Official Series Description


Lab Data Summary

Aggregate lab data for the LANCASTER soil series. This aggregation is based on all pedons with a current taxon name of LANCASTER, 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 LANCASTER 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
10616N0187S2015NE095500Lancaster7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1025,-97.06008
7402KS02900402KS029004Lancaster3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3636475,-97.5983734
7440A1793S1953KS169005LANCASTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8280563,-97.7802811
7440A1794S1953KS169006LANCASTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8122559,-97.8581238
7481P0658S1981KS115001LANCASTER7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5974998,-97.3208313
7402N0361S2002KS029002Lancaster7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3623085,-97.6008377
7501KS20104001KS201040Lancaster3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8901482,-97.1787415

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LANCASTER 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 LANCASTER 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 LANCASTER 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 LANCASTER 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with LANCASTER 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 LANCASTER 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 LANCASTER 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 LANCASTER, 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. KS-2012-01-20-30 | Clay County - September 1984

    Typical pattern of soils and underlying material in the Crete-Lancaster-Hedville association (Soil Survey of Clay County, Kansas; 1984).

  2. KS-2012-01-20-59 | Ellsworth County - February 1989

    Pattern of soils and parent material in the Lancaster-Hedville-Harney association (Soil Survey of Ellsworth County, Kansas; 1989).

  3. KS-2012-01-24-02 | Lincoln County - May 1985

    Typical pattern of soils and parent material in the Geary-Harney-Lancaster association (Soil Survey of Lincoln County, Kansas; 1985).

  4. KS-2012-01-24-03 | Lincoln County - May 1985

    Typical pattern of soils and parent material in the Lancaster-Hedville association (Soil Survey of Lincoln County, Kansas; 1985).

  5. KS-2012-01-24-11 | McPherson County - April 1983

    Typical pattern of soils in the Lancaster-Hedville-Edalgo association (Soil Survey of McPherson County, Kansas; 1983).

  6. KS-2012-01-25-22 | Republic County - November 1967

    Distribution of the soils in the Lancaster-Hedville-Crete association (Soil Survey of Republic County, Kansas; 1967).

  7. KS-2012-01-25-25 | Rice County - December 1974

    Distribution of the soils in the Smolan-Crete-Hobbs association (Soil Survey of Rice County, Kansas; 1974).

  8. KS-2012-01-25-26 | Rice County - December 1974

    Distribution of the soils in the Hedville-Lancaster-Smolan association (Soil Survey of Rice County, Kansas; 1974).

  9. KS-2012-01-25-28 | Saline County - May 1992

    Pattern of soils and parent material in the Wells-Crete-Lancaster association (Soil Survey of Saline County, Kansas; 1992).

  10. KS-2012-01-25-29 | Saline County - May 1992

    Pattern of soils and parent material in the Lancaster-Hedville-Crete association (Soil Survey of Saline County, Kansas; 1992).

  11. KS-2012-01-26-27 | Washington County - August 1993

    Typical pattern of soils and parent material in the Crete-Lancaster-Longford association (Soil Survey of Washington County, Kansas; 1993).

  12. NE-2012-02-08-17 | Gage County - May 1964

    Schematic diagram showing the relationship of major soil series to parent materials in Gage County, Nebraska (Soil Survey of Gage County, Nebraska; May 1964).

Map Units

Map units containing LANCASTER 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
Lancaster-Hedville complex, 3 to 20 percent slopes3396261126687562r8ygks00919791:24000
Lancaster loam, 1 to 3 percent slopes3390914404712tpvzks00919791:24000
Lancaster-Hedville complex, 3 to 20 percent slopes33962312726687642r8ygks02719831:24000
Lancaster loam, 3 to 7 percent slopes3391524326687631igwnks02719831:24000
Lancaster-Hedville complex, 3 to 20 percent slopes33961217726687672r8ygks02919721:24000
Lancaster loam, 3 to 7 percent slopes33913526687661igwnks02919721:24000
Lancaster-Armo loams, 3 to 7 percent slopes33952013820332tpw2ks02919721:24000
Lancaster-Hedville complex, 3 to 20 percent slopes3396280626687692r8yjks03319871:24000
Lancaster-Hedville complex, 3 to 20 percent slopes3396626126687732r8ygks04119771:24000
Lancaster-Hedville complex, 3 to 20 percent slopes33968114626687772r8ygks05319851:24000
Lancaster loam, 3 to 7 percent slopes, eroded33928613822202tpw0ks05319851:24000
Lancaster loam, 1 to 3 percent slopes33904613822192tpvzks05319851:24000
Lancaster-Hedville complex, 3 to 20 percent slopes3396558926687822r8yjks09719831:24000
Lancaster-Hedville complex, 3 to 20 percent slopes33964159826687842r8ygks10519831:24000
Geary-Lancaster complex, 5 to 10 percent slopes38523880927333362r9d2ks10519831:24000
Lancaster loam, 3 to 7 percent slopes3391117526687831igwnks10519831:24000
Lancaster-Armo loams, 3 to 7 percent slopes339516013820932tpw2ks10519831:24000
Lancaster-Hedville complex, 3 to 20 percent slopes33966250226687942r8ygks11319801:24000
Lancaster loam, 3 to 7 percent slopes33911043126687931igwnks11319801:24000
Lancaster loam, 1 to 3 percent slopes33901814292062tpvzks11319801:24000
Lancaster loam, 3 to 7 percent slopes33911116726687901igwnks11519811:24000
Lancaster-Hedville complex, 3 to 20 percent slopes3396706426687912r8ygks11519811:24000
Lancaster loam, 1 to 3 percent slopes3390596313827872tpvzks11519811:24000
Lancaster-Armo loams, 3 to 7 percent slopes3395183713819832tpw2ks12319771:24000
Lancaster-Hedville complex, 3 to 20 percent slopes3396165426687962r8ygks12319771:24000
Geary-Lancaster complex, 5 to 10 percent slopes385228527333442r9d2ks12319771:24000
Lancaster loam, 3 to 7 percent slopes33916326687951igwnks12319771:24000
Lancaster loam, 3 to 7 percent slopes3391996026688041igwnks14319781:24000
Lancaster-Hedville complex, 3 to 20 percent slopes3396785626688052r8ygks14319781:24000
Lancaster-Hedville complex, 3 to 20 percent slopes3396475326688072r8ygks15719651:24000
Lancaster loam, 3 to 7 percent slopes33919226688061igwnks15719651:24000
Lancaster loam, 1 to 3 percent slopes3390563214332322tpvzks15919711:24000
Hedville-Lancaster complex, 5 to 20 percent slopes3381505514332312ww0mks15919711:24000
Lancaster-Hedville complex, 3 to 20 percent slopes3396435226688092r8ygks15919711:24000
Lancaster loam, 3 to 7 percent slopes, eroded3392235314332342tpw0ks15919711:24000
Lancaster loam, 3 to 7 percent slopes33914926688081igwnks15919711:24000
Lancaster loam, 3 to 7 percent slopes3391426688111igwnks16119701:24000
Lancaster-Hedville complex, 3 to 20 percent slopes33962014926688132r8ygks16719801:24000
Lancaster loam, 3 to 7 percent slopes3391178526688121igwnks16719801:24000
Lancaster-Hedville complex, 3 to 20 percent slopes33969237026688152r8ygks16919891:24000
Lancaster loam, 3 to 7 percent slopes3391826326688141igwnks16919891:24000
Lancaster-Hedville complex, 3 to 20 percent slopes33964714126688242r8ygks20119881:24000
Lancaster loam, 3 to 7 percent slopes33911961026688231igwnks20119881:24000
Lancaster loam, 7 to 11 percent slopes417332216911122tpw6ne06720001:12000
Lancaster loam, 3 to 7 percent slopes339124326687441igwnne06720001:12000
Lancaster and Edalgo soils, 11 to 30 percent slopes41701169616918162tpw5ne09519701:20000
Lancaster loam, 3 to 7 percent slopes, eroded3392342816918142tpw1ne09519701:20000
Lancaster loam, 7 to 11 percent slopes4173240216918152tpw6ne09519701:20000
Lancaster soils, 7 to 11 percent slopes, severely eroded4175189016918131tsgmne09519701:20000
Lancaster loam, 7 to 16 percent slopes, severely eroded417421816924311tt3kne16919651:20000
Lancaster soils, 7 to 11 percent slopes, severely eroded41754722187382dgs6ne16919651:20000

Map of Series Extent

Approximate geographic distribution of the LANCASTER 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 .