Official Series Description


Lab Data Summary

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

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

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 BARBERMILL 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 BARBERMILL 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 BARBERMILL 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 BARBERMILL, 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 BARBERMILL 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
Adelmann-Barbermill-Breadloaf complex, 25 to 50 percent slopes307682225192082185yid00120121:24000
Barbermill soils-Breadloaf complex, 25 to 90 percent slopes3079197251921121860id00120121:24000
Barbermill-Brisbois-Sorf complex, 15 to 55 percent south slopes252362034349162lb04or6181:24000
Sorf-Barbermill-Badland complex, 20 to 50 percent south slopes189E12923429496t74cor6271:24000
Simas-Barbermill-Badland complex, 2 to 20 percent slopes188C10963425159t73wor6271:24000
Simas-Barbermill-Badland complex, 20 to 50 percent north slopes188E5403432025t73xor6271:24000
Sorf-Barbermill-Badland complex, 2 to 20 percent slopes189C5183432027t746or6271:24000
Simas-Barbermill-Badland complex, 20 to 50 percent slopes112E4983425060t6sjor6271:24000
McCoin-Barbermill-Badland complex, 20 to 50 percent south slopes154E4033425138nk4tor6271:24000
Cooperopolis-Barbermill-Badland complex, 5 to 40 percent slopes129E1823432223t732or6271:24000
Reywat-Barbermill-Rock outcrop complex, 10 to 40 percent slopes109E733425187t6sfor6271:24000
Barbermill-Mitchtown-Meadowridge complex, 30 to 60 percent slopes362E21073421847269tor6771:24000
Simas-Barbermill-Badland complex, 20 to 50 percent slopes112E9413421977t6sjor6771:24000
McCoin-Barbermill-Badland complex, 20 to 50 percent south slopes154E2283424680nk4tor6771:24000
Simas-Barbermill-Badland complex, 2 to 20 percent slopes188C1313424766t73wor6771:24000
Reywat-Barbermill-Rock outcrop complex, 10 to 40 percent slopes109E353424862t6sfor6771:24000

Map of Series Extent

Approximate geographic distribution of the BARBERMILL 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 .