Official Series Description


Lab Data Summary

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

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with BAXTON, 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 BAXTON 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
Baxton-Connieo, very bouldery-Rock outcrop complex, 15 to 35 percent slopes, moist1242E540015055051ngmt62719981:24000
Baxton-Connieo, very bouldery-Rock outcrop complex, 4 to 15 percent slopes, moist1242D285115054951nfmt62719981:24000
Connieo, very stony-Baxton, bouldery-Rock outcrop complex, 35 to 60 percent slopes1624F157915064951rnmt62719981:24000
Baxton-Connieo complex, 15 to 35 percent slopes1245E147315055551nmmt62719981:24000
Connieo-Baxton-Rock outcrop complex, 15 to 35 percent slopes1623E101715064851rmmt62719981:24000
Baxton-Connieo, very bouldery-Rock outcrop complex, 4 to 15 percent slopes1244D96915055351nkmt62719981:24000
Breeton-Baxton-Connieo complex, 4 to 15 percent slopes1802D81815072051tymt62719981:24000
Baxton-Connieo coarse sandy loams, 4 to 15 percent slopes, bouldery1243D71715055151nhmt62719981:24000
Catgulch-Baxton complex, 2 to 15 percent slopes, stony1661D65715067251sdmt62719981:24000
Catgulch-Baxton complex, 15 to 35 percent slopes, stony1661E63615067351sfmt62719981:24000
Baxton-Connieo-Rock outcrop complex, 15 to 35 percent slopes1244E62015055451nlmt62719981:24000
Baxton-Kellygulch-Connieo complex, 15 to 45 percent slopes1247E60615055751npmt62719981:24000
Connieo, very stony-Baxton, stony-Rock outcrop complex, 15 to 35 percent slopes1621E54915064551rjmt62719981:24000
Baxton, stony-Breeton, bouldery-Catgulch, very stony, complex, 15 to 35 percent slopes1246E53515055651nnmt62719981:24000
Connieo, stony-Baxton, stony-Rock outcrop complex, 2 to 15 percent slopes1621D36115064451rhmt62719981:24000
Catgulch, extremely bouldery-Baxton, extremely bouldery-Burtoner, bouldery, complex, 15 to 35 percent slopes1667E25515067851slmt62719981:24000
Baxton, very stony-Dominic, extremely stony-Catgulch, extremely stony complex, 8 to 35 percent slopes565E14424862692pg57mt6321:24000
Baxton-Connieo, very bouldery-Rock outcrop complex, 15 to 35 percent slopes, moist1242E67017030511v554mt63520061:24000
Baxton-Connieo complex, 4 to 15 percent slopes, bouldery1243D42317030521v555mt63520061:24000
Baxton-Connieo, very bouldery-Rock outcrop complex, 4 to 15 percent slopes, moist1242D13717030501v553mt63520061:24000
Connieo, very stony-Baxton, bouldery-Rock outcrop complex, 35 to 60 percent slopes1624F13117030631v55jmt63520061:24000
Catgulch-Baxton complex, 2 to 15 percent slopes, stony1661D7417030711v55smt63520061:24000
Baxton-Connieo-Rock outcrop complex, 15 to 35 percent slopes1244E5017030531v556mt63520061:24000
Baxton-Connieo, very bouldery-Rock outcrop complex, 15 to 35 percent slopes, moist2152151465914xjrmt63619831:24000
Baxton-Connieo coarse sandy loams, 4 to 15 percent slopes, bouldery214131465924xjsmt63619831:24000
Connieo-Baxton-Rock outcrop complex, 2 to 15 percent slopes, stony22411465944xjvmt63619831:24000
Catgulch-Baxton complex, 15 to 35 percent slopes, stony22311465954xjwmt63619831:24000
Baxton, very stony-Riverside, extremely stony-Catgulch, extremely stony complex, 8 to 35 percent slopes565E2021816843wdzsmt63720141:24000
Rochester-Baxton complex, 15 to 35 percent slopes395E146813896491hn1dmt64520131:12000

Map of Series Extent

Approximate geographic distribution of the BAXTON 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 .