Official Series Description


Lab Data Summary

Aggregate lab data for the SHELLABARGER soil series. This aggregation is based on all pedons with a current taxon name of SHELLABARGER, 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 SHELLABARGER 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
10600KS17701100KS177011Shellabarger3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1221046,-95.8938522
10694P080694KS177001Shellabarger6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1208344,-95.8722229
7600KS17701200KS177012Shellabarger3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1436615,-95.934494
7600KS17701400KS177014Shellabarger3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1411324,-95.9353256
7904KS07941704KS079417Shellabarger3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.95681,-97.5351639
7940A182276KS077001Shellabarger7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3352778,-98.185
7988KS15500988KS155009Shellabarger1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8038902,-97.9366684
7991P078591KS095001Shellabarger7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6903273,-97.843393
7991KS15500991KS155009Shellabarger2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8854446,-97.9710007
7997P009496KS155411Shellabarger7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8011944,-98.0684167
7997P009596KS155412Shellabarger6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8013611,-98.0695556
7940A1806S1958KS155001SHELLABARGER7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7958336,-97.9372253
80A40A472756OK073009Shellabarger7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.086113,-98.0655594

Water Balance

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

Click the image to view it full size.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with SHELLABARGER, 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-2010-09-03-03 | Reno County - 2002

    Typical pattern of soils and parent material in the Shellabarger-Albion-Nalim association (Soil Survey of Reno County, Kansas; 2002).

  2. KS-2012-01-20-36 | Comanche County - June 1989

    Typical pattern of soils and parent material in the Albion-Shellabarger association (Soil Survey of Comanche County, Kansas; 1989).

  3. KS-2012-01-25-15 | Pratt County - September 1968

    Major soils of associations 8 and 9 and the positions they normally occupy on the landscape (Soil Survey of Pratt County, Kansas; 1968).

  4. KS-2012-01-25-36 | Shawnee County - June 1970

    Loess-till area in the northern part of Shawnee County showing the relation of soils to the landscape in soil association 3 (Soil Survey of Shawnee County, Kansas; 1970).

  5. OK-2012-02-16-04 | Blaine County - February 1968

    Typical pattern of soils in associations 1, 3, 4, and 6 (Soil Survey of Blaine County, Oklahoma; February 1968).

  6. OK-2012-02-16-31 | Garfield County - October 1967

    Typical pattern of soils in the Pratt-Carwile-Shellabarger soil association (Soil Survey of Garfield County, Oklahoma; October 1967).

  7. OK-2012-02-17-11 | Major County - October 1968

    Soil associations in the eastern part of the county (Soil Survey of Major County, Oklahoma; October 1968).

  8. OK-2012-02-17-13 | Major County - October 1968

    Cross section along a line extending across the middle of the county from the western to the eastern boundary (Soil Survey of Major County, Oklahoma; October 1968).

Map Units

Map units containing SHELLABARGER 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
Albion and Shellabarger sandy loams, 6 to 15 percent slopes585010278513824481hdk3ks00719731:24000
Albion-Shellabarger sandy loams, 3 to 15 percent slopes58592275313824541hdk9ks00719731:24000
Shellabarger sandy loam, 3 to 6 percent slopes59571238313825231hdmjks00719731:24000
Shellabarger sandy loam, 3 to 6 percent slopes, eroded5958389413825242tt5sks00719731:24000
Nalim and Shellabarger fine sandy loams, 0 to 1 percent slopes5981282024787882tt4jks00719731:24000
Albion-Shellabarger sandy loams, 1 to 3 percent slopes5858142313824532tt5mks00719731:24000
Shellabarger sandy loam, 1 to 3 percent slopes5956103413825222tt54ks00719731:24000
Shellabarger fine sandy loam, 0 to 1 percent slopes594810113825202tt58ks00719731:24000
Shellabarger fine sandy loam, 1 to 3 percent slopes59493113825212tt57ks00719731:24000
Albion-Shellabarger sandy loams, 3 to 15 percent slopes58591526813816961hcrvks02519801:24000
Shellabarger loam, 3 to 6 percent slopes5952250513817441hctdks02519801:24000
Shellabarger sandy loam, 1 to 3 percent slopes59562313817451hctfks02519801:24000
Albion-Shellabarger sandy loams, 3 to 15 percent slopes58594953513812371hc91ks03319871:24000
Shellabarger sandy loam, 1 to 3 percent slopes59561728113812901hcbrks03319871:24000
Shellabarger sandy loam, 3 to 6 percent slopes5957701413812911hcbsks03319871:24000
Shellabarger sandy loam, 0 to 1 percent slopes5955360413812891hcbqks03319871:24000
Shellabarger loam, 3 to 6 percent slopes5952513812881hcbpks03319871:24000
Shellabarger fine sandy loam, 1 to 3 percent slopes59493044713827362tt57ks07719651:24000
Shellabarger fine sandy loam, 3 to 6 percent slopes59501008113827372tt59ks07719651:24000
Shellabarger and Albion soils, 7 to 15 percent slopes5946628613827342tt5nks07719651:24000
Shellabarger fine sandy loam, 3 to 6 percent slopes, eroded5951425013827382tt5bks07719651:24000
Shellabarger fine sandy loam, 0 to 1 percent slopes5948332013827352tt58ks07719651:24000
Albion and Shellabarger sandy loams, 6 to 15 percent slopes5850316513826651hds3ks07719651:24000
Shellabarger sandy loam, 1 to 3 percent slopes595689013827412tt54ks07719651:24000
Shellabarger loamy fine sand, 0 to 3 percent slopes595330513827392tt5qks07719651:24000
Shellabarger sandy loam, 3 to 6 percent slopes595716513827421hdvlks07719651:24000
Shellabarger loamy sand, 0 to 3 percent slopes595416113827402tt5rks07719651:24000
Shellabarger sandy loam, 3 to 6 percent slopes, eroded59585313827432tt5sks07719651:24000
Nalim-Shellabarger sandy loams, 0 to 1 percent slopes5896367714736722tt4gks07919701:24000
Shellabarger sandy loam, 1 to 3 percent slopes59568932914448122tt54ks09519771:24000
Shellabarger-Nalim complex, 1 to 3 percent slopes59602721714448162tt5vks09519771:24000
Shellabarger sandy loam, 3 to 6 percent slopes59572009914448131khfwks09519771:24000
Shellabarger sandy loam, 3 to 6 percent slopes, eroded5958744514448142tt5sks09519771:24000
Shellabarger loamy sand, 0 to 3 percent slopes5954304214448102tt5rks09519771:24000
Nalim and Shellabarger fine sandy loams, 0 to 1 percent slopes5981167224787892tt4jks09519771:24000
Shellabarger fine sandy loam, 1 to 3 percent slopes5949136014448072tt57ks09519771:24000
Albion and Shellabarger sandy loams, 6 to 15 percent slopes5850107514447671khddks09519771:24000
Albion-Shellabarger sandy loams, 1 to 3 percent slopes585826314447732tt5mks09519771:24000
Shellabarger, eroded, and Albion soils, 6 to 15 percent slopes595919914448152tt5tks09519771:24000
Shellabarger fine sandy loam, 3 to 6 percent slopes595011614448082tt59ks09519771:24000
Shellabarger sandy loam, 0 to 1 percent slopes595510514448112tt55ks09519771:24000
Shellabarger fine sandy loam, 0 to 1 percent slopes59484714448062tt58ks09519771:24000
Shellabarger and Nalim soils, 3 to 6 percent slopes59473614448052tt5pks09519771:24000
Shellabarger fine sandy loam, 3 to 6 percent slopes, eroded59512514448092tt5bks09519771:24000
Albion-Shellabarger sandy loams, 3 to 15 percent slopes58591089013804851hbhsks09719831:24000
Shellabarger loam, 3 to 6 percent slopes5952350413805441hbkpks09719831:24000
Albion and Shellabarger sandy loams, 6 to 15 percent slopes585091914549221ktyzks09719831:24000
Shellabarger sandy loam, 3 to 6 percent slopes595712313805461hbkrks09719831:24000
Shellabarger fine sandy loam, 1 to 3 percent slopes5949813805432tt57ks09719831:24000
Shellabarger sandy loam, 1 to 3 percent slopes5956713805451hbkqks09719831:24000
Albion and Shellabarger sandy loams, 6 to 15 percent slopes58502989214451231khrwks15119651:24000
Shellabarger fine sandy loam, 1 to 3 percent slopes59491133714451662tt57ks15119651:24000
Shellabarger sandy loam, 1 to 3 percent slopes5956209814451692tt54ks15119651:24000
Shellabarger fine sandy loam, 3 to 6 percent slopes, eroded5951199514451672tt5bks15119651:24000
Shellabarger fine sandy loam, 0 to 1 percent slopes594862014451652tt58ks15119651:24000
Shellabarger sandy loam, 0 to 1 percent slopes59557114451682tt55ks15119651:24000
Shellabarger sandy loam, 3 to 6 percent slopes59572614451701khtdks15119651:24000
Shellabarger sandy loam, 1 to 3 percent slopes59566163014438512tt54ks15519991:24000
Shellabarger-Nalim complex, 1 to 3 percent slopes59603563114438532tt5vks15519991:24000
Albion-Shellabarger sandy loams, 1 to 3 percent slopes58582378914438202tt5mks15519991:24000
Shellabarger sandy loam, 0 to 1 percent slopes59551140614438502tt55ks15519991:24000
Shellabarger, eroded, and Albion soils, 6 to 15 percent slopes5959509814438522tt5tks15519991:24000
Shellabarger loamy sand, 0 to 3 percent slopes5954267414438492tt5rks15519991:24000
Shellabarger and Nalim soils, 3 to 6 percent slopes5947160514438482tt5pks15519991:24000
Shellabarger sandy loam, 1 to 3 percent slopes59561966714439862tt54ks17319761:24000
Nalim-Shellabarger sandy loams, 0 to 1 percent slopes58961221414439782tt4gks17319761:24000
Shellabarger-Nalim complex, 1 to 3 percent slopes59601144514439892tt5vks17319761:24000
Shellabarger sandy loam, 3 to 6 percent slopes5957283614439871kgl7ks17319761:24000
Albion-Shellabarger sandy loams, 1 to 3 percent slopes5858219514439692tt5mks17319761:24000
Albion and Shellabarger sandy loams, 6 to 15 percent slopes585076014439671kgklks17319761:24000
Shellabarger sandy loam, 3 to 6 percent slopes, eroded595871214439882tt5sks17319761:24000
Shellabarger-Nalim complex, 1 to 3 percent slopes5960700724787702tt5vks18519751:24000
Nalim and Shellabarger fine sandy loams, 0 to 1 percent slopes5981330016774222tt4jks18519751:24000
Albion-Shellabarger sandy loams, 1 to 3 percent slopes58585114436452tt5mks18519751:24000
Shellabarger sandy loam, 1 to 3 percent slopes59562246214446212tt54ks19119741:24000
Shellabarger sandy loam, 3 to 6 percent slopes5957315114446221kh7qks19119741:24000
Shellabarger sandy loam, 3 to 6 percent slopes, eroded5958118514446232tt5sks19119741:24000
Shellabarger and Albion soils, 7 to 15 percent slopes5946514446202tt5nks19119741:24000

Map of Series Extent

Approximate geographic distribution of the SHELLABARGER 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 .