Official Series Description


Lab Data Summary

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

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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 BRANDYWINE, 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 BRANDYWINE 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
Brandywine-Urban land complex, 8 to 15 percent slopesBtC57112857449skdc00119751:12000
Brandywine gravelly loam, 15 to 40 percent slopesBrD29212857249shdc00119751:12000
Brandywine-Urban land complex, 0 to 8 percent slopesBtB20312857349sjdc00119751:12000
Brandywine-Urban land complex, 15 to 40 percent slopesBtD16212857549sldc00119751:12000
Urban land-Brandywine complex, 0 to 8 percent slopesUdB12712867449wsdc00119751:12000
Brandywine gravelly loam, 8 to 15 percent slopesBrC6112857149sgdc00119751:12000
Brandywine loam, 15 to 60 percent slopes5E116533970kxmvmd51019931:12000
Brandywine gravelly loam, 15 to 25 percent slopes, severely erodedBrD3553533360kx05md60019721:15840
Brandywine gravelly loam, 8 to 15 percent slopes, moderately erodedBrC2497533359kx04md60019721:15840
Brandywine gravelly loam, 25 to 45 percent slopes, severely erodedBrE3152533361kx06md60019721:15840
Brandywine stony loam, very deep, 25 to 50 percent slopesBnF8737516934kbx9va11319671:15840
Brandywine stony loam, very deep, 7 to 25 percent slopesBnD2625516933kbx8va11319671:15840
Brandywine loam, very deep, 15 to 25 percent slopesBeD2585516931kbx6va11319671:15840
Brandywine loam, very deep, 25 to 45 percent slopesBeF1629516932kbx7va11319671:15840
Brandywine loam, very deep, 5 to 15 percent slopesBeC1480516930kbx5va11319671:15840
Brandywine fine gravelly loam 15 to 25 percent slopesBdD912516929kbx4va11319671:15840
Chester-Brandywine loams, very deep, 7 to 15 percent slopesCkC853516953kbxxva11319671:15840
Chester-Brandywine loams, very deep, 2 to 7 percent slopesCkB642516952kbxwva11319671:15840
Chester-Brandywine loams, very deep, 7 to 15 percent slopes, erodedCkC2533516954kbxyva11319671:15840
Chester-Brandywine loams, very deep, 15 to 25 percent slopesCkD373516955kbxzva11319671:15840
Brandywine fine gravelly loam, 7 to 15 percent slopesBdC295516928kbx3va11319671:15840
Brandywine loam, moderately steep phaseBoD10165517400kcdbva15719581:20000
Brandywine stony loam, steep phaseByE8126517409kcdmva15719581:20000
Brandywine loam, sloping phaseBoC7563517399kcd9va15719581:20000
Eubanks-Brandywine complex, sloping phasesEbC5282517424kcf3va15719581:20000
Brandywine stony loam, moderately steep phaseByD5075517408kcdlva15719581:20000
Brandywine loam, steep phaseBoE3840517401kcdcva15719581:20000
Chester-Brandywine loams, eroded sloping phasesCeC23577517415kcdtva15719581:20000
Brandywine gritty loam, sloping phaseBgC3516517397kcd7va15719581:20000
Brandywine rocky loam, moderately steep phaseBrD3005517403kcdfva15719581:20000
Brandywine gritty loam, moderately steep phaseBgD1975517398kcd8va15719581:20000
Brandywine stony loam, sloping phaseByC1880517407kcdkva15719581:20000
Eubanks-Brandywine complex eroded moderately steep phasesEbD21513517425kcf4va15719581:20000
Brandywine rocky loam, steep phaseBrE1476517404kcdgva15719581:20000
Brandywine rocky loam, sloping phaseBrC1008517402kcddva15719581:20000
Brandywine silt loam, eroded sloping phaseBwC2638517405kcdhva15719581:20000
Brandywine silt loam, eroded moderately steep phaseBwD2474517406kcdjva15719581:20000
Chester-Brandywine loams, eroded gently sloping phasesCeB2452517414kcdsva15719581:20000
Brandywine gritty loam, gently sloping phaseBgB261517396kcd6va15719581:20000

Map of Series Extent

Approximate geographic distribution of the BRANDYWINE 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 .