-Hoffland complex, 0 to 3 percent slopes45362922192792s810ne07519731:24000
Els-Ipage fine sands, 0 to 3 percent slopes45451822192802s81jne07519731:24000
Els-Tryon complex, 0 to 3 percent slopes4563109917001181v23jne07920031:12000
Els-Ipage complex, 0 to 3 percent slopes45421344261000942s81hne08919811:20000
Valentine-Els complex, moist, 0 to 9 percent slopes485810587728765722s81mne08919811:20000
Els loamy sand, 0 to 3 percent slopes4533348291000931v1fyne08919811:20000
Els-Ipage fine sands, 0 to 3 percent slopes4545317922196162s81jne08919811:20000
Els-Ipage-Tryon loamy sands, 0 to 6 percent slopes454861122196242dhpsne08919811:20000
Valentine-Els complex, 0 to 9 percent slopes48611622196222s81lne08919811:20000
Els-Tryon complex, 0 to 3 percent slopes4563722196272wgdqne08919811:20000
Valentine-Els complex, 0 to 9 percent slopes4861210626687022s81lne09119611:24000
Ipage-Els complex, 0 to 3 percent slopes451867326686832v9w0ne09119611:24000
Els, calcareous-Hoffland complex, 0 to 3 percent slopes453643826686812s810ne09119611:24000
Els-Tryon complex, 0 to 3 percent slopes456329122289012dtc1ne09319681:12000
Els loamy fine sand, 0 to 3 percent slopes45275722289212dtcpne09319681:12000
Valentine-Els loamy fine sands, 0 to 9 percent slopes4863721316918781tsjqne09919821:20000
Els fine sand, 0 to 3 percent slopes4521103643576892s81fne10319771:20000
Els and Elsmere fine sands, 0 to 3 percent slopes4519940616993531v19vne11319691:24000
Els fine sand, 0 to 3 percent slopes452184622197942s81fne11319691:24000
Valentine-Els complex, 0 to 9 percent slopes486112926057042s81lne11319691:24000
Els-Ipage fine sands, 0 to 3 percent slopes4545663816995262s81jne11519861:20000
Valentine-Els complex, moist, 0 to 9 percent slopes4858622128765732s81mne11519861:20000
Els-Tryon complex, 0 to 3 percent slopes4563213716995532wgdqne11519861:20000
Els loamy sand, 0 to 3 percent slopes453379316995251v1fyne11519861:20000
Valentine-Els complex, 0 to 9 percent slopes48611525817002342s81lne11719661:31680
Ipage-Els complex, 0 to 3 percent slopes4518339826687102v9w0ne11719661:31680
Els, calcareous-Hoffland complex, 0 to 3 percent slopes4536238617002162s810ne11719661:31680
Ipage-Els loamy fine sands, 0 to 3 percent slopes4654269817096511vd11ne12119781:20000
Els loamy fine sand, 0 to 3 percent slopes4527209217096331vd0gne12119781:20000
Els fine sand, 0 to 3 percent slopes45211297416926072s81fne12319811:20000
Els loamy fine sand, 0 to 3 percent slopes4527192516926081tt98ne12319811:20000
Els fine sand, calcareous, 0 to 3 percent slopes452426922203562s81kne12319811:20000
Els loamy fine sand, 0 to 3 percent slopes452722922289782dtfjne12519581:20000
Ipage-Els loamy fine sands, 0 to 3 percent slopes4654622289792dtfkne12519581:20000
Valentine-Els loamy fine sands, 0 to 9 percent slopes4863822194662dhjpne13719671:20000
Ipage-Els loamy fine sands, 0 to 3 percent slopes46541368427646gc01ne14119841:20000
Els loamy fine sand, 0 to 3 percent slopes4527853427629gbzhne14119841:20000
Valentine-Els complex, moist, 0 to 9 percent slopes4858819311002682s81mne14919821:20000
Els-Ipage complex, 0 to 3 percent slopes4542623431002362s81hne14919821:20000
Els-Tryon complex, 0 to 3 percent slopes4563416741002602wgdqne14919821:20000
Els loamy sand, 0 to 3 percent slopes4533111221002351v1fyne14919821:20000
Els-Ipage-Tryon loamy sands, 0 to 6 percent slopes454870721002373c9gne14919821:20000
Els-Ipage fine sands, 0 to 3 percent slopes4545255422198322s81jne14919821:20000
Valentine-Els complex, 0 to 9 percent slopes486145328766642s81lne14919821:20000
Els, calcareous-Ipage complex, 0 to 3 percent slopes4539111941005843cnnne16119921:20000
Els fine sand, calcareous, 0 to 3 percent slopes452441981005822s81kne16119921:20000
Els, calcareous-Hoffland complex, 0 to 3 percent slopes453641761005832s810ne16119921:20000
Els, calcareous-Tryon complex, 0 to 3 percent slopes45417681005853cnpne16119921:20000
Els-Ipage fine sands, 0 to 3 percent slopes45451922198492s81jne16119921:20000
Els, calcareous-Selia fine sands, 0 to 3 percent slopes45401522198482dhy0ne16119921:20000
Valentine-Els complex, 0 to 9 percent slopes486134626056912s81lne17119631:24000
Els-Ipage fine sands, 0 to 3 percent slopes45452598716998332s81jne18319841:20000
Valentine-Els complex, moist, 0 to 9 percent slopes48582318216998682s81mne18319841:20000
Els loamy sand, 0 to 3 percent slopes4533757616998321v1fyne18319841:20000
Abiquiu, occasionaly flooded-Els families complex, 0 to 15 percent slopes1132329342372wghpnm6781:24000
Valentine-Els complex, 0 to 9 percent slopesT158C492813901272s81lsd00720041:20000
Els-Tryon complex, 0 to 3 percent slopesT055A142013900602wgdqsd00720041:20000
Els-Ipage fine sands, 0 to 3 percent slopesT054A129413900592s81jsd00720041:20000
Els, calcareous-Hoffland complex, 0 to 3 percent slopesT052A110213900572s810sd00720041:20000
Els fine sand, 0 to 3 percent slopesT050A21713900552s81fsd00720041:20000
Els fine sand, calcareous, 0 to 3 percent slopesT051A19413900562s81ksd00720041:20000
Els, calcareous-Selia fine sands, 0 to 2 percent slopesT053A2713900581hnglsd00720041:20000
Ipage-Els loamy fine sandsIa1479354800cx65sd11119781:20000
Ipage-Els-Shue complex, 0 to 6 percent slopesIe1841356589cz1wsd11519971:24000
Els, calcareous-Hoffland complex, 0 to 3 percent slopesT052A127313915452s810sd12119671:31680
Valentine-Els complex, 0 to 9 percent slopesT158C107313919972s81lsd12119671:31680
Els, calcareous-Selia complex, 0 to 1 percent slopesSa863353033cvc5sd12119671:31680
Els-Tryon complex, 0 to 3 percent slopesT055A72313915482wgdqsd12119671:31680
Els-Ipage fine sands, 0 to 3 percent slopesT054A71813915472s81jsd12119671:31680
Els fine sand, calcareous, 0 to 3 percent slopesT051A16113915442s81ksd12119671:31680
Els fine sand, 0 to 3 percent slopesT050A2013915432s81fsd12119671:31680
Valentine-Els complex, 0 to 9 percent slopesT158C133025827942s81lsd61320111:24000
Els, calcareous-Hoffland complex, 0 to 3 percent slopesT052A57825827622s810sd61320111:24000
Els-Tryon complex, 0 to 3 percent slopesT055A30325827642wgdqsd61320111:24000
Els-Ipage fine sands, 0 to 3 percent slopesT054A14025827632s81jsd61320111:24000
Els fine sand, 0 to 3 percent slopesT050A3925827602s81fsd61320111:24000
Els fine sand, calcareous, 0 to 3 percent slopesT051A2825827612s81ksd61320111:24000

Map of Series Extent

Approximate geographic distribution of the ELS 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 .