Official Series Description


Lab Data Summary

Aggregate lab data for the BRADYVILLE soil series. This aggregation is based on all pedons with a current taxon name of BRADYVILLE, 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 BRADYVILLE 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
n/a40A43601965TN149006SBradyville5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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 BRADYVILLE 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 BRADYVILLE 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 BRADYVILLE 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 BRADYVILLE, 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 BRADYVILLE 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
Bradyville silt loam, 2 to 5 percent slopesBdB2138595293602qh79tn00319981:24000
Bradyville-Urban land complex, 2 to 10 percent slopesBnC3619529362krv6tn00319981:24000
Bradyville silt loam, 5 to 12 percent slopesBdC227165293612qh7btn00319981:24000
Bradyville silt loam, 2 to 5 percent slopesBrB3965244072qh79tn01519991:24000
Bradyville silt loam, 5 to 12 percent slopesBrC22815244082qh7btn01519991:24000
Bradyville silt loam, 2 to 5 percent slopesBvB10655234102qh79tn03719771:15840
Talbott-Rock outcrop-Bradyville complex, 5 to 20 percent slopes, erodedTbD2127635250372xmpztn05719961:24000
Talbott-Rock outcrop-Bradyville complex, 20 to 50 percent slopes, erodedTbE284325250382xmq1tn05719961:24000
Bradyville-Rock outcrop-Talbott complex, 5 to 20 percent slopes, erodedBrD22761525012km9wtn05719961:24000
Talbott-Rock outcrop-Bradyville complex, 5 to 20 percent slopes, erodedTbC21396328982xmpztn09320051:12000
Bradyville-Rock outcrop complex, 5 to 25 percent slopesBrE1416526152knhntn10719991:24000
Rock outcrop-Bradyville complex, 5 to 50 percent slopesRoF587526153knhptn10719991:24000
Bradyville-Rock outcrop complex, 25 to 50 percent slopesBrF366526154knhqtn10719991:24000
Bradyville silt loam, 2 to 5 percent slopesBrB230165240592qh79tn11719991:24000
Bradyville silt loam, 5 to 12 percent slopesBrC29655240602qh7btn11719991:24000
Hagerstown silt loam, eroded gently sloping phaseHa1467527785kq6btn11919551:20000
Hagerstown silty clay loam, severely eroded sloping phaseHb717527786kq6ctn11919551:20000
Hagerstown rocky silty clay loam, eroded gently sloping phaseHc504527787kq6dtn11919551:20000
Bradyville-Rock outcrop complex, 5 to 25 percent slopesBrE2481530228301hbtn14520051:24000
Bradyville silt loam, 2 to 5 percent slopesBrB195675282052qh79tn14919741:15840
Bradyville-Rock outcrop complex, 2 to 12 percent slopesBtC11737528210kqn1tn14919741:15840
Bradyville silt loam, 0 to 2 percent slopesBrA5277528204kqmvtn14919741:15840
Bradyville-Rock outcrop complex, 0 to 2 percent slopesBtA4005528209kqn0tn14919741:15840
Bradyville-Urban land complexBu2206528211kqn2tn14919741:15840
Bradyville silty clay loam, 2 to 5 percent slopes, severely erodedBsB31952528207kqmytn14919741:15840
Bradyville silt loam, 5 to 12 percent slopesBrC219305282062qh7btn14919741:15840
Bradyville silty clay loam, 5 to 12 percent slopes, severely erodedBsC3841528208kqmztn14919741:15840
Bradyville silt loam, 2 to 5 percent slopesBrB25655298092qh79tn15919921:24000
Talbott-Rock outcrop-Bradyville complex, 12 to 20 percent slopes, erodedTbD2154665300912xmq0tn16319911:20000
Talbott-Rock outcrop-Bradyville complex, 20 to 50 percent slopes, erodedTbE2117285300922xmq1tn16319911:20000
Bradyville silt loam, 5 to 12 percent slopesBrC23865300112qh7btn16919931:24000
Bradyville silt loam, 2 to 5 percent slopesBrB23625300102qh79tn16919931:24000
Talbott-Rock outcrop-Bradyville complex, 12 to 20 percent slopes, erodedTbD2510516897102xmq0tn17919551:15840
Talbott-Rock outcrop-Bradyville complex, 20 to 50 percent slopes, erodedTbE2320816897092xmq1tn17919551:15840
Hagerstown silt loam, 2 to 5 percent slopes, erodedHaB2750523510kkrftn18719611:15840
Hagerstown silt loam, 5 to 12 percent slopes, erodedHaC2315523511kkrgtn18719611:15840
Bradyville silt loam, 2 to 5 percent slopesBrB2166205284472qh79tn18919881:20000
Bradyville silt loam, 5 to 12 percent slopesBrC238735284482qh7btn18919881:20000
Bradyville silt loam, 2 to 5 percent slopes, eroded, rockyBvB21295528449kqwrtn18919881:20000

Map of Series Extent

Approximate geographic distribution of the BRADYVILLE 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 .