Official Series Description


Lab Data Summary

Aggregate lab data for the KANAWHA soil series. This aggregation is based on all pedons with a current taxon name of KANAWHA, 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 KANAWHA 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.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
12778P0177S1978WV089009Kanawha5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6458321,-80.7624969
12778P0178S1978WV089010Kanawha5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6124992,-80.7861099

Water Balance

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

Soil series competing with KANAWHA 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 KANAWHA 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 KANAWHA 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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Soil series sharing subgroup-level classification with KANAWHA, 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. WV-2010-11-08-03 | Doddridge County - 2005

    Chagrin soil along Middle Island Creek. Also shown is the typical pattern of other soils and their underlying parent material in parts of Doddridge County (Soil Survey of Doddridge County, West Virginia; 2005).

  2. WV-2010-11-08-10 | Lincoln County - 2007

    Typical pattern of soils and parent material in an area of the Highsplint-Matewan-Cloverlick general soil map unit (Soil Survey of Lincoln County, West Virginia; 2007).

Map Units

Map units containing KANAWHA 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
Kanawha loam, 2 to 6 percent slopesKaB2217104831vdwwoh01319781:15840
Kanawha silt loam, 1 to 8 percent slopesKaB1309536813l0lkoh05319881:15840
Kanawha silt loam, 2 to 6 percent slopesKbB114603431l0lvoh05319881:15840
Kanawha loam, 2 to 6 percent slopesKaB1551536917l0pxoh05919981:15840
Kanawha silt loam, 2 to 6 percent slopesKaB10200536147kzx2oh08719891:15840
Kanawha silt loam, 6 to 12 percent slopesKaC2283536148kzx3oh08719891:15840
Kanawha-Urban land complexKc2820514861k8rfwv00519881:24000
Kanawha loam, 0 to 3 percent slopes, rarely floodedKa8805148602t1lbwv00519881:24000
Kanawha loam, 3 to 8 percent slopes, rarely floodedKnB7405136642t1lcwv01119841:20000
Kanawha loam, 3 to 8 percent slopes, protectedKaB550513662k7hrwv01119841:20000
Kanawha loam, 0 to 3 percent slopes, protectedKaA550513661k7hqwv01119841:20000
Kanawha-Urban land complex, 0 to 8 percent slopesKuB410513665k7hvwv01119841:20000
Kanawha loam, 0 to 3 percent slopes, rarely floodedKnA2605136632t1lbwv01119841:20000
Kanawha loam, 0 to 3 percent slopes, rarely floodedKa6585617352t1lbwv01720011:24000
Kanawha-Urban land complexKu44561736lvjjwv01720011:24000
Kanawha loam, 0 to 3 percent slopes, rarely floodedKa10865149082t1lbwv02119951:24000
Urban land-Kanawha complexUk3732512869k6p5wv03919761:20000
Kanawha fine sandy loam, 0 to 3 percent slopesKaA1934512850k6nkwv03919761:20000
Kanawha fine sandy loam, 3 to 8 percent slopesKaB797512851k6nlwv03919761:20000
Kanawha silt loam, 0 to 3 percent slopes, protectedKaA545553321lks2wv04320051:24000
Kanawha silt loam, 3 to 8 percent slopes, protectedKaB445553322lks3wv04320051:24000
Urban land-Kanawha complex, 0 to 8 percent slopes, protectedUkB369553333lksgwv04320051:24000
Kanawha silt loam, 0 to 3 percent slopes, rarely floodedKaA24817206201vrfwwv05120071:12000
Urban land-Kanawha complex, 0 to 3 percent slopesUsA48186264820j7fwv05120071:12000
Kanawha loam, 3 to 8 percent slopes, rarely floodedKaB9675131722t1lcwv07919811:20000
Urban land-Kanawha complex, 0 to 8 percent slopesUkB605513202k70xwv07919811:20000
Kanawha loam, 0 to 3 percent slopes, rarely floodedKaA4875131712t1lbwv07919811:20000
Urban land-Kanawha-Cotaco complex, 0 to 8 percent slopesUvB1150515038k8y4wv09919931:24000
Kanawha loam, 0 to 3 percent slopes, rarely floodedKaA8905150202t1lbwv09919931:24000
Kanawha loam, 3 to 8 percent slopes, rarely floodedKaB6305150212t1lcwv09919931:24000
Kanawha loam, 0 to 3 percent slopes, rarely floodedKnA11713841472t1lbwv60020051:24000
Kanawha variant gravelly loamKv1301515586k9htwv60319781:20000
Kanawha loamKa1245515585k9hswv60319781:20000
Kanawha loam, 0 to 3 percent slopes, rarely floodedKa12485143912t1lbwv61119771:20000
Urban land-Kanawha complex, 0 to 8 percent slopesUkB665115556617sgbwv62020051:24000
Urban land-Kanawha complex, 0 to 8 percent slopes, protectedUnB420115556717sgcwv62020051:24000
Urban land-Kanawha-Cotaco complex, 0 to 8 percent slopesUtB10115556817sgdwv62020051:24000
Urban land-Kanawha complex, 0 to 3 percent slopes, rarely floodedUwA26524532752nbtxwv70520091:24000
Kanawha fine sandy loamKa20932516590k9ywwv7131:24000

Map of Series Extent

Approximate geographic distribution of the KANAWHA 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 .