Official Series Description


Lab Data Summary

Aggregate lab data for the BEWLEYVILLE soil series. This aggregation is based on all pedons with a current taxon name of BEWLEYVILLE, 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 BEWLEYVILLE 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
122S75AL-083-175AL083001-pgmBewleyville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.7672271728516,-87.0827865600586

Water Balance

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

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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 BEWLEYVILLE, 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-2012-01-26-06 | 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).

  3. KY-2012-02-01-52 | Simpson County - May 1985

    Relationship of soils to topography and underlying material in the Pembroke-Bewleyville general soil map unit (Soil Survey of Simpson County, Kentucky; May 1985).

  4. KY-2012-02-01-69 | Wayne County - March 1990

    The relationship of soils to topography and underlying material in the Decatur-Bewleyville-Clarksville general soil map unit (Soil Survey of Wayne County, Kentucky; March 1990).

Map Units

Map units containing BEWLEYVILLE 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
Bewleyville silt loam, 2 to 6 percent slopesBeB6716328683c10pal03319861:20000
Bewleyville silt loam, 6 to 10 percent slopesBeC2548328684c10qal03319861:20000
Bewleyville silt loam, 6 to 12 percent slopesBvC8540549892lg6gky17119771:20000
Bewleyville silt loam, 2 to 6 percent slopesBvB6765549891lg6fky17119771:20000
Bewleyville silt loam, 2 to 6 percent slopesBeB1260549793lg38ky21319821:20000
Bewleyville silt loam, 6 to 12 percent slopesBeC425549794lg39ky21319821:20000
Bewleyville silt loam, 2 to 6 percent slopesBwB2551550060lgcwky23119851:20000
Bewleyville silt loam, 5 to 12 percent slopes, erodedBeC21059524405klp9tn01519991:24000
Bewleyville silt loam, 12 to 20 percent slopes, erodedBeD2143524406klpbtn01519991:24000
Bewleyville silt loam, 5 to 12 percent slopes, erodedBeC22609636846pcpftn02720021:24000
Bewleyville silt loam, 2 to 5 percent slopes, erodedBeB2707531070ktm9tn02720021:24000
Bewleyville silt loam, 5 to 12 percent slopes, erodedBeC2543530178kspjtn08719991:24000
Bewleyville silt loam, 2 to 5 percent slopes, erodedBeB2283530177ksphtn08719991:24000
Bewleyville silt loam, 2 to 5 percent slopes, erodedBtB258095276262zpqltn09919551:20000
Bewleyville silty clay loam, 5 to 12 percent slopes, severely erodedBtC318005276292zpqptn09919551:20000
Bewleyville silt loam, 5 to 12 percent slopes, erodedBtC216295276282zpqmtn09919551:20000
Bewleyville silt loam, 2 to 5 percent slopesBtB8265276252zpqktn09919551:20000
Bewleyville silt loam, 5 to 12 percent slopesBtC4125276272zpqntn09919551:20000
Bewleyville silt loam, 2 to 5 percent slopesBwB4294525819kn4xtn10319991:24000
Bewleyville silt loam, 5 to 12 percent slopesBwC1070525820kn4ytn10319991:24000
Bewleyville silt loam, 2 to 5 percent slopes, erodedBeB23029527693kq3ctn11119921:24000
Bewleyville silt loam, 5 to 12 percent slopes, erodedBeC21217527694kq3dtn11119921:24000
Bewleyville silt loam, 5 to 12 percent slopes, erodedBeC21481843360x9l5tn13320031:24000
Bewleyville silt loam, 2 to 5 percent slopes, erodedBeB2328843359x9l4tn13320031:24000
Bewleyville silt loam, 2 to 5 percent slopes, erodedCc59523968942lg55tn16119531:20000
Bewleyville silt loam, 5 to 12 percent slopes, erodedCb49423968932lg54tn16119531:20000
Bewleyville silty clay loam, 2 to 5 percent slopes, erodedBeB211492528345kqsdtn16519931:20000
Bewleyville silty clay loam, 5 to 12 percent slopes, erodedBeC24244528346kqsftn16519931:20000
Bewleyville silt loam, 2 to 5 percent slopes, erodedBeB2796528445kqwmtn18919881:20000
Bewleyville silt loam, 5 to 12 percent slopes, erodedBeC2702528446kqwntn18919881:20000
Bewleyville silt loam, 2 to 5 percent slopesBeB4382528629kr2ktn60419741:20000
Bewleyville silt loam, 5 to 12 percent slopesBeC3519528630kr2ltn60419741:20000
Bewleyville silt loam, 5 to 12 percent slopes, erodedBeC2689824274022mgx9tn61019601:15840
Bewleyville silt loam, 2 to 5 percent slopesBeB321624274002mgx7tn61019601:15840
Bewleyville silty clay loam, 5 to 12 percent slopes, severely erodedBmC3166624274042mgxctn61019601:15840
Bewleyville silt loam, 5 to 12 percent slopesBeC74324274012mgx8tn61019601:15840
Bewleyville silt loam, 12 to 20 percent slopes, erodedBeD254224274032mgxbtn61019601:15840
Bewleyville silty clay loam, 12 to 20 percent slopes, severely erodedBmD335824274052mgxdtn61019601:15840
Bewleyville-Dickson complex, 2 to 6 percent slopesBeB310024391662mw4stn70119851:24000

Map of Series Extent

Approximate geographic distribution of the BEWLEYVILLE 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 .