Official Series Description


Lab Data Summary

Aggregate lab data for the CASS soil series. This aggregation is based on all pedons with a current taxon name of CASS, 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 CASS 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
102C04N0891S2004NE053001Cass5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4549103,-96.6895294
102C04N0892S2004NE053002Cass5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4517975,-96.6890717
102C04N0893S2004NE053004Cass5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4584694,-96.7460098
102C04N0894S2004NE053005Cass5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.504982,-96.7914276
102C04N0897S2004NE055040Cass5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3660622,-96.3960876
102C04N0898S2004NE055059Cass5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2151413,-96.2914581
10640A22401953NE155004Cass5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1491667,-96.3488889
7180P04151980NE079001Cass7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8427773,-98.3566666
7310KS157511510KS1575115Cass3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9613266,-97.8667068
7409KS157104009KS1571040cass3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8241272,-97.8218994
7410KS15700210KS157002cass3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6715851,-97.783165

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CASS 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 CASS 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 CASS 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 CASS 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 CASS 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 CASS 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 CASS 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 CASS, 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-2012-01-24-08 | Marion County - December 1983

    Typical pattern of soils and underlying material in the Lancaser-Hedville association (Soil Survey of Marion County, Kansas; 1983).

  2. 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).

  3. NE-2012-02-10-13 | Clay County - March 1981

    Typical pattern of soils in the Geary-Holder-Uly and the Hord-Cass-Hobbs associations showing the relationship of the soils to topography and parent material (Soil Survey of Clay County, Nebraska; March 1981).

  4. NE-2012-02-13-61 | Nance County - July 1960

    General soil areas of Nance County from a "bird's-eye view" (Soil Survey of Nance County, Nebraska; July 1960).

  5. NE-2012-02-13-62 | Nance County - July 1960

    Principal soils of Nance County (Soil Survey of Nance County, Nebraska; July 1960).

  6. NE-2012-02-13-63 | Nance County - July 1960

    A cross section along the eastern side of Nance County showing the relationship of the soils to the geological materials (Soil Survey of Nance County, Nebraska; July 1960).

  7. NE-2012-02-13-82 | Saunders County - January 1965

    Soils in the Sarpy-Barney association (Soil Survey of Saunders County, Nebraska; January 1965).

  8. NE-2012-02-13-83 | Saunders County - January 1965

    Soils in the Leshara-Wann association (Soil Survey of Saunders County, Nebraska; January 1965).

Map Units

Map units containing CASS 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
Cass variant loam152829497435tpco12119821:24000
Cass fine sandy loam, occasionally flooded3521464414546412zt6yks02719831:24000
Cass fine sandy loam, occasionally flooded3521250513820382zt6yks02919721:24000
Cass fine sandy loam, occasionally flooded352184313822022zt6yks05319851:24000
Cass fine sandy loam, rarely flooded37103811554042ywsqks07919701:24000
Cass fine sandy loam, rarely flooded3710314714292142ywsqks11319801:24000
Cass fine sandy loam, occasionally flooded352189113827612zt6yks11519811:24000
Cass fine sandy loam, occasionally flooded352171726056392zt6yks15719651:24000
Cass fine sandy loam, occasionally flooded3521217613821562zt6yks16919891:24000
Cass fine sandy loam, frequently flooded3520149314548751ktxgks20119881:24000
Cass fine sandy loam, occasionally flooded352159014548762zt6yks20119881:24000
Cass loam, occasionally flooded8436331416918841tsjxne00119701:20000
Cass fine sandy loam, rarely flooded371085416918981tskcne00119701:20000
Cass loam, rarely flooded843529316918971tskbne00119701:20000
Cass silt loam, occasionally flooded843912822160762dd0bne00119701:20000
Cass fine sandy loam, overwash, occasionally flooded84343522160752dd09ne00119701:20000
Cass loam, rarely flooded8435735426938gb86ne00319751:20000
Cass fine sandy loam, 0 to 2 percent slopes, rarely flooded37102854269372y22lne00319751:20000
Cass loam, occasionally flooded84361922159842dcxcne00319751:20000
Cass soils, rarely flooded8440729427031gbc6ne01119661:20000
Cass silt loam, occasionally flooded8439624013742lltpne01119661:20000
Cass fine sandy loam, 0 to 2 percent slopes, occasionally flooded352127473576182y226ne01519761:20000
Cass loam, rarely flooded84351422174862dfgtne01519761:20000
Cass fine sandy loam, rarely flooded371061417000431v213ne01919671:20000
Cass loam, rarely flooded843547417000381v20yne01919671:20000
Cass-Novina complex, occasionally flooded84422822160242dcynne02519811:20000
Cass silt loam, occasionally flooded8439119216921011tsrxne03519791:20000
Cass fine sandy loam, overwash, occasionally flooded843435816921001tsrwne03519791:20000
Cass loam, occasionally flooded8436522187772dgtgne03519791:20000
Cass fine sandy loam, 0 to 2 percent slopes, occasionally flooded352111164277622y226ne03919731:20000
Cass fine sandy loam, 0 to 2 percent slopes, rarely flooded371030022169832y22lne03919731:20000
Cass fine sandy loam, rarely flooded3710346716995761v1k1ne04119801:20000
Cass loam, rarely flooded84352015426876gb66ne05319751:20000
Cass fine sandy loam, 0 to 2 percent slopes, rarely flooded371017724268742y22lne05319751:20000
Cass fine sandy loam, clayey substratum, rarely flooded8433666426875gb65ne05319751:20000
Cass loam, occasionally flooded843631822170922df23ne05319751:20000
Cass fine sandy loam, 0 to 2 percent slopes, occasionally flooded352127622170882y226ne05319751:20000
Cass loam, clayey substratum, rarely flooded8438242426877gb67ne05319751:20000
Cass-Novina complex, occasionally flooded8442113817109361vfchne05520071:12000
Cass-Wann fine sandy loams, occasionally flooded8443102917109351vfcgne05520071:12000
Cass fine sandy loam, rarely flooded3710104716999301v1xgne07719871:20000
Cass fine sandy loam, rarely flooded371049961000893c4pne08919811:20000
Cass loam, occasionally flooded8436170316917641tsf1ne09519701:20000
Cass loam, rarely flooded843546216917871tsfsne09519701:20000
Cass loam, rarely flooded84351694357683d065ne10319771:20000
Cass loam, channeled, frequently flooded8437685357684d066ne10319771:20000
Cass fine sandy loam, calcareous variant, rarely flooded8432302816991481v137ne11119711:24000
Cass fine sandy loam, rarely flooded3710147416991471v136ne11119711:24000
Cass fine sandy loam, 0 to 2 percent slopes, occasionally flooded352114564273902y226ne11919811:20000
Cass loam, occasionally flooded8436839427391gbqtne11919811:20000
Cass fine sandy loam, 0 to 2 percent slopes, occasionally flooded352144294274662y226ne12519581:20000
Cass silt loam, occasionally flooded84393458427459gbt0ne12519581:20000
Cass loam, occasionally flooded8436206816920481tsq6ne12919741:20000
Cass fine sandy loam, occasionally flooded35211026057112zt6yne12919741:20000
Cass fine sandy loam, rarely flooded371031116917341tsd2ne13719671:20000
Cass fine sandy loam, 0 to 2 percent slopes, rarely flooded371012764275492y22lne13919701:20000
Cass loam, rarely flooded8435604427550gbwyne13919701:20000
Cass fine sandy loam, 0 to 2 percent slopes, occasionally flooded3521922171332y226ne13919701:20000
Cass fine sandy loam, 0 to 2 percent slopes, rarely flooded3710553316922802y22lne14319671:20000
Cass-Novina complex, occasionally flooded844276317110001vffkne15320071:12000
Cass-Wann fine sandy loams, occasionally flooded844366617109991vffjne15320071:12000
Cass fine sandy loam, 0 to 2 percent slopes, rarely flooded371018754268172y22lne16719801:20000
Cass fine sandy loam, 0 to 2 percent slopes, occasionally flooded35211622172162y226ne16719801:20000
Cass very fine sandy loam, rarely flooded8441432616924031tt2nne16919651:20000
Cass fine sandy loam, occasionally flooded3521100816924022zt6yne16919651:20000
Cass loam, occasionally flooded843620022187332dgs1ne16919651:20000
Cass loam, occasionally flooded8436975395531f8l2ne17720001:12000
Cass fine sandy loam, 0 to 2 percent slopes, occasionally flooded35216453955302y226ne17720001:12000
Cass fine sandy loam, channeledCd2370355233cxn4sd05319821:20000
Cass fine sandy loamCd1797354380cwrmsd12319751:20000
Cass fine sandy loam, 0 to 2 percent slopes, occasionally floodedCf2500370802dfvctx34119681:24000
Cass and Humbarger soils, 0 to 2 percent slopes, occasionally floodedCh5168372096dh63tx42119701:24000

Map of Series Extent

Approximate geographic distribution of the CASS 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 .