Official Series Description


Lab Data Summary

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

Competing Series

Soil series competing with BRANHAM 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 BRANHAM 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 BRANHAM 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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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with BRANHAM, 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 BRANHAM 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
Libeg-Branham-Sebud families, complex, moderately steep mountain slopes537C781202406225y6bid75819981:24000
Bearmouth-Branham-Marcetta families, complex, steep mountain slopes541E34381486764zq0mt60520071:24000
Bearmouth-Branham families-Rock outcrop complex, steep mountain slopes542Pr30021486814zq5mt60520071:24000
Libeg-Branham-Sebud families, complex, moderately steep mountain slopes537C26001486624zpkmt60520071:24000
Bearmouth-Tiban-Branham families, complex, steep mountain slopes542P12931487934ztsmt60520071:24000
Branham-Rock outcrop complex, 8 to 45 percent slopes2247185961820f2pmt60520071:24000
Bearmouth-Branham-Marcetta families, complex, steep mountain slopes541E11825977174zq0mt61220111:24000
Woodtick-Branham-Rock outcrop complex, 4 to 35 percent slopes992F139624811122p8swmt61420121:24000
Stecum-Goldflint-Branham complex, 12 to 35 percent slopes335E13516975471tzflmt61620031:24000
Caseypeak-Branham-Rock outcrop complex, 15 to 35 percent slopes1842E125215074051vlmt62719981:24000
Caseypeak-Branham-Rock outcrop complex, 2 to 15 percent slopes1842D104815073951vkmt62719981:24000
Tuggle-Branham-Rock outcrop complex, 2 to 15 percent slopes1841D66415073851vjmt62719981:24000
Branham-Opitz-Tuggle complex, 2 to 15 percent slopes171D52715068851sxmt62719981:24000
Branham-Clugulch-Rock outcrop complex, 15 to 35 percent slopes172E42315069651t5mt62719981:24000
Branham-Tuggle complex, 15 to 35 percent slopes1853E38115074651vsmt62719981:24000
Caseypeak, bouldery-Branham, bouldery-Rock outcrop complex, 35 to 60 percent slopes1842F33715074151vmmt62719981:24000
Branham-Opitz-Tuggle complex, 15 to 35 percent slopes171E32515068951symt62719981:24000
Branham-Lowder loams, 0 to 8 percent slopes1851D25815074351vpmt62719981:24000
Opitz, bouldery-Branham, very bouldery-Tuggle, very bouldery, complex, 8 to 35 percent slopes2051E23315082051y5mt62719981:24000
Branham-Clugulch-Rock outcrop complex, 2 to 15 percent slopes172D18815069551t4mt62719981:24000
Branham, stony-Tuggle, very stony-Rock outcrop complex, 35 to 60 percent slopes173F18515070551tgmt62719981:24000
Branham-Lowder loams, 8 to 25 percent slopes1851E16515074451vqmt62719981:24000
Branham-Tuggle complex, 2 to 15 percent slopes1853D16415074551vrmt62719981:24000
Wissikihon-Branham-Highrye complex, 8 to 30 percent slopes306E47517031331v57smt63520061:24000
Caseypeak-Branham-Rock outcrop complex, 15 to 35 percent slopes1842E33917030771v55zmt63520061:24000
Silas, stony-Branham, stony-Tepete complex, 2 to 15 percent slopes319D22717031401v580mt63520061:24000
Stecum-Goldflint-Branham complex, 12 to 35 percent slopes335E16017031461v586mt63520061:24000
Branham-Clugulch-Rock outcrop complex, 15 to 35 percent slopes172E14317030241v548mt63520061:24000
Minestope, extremely bouldery-Branham, extremely bouldery-Rock outcrop complex, 8 to 35 percent slopes384E11317031591v58mmt63520061:24000
Branham-Opitz-Tuggle complex, 2 to 15 percent slopes171D8017030231v547mt63520061:24000
Branham-Tuggle complex, 15 to 35 percent slopes1853E6617030781v560mt63520061:24000
Oro Fino-Highrye-Branham complex, 4 to 15 percent slopes312D5617031341v57tmt63520061:24000
Beeftrail-Branham-Minestope complex, 2 to 15 percent slopes305D3517031321v57rmt63520061:24000
Branham-Rock outcrop complex, 8 to 45 percent slopes22100461464444xd0mt63619831:24000
Earcree, dry-Branham-Rock outcrop complex, 35 to 60 percent slopes4441821464684xdsmt63619831:24000
Branham coarse sandy loam, 2 to 8 percent slopes2125321464434xczmt63619831:24000
Caseypeak-Branham-Rock outcrop complex, 15 to 35 percent slopes2222471465964xjxmt63619831:24000
Bearmouth-Branham-Marcetta families, complex, steep mountain slopes2862017101431vdjxmt63619831:24000
Bearmouth-Branham families-Rock outcrop complex, steep mountain slopes2911117101481vdk2mt63619831:24000
Branham-Opitz-Tuggle complex, 2 to 15 percent slopes21691465804xjdmt63619831:24000
Minestope, extremely bouldery-Branham, extremely bouldery-Rock outcrop complex, 8 to 35 percent slopes384E3615362083d4s3mt67020071:24000
Wissikihon-Branham-Highrye complex, 8 to 30 percent slopes306E2666750072t5hwmt67020071:24000
Beeftrail-Branham-Minestope complex, 2 to 15 percent slopes305D2415362085d4s5mt67020071:24000
Stecum-Goldflint-Branham complex, 12 to 35 percent slopes335E2269362258d4yrmt67020071:24000
Silas, stony-Branham, stony-Tepete complex, 2 to 15 percent slopes319D139813798631h9vqmt67020071:24000
Oro Fino-Highrye-Branham complex, 4 to 15 percent slopes312D978362084d4s4mt67020071:24000
Beeftrail, stony-Branham, stony-Fleecer complex, 8 to 20 percent slopes324E650362390d530mt67020071:24000
Fleecer-Branham-Passmore complex, 2 to 8 percent slopes326C408362103d4srmt67020071:24000
Branham-Rogert complex, 5 to 25 percent slopes, stony602696224554822nf43wy6301:24000
Blackbear, rubbly-Branham, rubbly-Bobowic complex, 4 to 25 percent slopes7502752716987191v0ndwy6351:24000
Blackbear, rubbly-Branham, rubbly-Bobowic complex, 4 to 25 percent slopes750212525144071v0ndwy66219981:24000

Map of Series Extent

Approximate geographic distribution of the BRANHAM 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 .