Official Series Description


Lab Data Summary

Aggregate lab data for the WENTWORTH soil series. This aggregation is based on all pedons with a current taxon name of WENTWORTH, 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 WENTWORTH 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
102B40A2476S1961SD079002WENTWORTH6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0424995,-96.9472198
102B05N0472S2004SD099001Wentworth7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6147766,-97.1281357

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WENTWORTH 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 WENTWORTH 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 WENTWORTH 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 WENTWORTH 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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Competing Series

Soil series competing with WENTWORTH 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 WENTWORTH 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 WENTWORTH 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 .

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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.

Soil series sharing subgroup-level classification with WENTWORTH, 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. SD-2010-11-01-10 | Minnehaha County - 2004

    Typical pattern of soils and parent material in the Egan-Ethan-Trent association (Soil Survey of Minnehaha County, South Dakota; 2004).

  2. SD-2012-03-15-68 | Lake County - December 1973

    Relationship of soils to topography and the underlying materials in the Egan-Wentworth association (Soil Survey of Lake County, SD; 1973).

  3. SD-2012-03-15-83 | Moody County - April 1989

    Pattern of soils and parent material in the Egan-Baltic association (Soil Survey of Moody County, SD; 1989).

Map Units

Map units containing WENTWORTH 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
Wentworth silty clay loam, 0 to 2 percent slopes71010154091332vwc6ia11919731:15840
Wentworth silty clay loam, 2 to 6 percent slopes710B6724091342vwc8ia11919731:15840
Wentworth silty clay loam, 5 to 9 percent slopes, moderately eroded710C2666409135fqqxia11919731:15840
Egan-Wentworth-Trent complex, 2 to 6 percent slopesEeB1984187482vwcfsd01119951:24000
Wentworth-Trent complex, 0 to 2 percent slopesWeA1274188232vwc9sd01119951:24000
Wakonda-Wentworth-Whitewood complex, 0 to 2 percent slopesWc7333445622gypxsd02719951:24000
Wentworth-Trent complex, 0 to 2 percent slopesTwA34844456182vwc9sd02719951:24000
Wentworth-Trent complex, 2 to 6 percent slopesWkB5774456242vwcbsd02719951:24000
Egan-Wentworth complex, 2 to 6 percent slopesEhB668854164932vwcdsd07919671:20000
Egan-Wentworth complex, 0 to 2 percent slopesWeA36754165212vwccsd07919671:20000
Wentworth-Chancellor silty clay loams, 0 to 2 percent slopesWhA105640416664fzkssd08319711:20000
Wentworth silty clay loam, 0 to 2 percent slopesWeA222414166632vwc6sd08319711:20000
Wentworth silty clay loam, 2 to 6 percent slopesWbB63384180402vwc8sd08719761:20000
Wentworth-Ethan complex, 2 to 5 percent slopesWcB4812418041g106sd08719761:20000
Wentworth silty clay loam, 0 to 2 percent slopesWaA26454180392vwc6sd08719761:20000
Wentworth-Trent-Tetonka complex, 0 to 3 percent slopesWdA1423418042g107sd08719761:20000
Egan-Wentworth-Trent complex, 2 to 6 percent slopesEgB206004460352vwcfsd09919951:24000
Wentworth-Chancellor-Wakonda silty clay loams, 0 to 2 percent slopesWcA4874446086gz5wsd09919951:24000
Wentworth-Trent complex, 2 to 6 percent slopesWhB35604460882vwcbsd09919951:24000
Wentworth-Trent complex, 0 to 2 percent slopesWhA31744460872vwc9sd09919951:24000
Egan-Wentworth complex, 2 to 6 percent slopesWeB293844183572vwcdsd10119851:20000
Wentworth-Chancellor-Wakonda silty clay loams, 0 to 2 percent slopesWcA12094418356g1bcsd10119851:20000
Wentworth-Trent complex, 0 to 2 percent slopesWhA36154183582vwc9sd10119851:20000
Wentworth-Chancellor-Wakonda silty clay loams, 0 to 2 percent slopesWcA29581418244g16rsd12519801:20000
Egan-Wentworth complex, 2 to 6 percent slopesEgB282984182302vwcdsd12519801:20000
Wakonda-Wentworth-Chancellor silty clay loams, 0 to 3 percent slopesWaA1545418243g16qsd12519801:20000
Wentworth silty clay loam, 0 to 2 percent slopesWbA85694537262vwc6sd12719741:20000
Wentworth-Worthing silty clay loamsWc4276453728h74dsd12719741:20000
Wentworth silty clay loam, 2 to 6 percent slopesWbB42104537272vwc8sd12719741:20000
Egan-Wentworth complex, 2 to 6 percent slopesEcB37244180762vwcdsd13519771:20000
Wentworth silty clay loam, 0 to 2 percent slopesWbA28124181112vwc6sd13519771:20000
Wentworth-Trent complex, 2 to 6 percent slopesWcB25924181122vwcbsd13519771:20000
Egan-Wentworth complex, 0 to 2 percent slopesEcA11604180752vwccsd13519771:20000
Egan-Wentworth complex, 2 to 6 percent slopesEgB40054179632vwcdsd60219751:20000

Map of Series Extent

Approximate geographic distribution of the WENTWORTH 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 .