Official Series Description


Lab Data Summary

Aggregate lab data for the CLAIBORNE soil series. This aggregation is based on all pedons with a current taxon name of CLAIBORNE, 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 CLAIBORNE 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
115BM88105091988MO105009Claiborne3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM88105111988MO105011Claiborne3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM90105151990MO105015Claiborne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM90105251990MO105025Claiborne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
116A81P06801981MO145006Claiborne5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7666664,-94.5
116AM92209121992MO209135Claiborne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8486111,-93.4436111
116AM96179301996MO179030MClaiborne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5374972,-91.2987528
116AM96179351996MO179035MClaiborne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4775972,-90.9444
116AM96179371996MO179037MClaiborne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4836167,-90.9735611
116AM98223461998MO223139Claiborne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0670052,-90.1330948
116AM98223471998MO223145Claiborne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0505486,-90.1807556
116AM00179142000MO179014MClaiborne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.317125,-91.0497194
116AM00179172000MO179017MClaiborne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3151722,-91.0504
116AM00179332000MO179033MClaiborne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3153472,-91.0413694
116AM06035072006MO035007Claiborne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9652778,-91.0530556
116BM86085011986MO085001Claiborne3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2037917,-93.4213056
116BM90105031990MO105003Claiborne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2037904,-93.4213064
116BM92209421992MO209179Claiborne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8912639,-93.5416194

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CLAIBORNE 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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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 CLAIBORNE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the CLAIBORNE series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the CLAIBORNE 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

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.

Competing Series

Soil series competing with CLAIBORNE 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 CLAIBORNE 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 CLAIBORNE 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.

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 CLAIBORNE, 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-2010-11-05-34 | Scott County - 2006

    Diagram of a sequence of landform positions in areas underlain with limestone in Scott 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 Scott County, Virginia; 2006).

Map Units

Map units containing CLAIBORNE 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
Claiborne silt loam, 25 to 45 percent slopesCaE3292524247klj6tn01319931:24000
Claiborne silt loam, 12 to 25 percent slopesCaD1837524246klj5tn01319931:24000
Claiborne silt loam, 5 to 12 percent slopesCaC452524245klj4tn01319931:24000
Claiborne silt loam, steep phaseCnz8649524491kls2tn02519481:24000
Claiborne silt loamCn6964524489kls0tn02519481:24000
Claiborne silt loam, rolling phaseCno2872524490kls1tn02519481:24000
Claiborne silt loam, hilly phaseCnl2433529952ksg7tn17319451:24000
Claiborne silt loam, steep phaseCnz2106529954ksg9tn17319451:24000
Claiborne silt loam, rolling phaseCno1160529953ksg8tn17319451:24000
Claiborne silt loam, 25 to 40 percent slopesCeE8820528531kqzdtn60219731:15840
Claiborne silt loam, 12 to 25 percent slopesCeD3676528530kqzctn60219731:15840
Claiborne silt loam, 5 to 12 percent slopesCeC1457528529kqzbtn60219731:15840
Claiborne soils, 15 to 35 percent slopes, severely erodedCfE3249528532kqzftn60219731:15840
Claiborne silt loam, 35 to 65 percent slopes, eroded14F7720778041v3m3va16920031:24000
Claiborne silt loam, 15 to 25 percent slopes, eroded14D3417778039v3m1va16920031:24000
Claiborne silt loam, 25 to 35 percent slopes, eroded14E3130778040v3m2va16920031:24000
Claiborne silt loam, 8 to 15 percent slopes, eroded14C1118778038v3m0va16920031:24000

Map of Series Extent

Approximate geographic distribution of the CLAIBORNE 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 .