Official Series Description


Lab Data Summary

Aggregate lab data for the CULLOWHEE soil series. This aggregation is based on all pedons with a current taxon name of CULLOWHEE, 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 CULLOWHEE 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
130B86P093686NC099003Cullowhee7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.288887,-83.1800003

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CULLOWHEE 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 CULLOWHEE 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 CULLOWHEE 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 CULLOWHEE 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 CULLOWHEE 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 CULLOWHEE series and competing. 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 CULLOWHEE 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.

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.

Soil series sharing subgroup-level classification with CULLOWHEE, 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. NC-2012-02-07-22 | Jackson County - June 1997

    Relationship of soils and landscape position in the Braddock-Nikwasi-Dellwood-Cullowhee general soil map unit (Soil Survey of Jackson County, North Carolina; June 1997).

Map Units

Map units containing CULLOWHEE 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
Cullowhee loam, 0 to 3 percent slopes, frequently floodedCuA793548061ld9dnc01119971:12000
Cullowhee fine sandy loam, 0 to 3 percent slopes, occasionally floodedCwA301724231092mbftnc03920091:12000
Cullowhee-Ela complex, 0 to 3 percent slopes, occasionally floodedCwA14171912743226cdnc07520071:12000
Cullowhee fine sandy loam, 0 to 2 percent slopes, occasionally floodedCwA1010547058lc81nc09919911:12000
Cullowhee-Ela complex, 0 to 3 percent slopes, occasionally floodedTo94323904032l7dsnc17519681:12000
Cullowhee loam, 0 to 3 percent slopes, frequently floodedCuA503529797ks97nc18920011:12000
Tate-Cullowhee, frequently flooded complex, 0 to 25 percent slopesTcC818523961262lfcdnc19319931:24000
Cullowhee fine sandy loam, 0 to 3 percent slopes, frequently floodedCwA122913834301hfksnc19319931:24000
Cullowhee-Ela complex, 0 to 3 percent slopes, occasionally floodedCwA634556267lnv3nc60520071:12000
Cullowhee-Nikwasi complex, 0 to 2 percent slopes, frequently floodedCxA3194546757lbybnc60619911:12000
Cullowhee-Ela complex, 0 to 2 percent slopes, frequently floodedCw145553591ll1stn64020071:24000

Map of Series Extent

Approximate geographic distribution of the CULLOWHEE 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 .