Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
12774PA0310011974PA031001Sewell3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2336111,-79.3816667

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the SEWELL series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the SEWELL series and siblings. 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 SEWELL 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with SEWELL share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the SEWELL 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 SEWELL 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.

Click the image to view it full size.

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 SEWELL, 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. VA-2010-11-05-07 | Buchanan County -

    Illustration of an area that has been surface mined for coal, showing a sequence of native residual and colluvial soils, mine soils, rock outcrop, and multiple exposed highwalls. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Buchanan County, Virginia).

  2. VA-2010-11-05-16 | Dickenson County - 2009

    Illustration of an area that has been surface mined for coal, showing a sequence of native residual and colluvial soils, mine soils, rock outcrop, and multiple exposed highwalls. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Dickenson County, Virginia; 2009).

  3. VA-2010-11-05-17 | Dickenson County - 2009

    Illustration of an area that has been surface mined for coal, showing a sequence of native residual and colluvial soils, mine soils, rock outcrop, and a single exposed highwall. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Dickenson County, Virginia; 2009).

  4. VA-2010-11-05-26 | Lee County - 2006

    Typical pattern of soils in the Appalachian Plateau portion of Lee County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to parent material and landform position (Soil Survey of Lee County, Virginia; 2006).

  5. VA-2010-11-05-31 | Russell County - 2007

    Diagram of a sequence of landform positions in the Appalachian Plateau area of Russell County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Russell County, Virginia; 2007).

  6. VA-2012-05-10-04 | Buchanan County - 2009

    An illustration of an area that has been surface-mined for coal that shows a sequence of native residual and colluvial soils, mine soils, rock outcrop, and multiple exposed highwalls. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Buchanan County, Virginia; 2009).

  7. VA-2012-05-10-05 | Buchanan County - 2009

    An illustration of an area that has been surface-mined for coal that shows a sequence of native residual and colluvial soils, mine soils, rock outcrop, and a single exposed highwall. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Buchanan County, Virginia; 2009).

  8. VA-2012-05-11-02 | Dickenson County - 2009

    Illustration of an area that has been surface mined for coal, showing a sequence of native residual and colluvial soils, mine soils, rock outcrop, and multiple exposed highwalls. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Dickenson County, Virginia; 2009).

  9. VA-2012-05-11-03 | Dickenson County - 2009

    Illustration of an area that has been surface mined for coal, showing a sequence of native residual and colluvial soils, mine soils, rock outcrop, and a single exposed highwall. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Dickenson County, Virginia; 2009).

  10. VA-2012-05-11-07 | Lee County - 2006

    Typical pattern of soils in the Appalachian Plateau portion of Lee County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to parent material and landform position (Soil Survey of Lee County, Virginia; 2006).

  11. VA-2012-05-11-11 | Russell County - 2007

    Diagram of a sequence of landform positions in the Appalachian Plateau area of Russell County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Russell County, Virginia; 2007).

Map Units

Map units containing SEWELL 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
Cedarcreek-Sewell-Rock outcrop complex, 0 to 30 percent slopes, very stonyuCsrE11031584502ykstky19519861:24000
Sewell channery fine sandy loam, 20 to 40 percent slopesSbE690536425l061oh16319981:15840
Sewell very channery sandy loam, 0 to 8 percent slopesSeB1096633067p7rjpa03120121:24000
Sewell very channery sandy loam, 15 to 25 percent slopesSeD536339329930syppa03120121:24000
Sewell very channery sandy loam, 8 to 15 percent slopesSeC479339330030synpa03120121:24000
Cedarcreek-Sewell-Rock outcrop complex, 0 to 15 percent slopes, very stony4C923116709081t2q8va02720061:24000
Sewell-Kaymine-Rock outcrop complex, 0 to 80 percent slopes, extremely stony21F708216709041t2q4va02720061:24000
Fiveblock-Sewell complex, 0 to 15 percent slopes, extremely stony8C169216708961t2pwva02720061:24000
Cedarcreek-Sewell-Rock outcrop complex, 0 to 15 percent slopes, very stony2C342523998532lk7mva05120081:24000
Kaymine-Sewell-Rock outcrop complex, 0 to 80 percent slopes, extremely stony17F304923998742lk89va05120081:24000
Sewell channery sandy loam, 35 to 55 percent slopes, extremely stony22E22023998822lk8kva05120081:24000
Sewell channery sandy loam, 55 to 80 percent slopes, extremely stony22F6523998832lk8lva05120081:24000
Bethesda, Fairpoint, and Sewell soils, 0 to 80 percent slopes, very rocky6E5732521693khvtva10519971:24000
Cedarcreek-Sewell-Rock outcrop complex, 0 to 15 percent slopes, very stony16C226916719051t3rfva16720061:24000
Sewell-Kaymine-Rock outcrop complex, 0 to 80 percent slopes, extremely stony47F81016719041t3rdva16720061:24000
Cedarcreek-Sewell-Rock outcrop complex, 0 to 15 percent slopes, very stony15C208525074852q7pgva19520101:24000
Kaymine-Sewell-Rock outcrop complex, 0 to 80 percent slopes, extremely stony44G195725085702q7qlva19520101:24000
Sewell very channery sandy loam, very steep, extremely stonySwF1485514869k8rpwv00519881:24000
Sewell-Rock outcrop complex, very steep, extremely stonySrF330532235kvtwwv04719931:24000
Sewell extremely channery sandy loam, 3 to 15 percent slopes, very stonySeB260532234kvtvwv04719931:24000
Sewell channery sandy loam, strongly slopingSeC1140513507k7brwv10919841:24000
Sewell channery sandy loam, 8 to 25 percent slopes, reclaimedSlD42329001782rgttwv61119771:20000
Sewell very channery sandy loam, 25 to 70 percent slopes, unreclaimed, highwallShF22029001592rgtnwv61119771:20000
Sewell very channery sandy loam, 8 to 25 percent slopes, unreclaimed, highwallShD17229001582rgtmwv61119771:20000
Sewell channery sandy loam, 8 to 25 percent slopes, reclaimed, highwallSrD10329001702rgtqwv61119771:20000
Sewell channery sandy loam, 25 to 70 percent slopes, reclaimedSlF8829001792rgtvwv61119771:20000
Sewell channery sandy loam, 0 to 8 percent slopes, reclaimedSlB7529001772rgtswv61119771:20000
Sewell very channery sandy loam, 25 to 70 percent slopes, unreclaimedSwF6129001502rgtlwv61119771:20000
Sewell channery sandy loam, 25 to 70 percent slopes, reclaimed, highwallSrF3329001712rgtrwv61119771:20000
Sewell very channery sandy loam, 8 to 25 percent slopes, unreclaimedSwD2729001492rgtkwv61119771:20000
Sewell channery sandy loam, 0 to 8 percent slopes, reclaimed, highwallSrB529001692rgtpwv61119771:20000
Sewell very channery sandy loam, 0 to 8 percent slopes, unreclaimed, highwallShB529001572rgtjwv61119771:20000

Map of Series Extent

Approximate geographic distribution of the SEWELL 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 .