Official Series Description


Lab Data Summary

Aggregate lab data for the BANGTAIL soil series. This aggregation is based on all pedons with a current taxon name of BANGTAIL, 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 BANGTAIL 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 BANGTAIL 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 BANGTAIL 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 BANGTAIL 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 BANGTAIL 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 BANGTAIL 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 BANGTAIL 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 BANGTAIL 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 BANGTAIL, 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 BANGTAIL 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
Bangtail-Copenhaver complex, 8 to 25 percent slopes679E703015565556z4mt62219971:24000
Bangtail-Copenhaver-Adel complex, 15 to 35 percent slopes879E6288155760572jmt62219971:24000
Billman, stony-Bangtail-Tolbert, stony complex, 25 to 60 percent slopes660F385615564356yrmt62219971:24000
Bangtail-Timberlin complex, moist, 35 to 60 percent slopes, stony494F370215553356v6mt62219971:24000
Bangtail-Timberlin, stony complex, moist 15 to 45 percent slopes494E317615553256v5mt62219971:24000
Bangtail-Copenhaver complex, 35 to 60 percent slopes679F313815565656z5mt62219971:24000
Bangtail-Bridger complex, 15 to 45 percent slopes479E282715552056tsmt62219971:24000
Bangtail-Timberlin, stony complex, 15 to 45 percent slopes693E252015566356zdmt62219971:24000
Bangtail-Adel loams, 4 to 25 percent slopes679D241915565456z3mt62219971:24000
Bangtail-Timberlin complex, 35 to 60 percent slopes, stony693F151515566456zfmt62219971:24000
Bangtail-Doby-Redlodge complex, 4 to 45 percent slopes979E5031557765731mt62219971:24000
Bangtail clay loam, 35 to 60 percent slopes479F32915552156ttmt62219971:24000
Bangtail-Adel, cool, loams, 8 to 25 percent slopes579E31915560056xcmt62219971:24000
Martab-Bangtail complex, 25 to 60 percent slopes, stony892F227155762572lmt62219971:24000
Bynum-Bangtail complex, 4 to 15 percent slopes545C95924934252pqd9mt62420211:24000
Libeg, bouldery-Bangtail-Redchief, very stony complex, 4 to 35 percent slopes465E777024862612pg4zmt6321:24000
Philipsburg-Woodhall, stony-Bangtail complex, 15 to 35 percent slopes538E106024862642pg52mt6321:24000
Tophat-Adel-Bangtail complex, 4 to 25 percent slopes5547E3732496365swkymt6321:24000
Libeg, extremely bouldery-Bangtail, rubbly-Demast very stony complex, 15 to 60 percent slopes290F11423928012l9x4mt6321:24000
Bangtail-Timberlin complex, 35 to 60 percent slopes, stony169301465634xhvmt63619831:24000
Bangtail-Copenhaver complex, 35 to 60 percent slopes168211465614xhsmt63619831:24000
Redchief, very stony-Bangtail-Dailybasin, very bouldery complex, 8 to 45 percent slopes988F436023839262l0nvmt63720141:24000
Libeg, bouldery-Bangtail-Redchief, very stony complex, 4 to 35 percent slopes465E3977894120z0dlmt63720141:24000
Philipsburg-Woodhall, stony-Bangtail complex, 15 to 35 percent slopes538E294513895031hmwpmt63720141:24000
Bangtail-Copenhaver-Adel complex, 15 to 35 percent slopes879E17222493522572jmt63720141:24000
Bangtail-Adel complex, 4 to 25 percent slopes679D1628185853820cyvmt63720141:24000
Bangtail-Copenhaver complex, 35 to 60 percent slopes679F1509185853320cypmt63720141:24000
Libeg, extremely bouldery-Bangtail, rubbly-Demast very stony complex, 15 to 60 percent slopes290F129413861871hjfqmt63720141:24000
Bangtail-Copenhaver complex, 8 to 25 percent slopes679E727185853620cysmt63720141:24000
Tophat-Adel-Bangtail complex, 4 to 25 percent slopes5547E5712493530swkymt63720141:24000
Bangtail clay loam, 35 to 60 percent slopes479F1223775622kt1kmt63720141:24000
Tophat-Adel-Bangtail complex, 4 to 25 percent slopes5547E2645741487swkymt6691:24000
Bangtail, extremely stony-Woodhal, very stony-Dalys, extremely stony, complex, 4 to 70 percent slopes5705F1604699352rgqrmt6691:24000
Bridger-Bangtail complex, 8 to 35 percent slopes5526E955711066rvxmmt6691:24000
Bangtail-Timberlin, stony complex, 15 to 45 percent slopes693E157741556swn5mt6691:24000
Bangtail-Timberlin, stony complex, moist 15 to 45 percent slopes494E27741445swjlmt6691:24000
Bangtail-Timberlin complex, moist, 35 to 60 percent slopes, stony494F27741444swjkmt6691:24000
Bangtail-Copenhaver complex, 8 to 25 percent slopes679E19741638swqtmt6691:24000
Bangtail-Bridger complex, 15 to 45 percent slopes479E12741450swjrmt6691:24000
Bangtail-Inchau-Nieman complex, 15 to 45 percent slopes, stony623134625160622qfv2wy6301:24000

Map of Series Extent

Approximate geographic distribution of the BANGTAIL 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 .