Official Series Description


Lab Data Summary

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


Water Balance

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with BUNCOMBE, 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-2010-09-28-06 | Rutherford County - 1997

    Typical relationship of soils, landform position, and parent material in the Chewacla-Toccoa-Buncombe general soil map unit (Soil Survey of Rutherford County, North Carolina; 1997).

  2. NC-2010-09-28-09 | Rutherford County - 1997

    A cross section showing the relationship between flood plain soils and a seasonal high water table (Soil Survey of Rutherford County, North Carolina; 1997).

  3. NC-2012-02-07-30 | Lincoln County - January 1995

    Relationship of soils, parent material, and seasonal high water table in the Chewacla-Riverview general soil map unit (Soil Survey of Lincoln County, North Carolina; January 1995).

  4. NC-2012-02-07-38 | Polk County - 1998

    The relationship between soils, landscape, and parent material in the Pacolet-Madison-Rion general soil map unit. The clayey Pacolet, Madison, and Cecil soils occur on ridgetops. The loamy Rion, Grover, and Ashlar soils are on the adjacent side slopes (Soil Survey of Polk County, North Carolina; 1998).

  5. NC-2012-02-07-39 | Polk County - 1998

    The relationship between soils, landscape, and parent material in the Riverview-Chewacla-Buncombe general soil map unit. The Buncombe soils are in convex areas adjacent to the stream channel; the Chewacla soils are in the lower, concave areas further from the channel; and the Riverview soils occur in the remaining areas of the flood plain. The clayey Masada, Dogue, and Roanoke soils are on the higher stream terraces (Soil Survey of Polk County, North Carolina; 1998).

  6. SC-2012-03-14-17 | Cherokee County - July 1962

    Schematic drawing of a small part of soil association 5 showing the relation of the main soil series in the dominant land types, Mixed alluvial land and Mixed wet alluvial land (Soil Survey of Cherokee County, SC; 1962).

Map Units

Map units containing BUNCOMBE 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
Buncombe loamy sandBa52312269643nyal01719571:20000
Sandy alluvial landSa97329506c1w7al05719631:15840
Buncombe-Bigbee complex, 0 to 5 percent slopes, frequently floodedBuB1069330372c2s5al06920021:24000
Riverview, Chewacla and Buncombe soils, 0 to 3 percent slopes, frequently floodedRCB9031162812z475al10119581:20000
Buncombe loamy sandBu100612282543t3al11119651:15840
Buncombe loamy sand, 0 to 2 percent slopes, frequently floodedBuA17014763971lk9qal12320051:24000
Buncombe loamy sand, 0 to 6 percent slopes, occasionally floodedBwB3801018573135x6ga03520031:24000
Buncombe loamy sand, 0 to 6 percent slopesBfs52512623347c1ga09719601:15840
Buncombe loamy fine sandBa29512430845byga11719571:20000
Buncombe loamy sand, 0 to 3 percent slopes, occasionally floodedBaA78516723441t46lga12120071:12000
Buncombe loamy fine sandBfs370639932pgwzga13519661:15840
Buncombe loamy sandsBfs93012445945htga13719601:20000
Buncombe loamy sandBfs10112457445mjga14719611:20000
Buncombe loamy sand, 0 to 6 percent slopes, occasionally floodedBwB520126940482vga15919971:24000
Buncombe loamy sandBfs35012467445qrga19919601:15840
Buncombe loamy sand, 0 to 6 percent slopes, occasionally floodedBcB85022005232cvtmga20720071:24000
Buncombe loamy sandBfs675125197468mga60419721:20000
Buncombe loamy sand, 0 to 2 percent slopesBmA1295325459bxnpga61519811:20000
Buncombe loamy sandBfs107012542346hxga61819661:15840
Buncombe loamy sandBfs1040531324ktwhga62219671:20000
Buncombe loamy sandBfs52512547146kgga62319651:15840
Buncombe loamy sandBfs96012564646r3ga63219671:15840
Buncombe loamy sandBfs71512575046vgga64219671:15840
Buncombe loamy sand, 0 to 5 percent slopes, frequently floodedBwB67012734248htga64919921:12000
Buncombe loamy sand, 0 to 2 percent slopes, occasionally floodedBuA713747853t369ga65520121:24000
Buncombe loamy sand, 0 to 5 percent slopes, frequently floodedBuB11724312332mlwwnc03519691:15840
Buncombe loamy sand, 1 to 5 percent slopes, rarely floodedBuB9181170553xsznc04520001:24000
Buncombe loamy sand, 0 to 5 percent slopes, frequently floodedBuB74524325572mn8lnc05919881:24000
Riverview and Buncombe soils, 0 to 3 percent slopes, frequently floodedRmA15351126063s5gnc06919971:24000
Buncombe loamy sand, 0 to 5 percent slopes, frequently floodedBuB9224243892mcs3nc09720111:12000
Buncombe sand, 0 to 5 percent slopes, rarely floodedBnB2411136173t72nc10919891:24000
Buncombe loamy sand, 0 to 5 percent slopes, occasionally floodedBuB14201110753ql2nc14919921:24000
Buncombe loamy sand, 0 to 5 percent slopes, occasionally floodedBuB21071176063ycrnc16119971:24000
Buncombe sand, 0 to 4 percent slopesBuB251115498717rvnsc00119761:20000
Buncombe loamy sandBc5111320664ff6sc02119601:20000
Buncombe loamy sand, 2 to 5 percent slopesBwB2751324644fv1sc04519721:20000
Buncombe-Santee associationBS76671325294fx4sc05319751:20000
Buncombe associationBR40661325284fx3sc05319751:20000
Buncombe coarse sand, 0 to 3 percent slopes, rarely flooded3B314592701kzh7sc07120051:24000
Buncombe loamy sandBu3141310164dbbsc07719671:20000
Buncombe sandBu4741314584dslsc08719701:20000
Buncombe loamy sand, 0 to 3 percent slopes, occasionally floodedBuA43625138302lpzwsc09120131:15840
Buncombe loamy fine sandBe702525068kmcptn05919541:15840
Buncombe loamy sandBu315528401kqv6tn17119801:24000
Buncombe loamy fine sand, 0 to 3 percent slopes, frequently floodedBy66716896301tq66tn17919551:15840
Buncombe loamy sand, 2 to 5 percent slopes, rarely flooded2B2961181403yxzva00719941:24000
Buncombe-Toccoa complexBt9661186963zhxva03719701:15840
Buncombe loamy sandBn4201186953zhwva03719701:15840
Buncombe loamy fine sand, 0 to 4 percent slopes71B3181189323zrjva04119741:15840
Buncombe loamy fine sandyBd43712176842q0va06519501:15840
Buncombe loamy fine sand53351190573zwkva07519761:15840
Buncombe loamy fine sandyBu225119209401gva08719731:15840
Buncombe loamy fine sandBu211516939kbxgva11319671:15840
Buncombe loamy fine sand, 0 to 2 percent slopes, occasionally floodedBuA26311952140cjva11719901:24000
Buncombe loamy sand, 0 to 5 percent slopes5B336120212412tva14519841:15840
Buncombe loamy fine sandBe343120233413hva14719501:20000
Buncombe loamy fine sandBz362517410kcdnva15719581:20000
Buncombe loamy sand, 0 to 2 percent slopes, occasionally flooded6A1807705262rnwdva17519961:24000
Buncombe loamy sand, 0 to 2 percent slopes, occasionally flooded6A79417230291vtylva18320061:24000
Buncombe loamy fine sandBu56512068041kxva63119731:15840

Map of Series Extent

Approximate geographic distribution of the BUNCOMBE 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 .