Official Series Description


Lab Data Summary

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

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with BREVARD 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 BREVARD 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 BREVARD 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.

Click the image to view it full size.

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 BREVARD, 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-2010-09-27-07 | Burke County - 2006

    Typical relationship between soils, landform, and parent material in the Cliffield-Pigeonroost general soil map unit in the South Mountains (Soil Survey of Burke County, North Carolina; 2006).

  2. NC-2010-09-28-12 | Surry County - 2007

    Relationship of soils, landscape, and geology in the Cowee-Evard general soil map unit and the Chestnut-Peaks general soil map unit (Soil Survey of Surry County, North Carolina; 2007).

Map Units

Map units containing BREVARD 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
Brevard fine sandy loam, 1 to 6 percent slopes, rarely floodedBvB7701167833xj6nc02320001:24000
Brevard loam, 7 to 15 percent slopesBrC2899546842lc12nc08919741:20000
Brevard loam, 15 to 25 percent slopesBrE2634546843lc13nc08919741:20000
Brevard loam, 25 to 45 percent slopesBrF65546844lc14nc08919741:20000
Brevard-Greenlee complex, 8 to 25 percent slopes, very boulderyBrE12624247762md5lnc09720111:12000
Brevard-Greenlee complex, 25 to 60 percent slopes, very boulderyBrF2424247772md5mnc09720111:12000
Brevard sandy loam, 8 to 15 percent slopesBrC3561110743ql1nc14919921:24000
Brevard-Greenlee complex, 25 to 60 percent slopes, extremely boulderyBrE314813836691hfthnc16919921:24000
Brevard-Greenlee complex, 8 to 25 percent slopes, extremely boulderyBrD65213836701hftjnc16919921:24000
Brevard-Greenlee complex, 8 to 25 percent slopes, very boulderyBrD65214275531jxh3nc17120051:24000
Brevard-Greenlee complex, 25 to 60 percent slopes, very boulderyBrE52812750948p6nc17120051:24000
Brevard loam, 10 to 25 percent slopesBvE334323903612l7cfnc17519681:15840
Brevard loam, 25 to 45 percent slopesBvF48623903632l7chnc17519681:15840
Evard-Brevard association, steepEVF208131324804fvksc04519721:20000
Brevard-Evard complex, 15 to 25 percent slopesBvE169421324634fv0sc04519721:20000
Brevard fine sandy loam, 10 to 15 percent slopesBrD48631324604ftxsc04519721:20000
Brevard fine sandy loam, 6 to 10 percent slopesBrC39141324594ftwsc04519721:20000
Brevard sandy clay loam, 10 to 25 percent slopes, erodedBsE212781324624ftzsc04519721:20000
Brevard sandy clay loam, 2 to 10 percent slopes, erodedBsC25681324614ftysc04519721:20000
Tusquitee loam, 4 to 10 percent slopesTuC5101310774dd9sc07719671:20000
Brevard fine sandy loam, 7 to 15 percent slopes7C13091307474d1nsc60419821:24000
Brevard fine sandy loam, 15 to 50 percent slopes7E7211307484d1psc60419821:24000
Brevard loam, 15 to 25 percent slopesBrD1803523733kkzmtn13919971:24000
Brevard loam, 25 to 45 percent slopesBrE974523734kkzntn13919971:24000
Brevard loam, 5 to 15 percent slopesBrC854523732kkzltn13919971:24000
Brevard-Greenlee complex, 8 to 25 percent slopes, very bouldery7D2016705041t297va07720061:24000

Map of Series Extent

Approximate geographic distribution of the BREVARD 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 .