Official Series Description


Lab Data Summary

Aggregate lab data for the BRASSTOWN soil series. This aggregation is based on all pedons with a current taxon name of BRASSTOWN, 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 BRASSTOWN were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
130B04N077904TN155001Brasstown7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.720654,-83.375995
130B85P062885NC039002Brasstown7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.0941658,-84.1233368

Water Balance

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

Click the image to view it full size.



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 BRASSTOWN series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the BRASSTOWN series and siblings. 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 BRASSTOWN 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 .

Click the image to view it full size.

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 flats position figure.

Competing Series

Soil series competing with BRASSTOWN share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the BRASSTOWN 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 BRASSTOWN 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 BRASSTOWN, 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

No block diagrams are available.

Map Units

Map units containing BRASSTOWN 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
Junaluska-Brasstown complex, basin, 15 to 30 percent slopesJbD291316720332vx32nc02120061:12000
Junaluska-Brasstown complex, basin, 8 to 15 percent slopesJbC160516720322vx39nc02120061:12000
Junaluska-Brasstown complex, basin, 30 to 50 percent slopesJbE141916720342vx37nc02120061:12000
Junaluska-Brasstown complex, 2 to 8 percent slopesJbB32616720311t3whnc02120061:12000
Junaluska-Brasstown complex, 15 to 30 percent slopesJbD3347824231232vx31nc03920091:12000
Junaluska-Brasstown complex, 30 to 50 percent slopesJbE3175024231242vx36nc03920091:12000
Junaluska-Brasstown complex, 8 to 15 percent slopesJbC1035424231222vx38nc03920091:12000
Junaluska-Brasstown complex, 30 to 50 percent slopes, rockyJkE474024231262vx3bnc03920091:12000
Farner-Brasstown complex, 15 to 30 percent slopesFbD201724231042mbfnnc03920091:12000
Farner-Brasstown complex, 8 to 15 percent slopesFbC134124231032mbfmnc03920091:12000
Junaluska-Brasstown-Urban land complex, 15 to 30 percent slopesJnD67424231282mbgfnc03920091:12000
Junaluska-Brasstown-Urban land complex, 2 to 15 percent slopesJnC42524231272mbgdnc03920091:12000
Junaluska-Brasstown complex, 2 to 8 percent slopesJbB15624231212mbg6nc03920091:12000
Farner-Brasstown complex, 2 to 8 percent slopesFbB6524231022mbflnc03920091:12000
Junaluska-Brasstown complex, 30 to 50 percent slopesJbE57185464272vx36nc04319911:12000
Junaluska-Brasstown complex, 15 to 30 percent slopesJbD46175464262vx31nc04319911:12000
Brasstown-Junaluska complex, 8 to 15 percent slopesBsC1192546385lbkbnc04319911:12000
Junaluska-Brasstown complex, 30 to 50 percent slopesJbE1267119127532vx36nc07520071:12000
Junaluska-Brasstown complex, 15 to 30 percent slopesJbD697819127522vx31nc07520071:12000
Junaluska-Brasstown complex, 8 to 15 percent slopesJbC30119127542vx38nc07520071:12000
Junaluska-Brasstown-Urban land complex, 8 to 50 percent slopesJnD2081912755226csnc07520071:12000
Junaluska-Brasstown complex, 30 to 50 percent slopesJbE13895470802vx36nc09919911:12000
Junaluska-Brasstown complex, 15 to 30 percent slopesJbD9205470792vx31nc09919911:12000
Junaluska-Brasstown complex, 25 to 60 percent slopesJbE57415472052vx35nc11119891:24000
Junaluska-Brasstown complex, 6 to 25 percent slopesJbD1790547204lcdrnc11119891:24000
Brasstown-Junaluska complex, 30 to 50 percent slopesBsE29025457982vx2znc11319901:12000
Brasstown-Junaluska complex, 15 to 30 percent slopesBsD11595457972vx2wnc11319901:12000
Brasstown-Junaluska complex, 50 to 95 percent slopesBsF546545799l9yfnc11319901:12000
Brasstown-Junaluska complex, 8 to 15 percent slopesBsC91545796l9ybnc11319901:12000
Junaluska-Brasstown complex, basin, 30 to 50 percent slopesJbE160016713922vx37nc11520061:12000
Junaluska-Brasstown complex, basin, 15 to 30 percent slopesJbD150816713912vx32nc11520061:12000
Junaluska-Brasstown complex, 50 to 95 percent slopesJbF13716713931t36xnc11520061:12000
Brasstown-Junaluska complex, high precipitation, 15 to 30 percent slopesFfE188623935092vx2xnc17519681:12000
Brasstown-Junaluska complex, 8 to 15 percent slopesFfD69023903802l7d1nc17519681:12000
Brasstown-Junaluska complex, 30 to 50 percent slopesBsE893319125942vx2znc60520071:12000
Brasstown-Junaluska complex, 15 to 30 percent slopesBsD413619125912vx2wnc60520071:12000
Junaluska-Brasstown-Tsali-Urban land complex, 30 to 95 percent slopesJgF6401910253223s2nc60520071:12000
Junaluska-Brasstown-Tsali-Urban land complex, 15 to 30 percent slopesJgD5801910252223s1nc60520071:12000
Brasstown-Junaluska complex, 8 to 15 percent slopesBsC18319125962266nnc60520071:12000
Junaluska-Brasstown-Tsali-Urban land complex, 2 to 15 percent slopesJgC25756320td0fnc60520071:12000
Brasstown-Junaluska complex, basin, 30 to 50 percent slopesBsE85725467502vx30nc60619911:12000
Brasstown-Junaluska complex, basin, 15 to 30 percent slopesBsD39265467492vx2ync60619911:12000
Brasstown-Junaluska complex, 8 to 15 percent slopesBsC256546748lby1nc60619911:12000
Junaluska-Brasstown complex, 35 to 50 percent slopes43F231523959442lf5jtn05919541:15840
Junaluska-Brasstown complex, 20 to 35 percent slopes43E142823959432lf5htn05919541:15840
Junaluska-Brasstown complex, 12 to 20 percent slopes43D101223959422lf5gtn05919541:15840
Brasstown loam, 2 to 12 percent slopes53C17923959452lf5ktn05919541:15840
Brasstown loam, 50 to 80 percent slopes53G16423959492lf5ptn05919541:15840
Brasstown loam, 35 to 50 percent slopes53F9423959482lf5ntn05919541:15840
Brasstown loam, 20 to 35 percent slopes53E923959472lf5mtn05919541:15840
Junaluska-Brasstown complex, 15 to 35 percent slopesJnD161695237622vx33tn13919971:24000
Junaluska-Brasstown complex, 5 to 15 percent slopesJnC382523761kl0jtn13919971:24000
Brasstown loam, 12 to 20 percent slopesBtD606213872491hkjztn60620011:24000
Junaluska-Brasstown complex, 35 to 50 percent slopesJbF1909524799km30tn60620011:24000
Junaluska-Brasstown complex, 20 to 35 percent slopesJbE1809524798km2ztn60620011:24000
Brasstown loam, 50 to 80 percent slopesBtG1578524761km1stn60620011:24000
Junaluska-Brasstown complex, 12 to 20 percent slopesJbD1573524797km2ytn60620011:24000
Brasstown loam, 20 to 35 percent slopesBtE825524759km1qtn60620011:24000
Brasstown loam, 2 to 12 percent slopesBtC589524757km1ntn60620011:24000
Brasstown loam, 35 to 50 percent slopesBtF144524760km1rtn60620011:24000
Junaluska-Brasstown complex, 30 to 50 percent slopes, stonyJbE12784553571ll14tn64020071:24000
Junaluska-Brasstown complex, 15 to 30 percent slopes, stonyJbD6547553570ll13tn64020071:24000

Map of Series Extent

Approximate geographic distribution of the BRASSTOWN 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 .