Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

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

Click the image to view it full size.

Soil series sharing subgroup-level classification with WHITWELL, 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. KY-2012-01-26-02 | Adair County - April 1964

    Diagram of the Baxter-Christian-Bewleyville association (Soil Survey of Adair County (Soil Survey of Adair County, Kentucky; April 1964).

  2. KY-2012-01-26-05 | Adair County - April 1964

    Diagram of the Staser-Taft-Landisburg association on flood plains, terraces, and foot slopes (Soil Survey of Adair County (Soil Survey of Adair County, Kentucky; April 1964).

  3. KY-2012-01-26-06 | Adair County - April 1964

    Geological cross section of Adair County showing the relationship of the soils to the underlying rocks (Soil Survey of Adair County (Soil Survey of Adair County, Kentucky; April 1964).

  4. KY-2012-01-27-58 | Elliott County - 1965

    Diagram of Muskingum-Montevallo-Ramsey association, showing relationship of soil series to topography and parent material (Soil Survey of Elliott County, Kentucky; 1965).

  5. TN-2010-11-02-05 | Cumberland County - 2006

    The pattern of soils and parent material in Grassy Cove. The Waynesboro-Whitwell general soil map unit is in the center of the cove (Soil Survey of Cumberland County, Tennessee; 2006).

Map Units

Map units containing WHITWELL 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
Spadra-Whitwell complex, 0 to 3 percent slopes, occasionally floodedSpB17150331558c40fal12719861:24000
Whitwell-Swafford complex, 2 to 6 percent slopesWcB274413957531hvd9al13320121:24000
Whitwell silt loam, 1 to 5 percent slopes, rarely floodedWtB250216119341r3bwga01520131:12000
Whitwell loam, 1 to 3 percent slopes, occasionally floodedWhA675531219kts3ga04719871:20000
Shady-Whitwell complex, 2 to 6 percent slopes, rarely floodedSeB2985202379325xxnga12920071:12000
Whitwell-Conasauga complex, 2 to 6 percent slopes, rarely floodedWxB1280202383525xz0ga12920071:12000
Whitwell silt loam, 0 to 2 percent slopes, occasionally floodedWtA740202383425xyzga12920071:12000
Whitwell silt loamWh11270531313ktw4ga62119751:20000
Whitwell silt loam, 0 to 2 percent slopes, occasionally floodedWtA3825562909lwrcga64820011:12000
Whitwell silt loam, 2 to 6 percent slopesWtB1830562910lwrdga64820011:12000
Whitwell-Urban land complex, 0 to 2 percent slopes, occasionally floodedWuA255562937lws8ga64820011:12000
Whitwell loam, 1 to 4 percent slopes, occasionally floodedWw399188736021byltn00119781:15840
Whitwell silt loam, occasionally floodedWh1604526697kp27tn00719871:24000
Whitwell loam, 0 to 3 percent slopesWd2615269962wplltn01119511:20000
Whitwell loam, occasionally floodedWh1126524283klkctn01319931:24000
Whitwell loam, gently sloping phaseWn723525008km9rtn03119561:20000
Whitwell loam, level phaseWm711525007km9qtn03119561:20000
Whitwell loam, eroded, gently sloping phaseWo173525009km9stn03119561:20000
Whitwell loam, 2 to 5 percent slopesWhB1665523908kl58tn03519981:24000
Whitwell loam, 0 to 2 percent slopes, occasionally floodedWhA3135239072wpljtn03519981:24000
Whitwell loamWg4937527271kpnrtn05119501:20000
Whitwell loam, rarely floodedWh836525274kmlbtn06119901:24000
Whitwell loam, 0 to 3 percent slopes, occasionally floodedWh358010178962wplktn06519801:15840
Shady-Whitwell complex, 0 to 3 percent slopes, rarely floodedSo1942632844p7jbtn09320051:12000
Whitwell loam, 2 to 5 percent slopes, rarely floodedWwB572632852p7jltn09320051:12000
Whitwell loam, 0 to 2 percent slopes, rarely floodedWm18215263282wplhtn11519511:20000
Whitwell loam, 0 to 2 percent slopes, rarely floodedWt4635279612wplhtn12319741:20000
Whitwell loam, 0 to 3 percent slopes, occasionally floodedWt727523792kl1jtn13919971:24000
Whitwell loam, 1 to 4 percent slopes, occasionally floodedWhB60151475620301gztn14520051:24000
Whitwell loam, 0 to 2 percent slopes, rarely floodedWh12115296492wplhtn15319951:24000
Whitwell loamWw1488529938ksfstn17719651:15840
Whitwell loam, 0 to 2 percent slopes, occasionally floodedWt12425286212wpljtn60219731:15840
Whitwell loam, occasionally floodedWt163524849km4mtn60620011:24000
Whitwell loam, 0 to 2 percent slopes, rarely floodedWe38918995802wplhtn60919551:20000

Map of Series Extent

Approximate geographic distribution of the WHITWELL 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 .