Official Series Description


Lab Data Summary

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

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Soil series sharing subgroup-level classification with ABSAROOK, 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 ABSAROOK 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
Tolbert-Absarook-Rock outcrop complex, 15 to 35 percent slopes870E5853155759572hmt62219971:24000
Absarook-Tolbert complex, 4 to 15 percent slopes470D509715551756tpmt62219971:24000
Absarook-Farnuf-Tolbert complex, 4 to 15 percent slopes668D102715565156z0mt62219971:24000
Tolbert-Absarook-Rock outcrop complex, 4 to 15 percent slopes870D892155758572gmt62219971:24000
Farnuf-Absarook-Tolbert complex, 2 to 8 percent slopes668C85715565056yzmt62219971:24000
Absarook, stony-Meagher, extremely bouldery-Bacbuster, very bouldery complex, 4 to 15 percent slopes450D672485203wckrmt62420211:24000
Absarook-Beenom complex, 2 to 15 percent slopes461D474151091526xmt62719981:24000
Tolbert, very stony-Rock outcrop-Absarook, stony, complex, 8 to 35 percent slopes245E350150929521pmt62719981:24000
Martinsdale-Absarook-Whitlash complex, 2 to 8 percent slopes, stony735C17815131252g1mt62719981:24000
Absarook-Martinsdale, stony, complex, 2 to 8 percent slopes911C7715160552rhmt62719981:24000
Tolbert-Vershal-Absarook complex, 4 to 15 percent slopes70D151623927662l9w0mt6321:24000
Absarook, stony-Meagher, extremely bouldery-Bacbuster, very bouldery complex, 4 to 15 percent slopes450D10902486258wckrmt6321:24000
Absarook, stony-Cedric, very stony-Pachel complex, 2 to 8 percent slopes90C25223927702l9w4mt6321:24000
Tolbert-Vershal-Absarook complex, 4 to 15 percent slopes70D18368603552n81fmt63720141:24000
Absarook, stony-Gnojek, very stony complex, 2 to 8 percent slopes90C1091713833841hfj9mt63720141:24000
Newlancreek-Sixteenmile-Absarook complex, 2 to 8 percent slopes72C7528639639pgljmt63720141:24000
Absarook, stony-Meagher, extremely bouldery-Bacbuster, very bouldery complex, 4 to 15 percent slopes450D6174815478wckrmt63720141:24000
Meagher, extremely stony-Absarook, very stony-complex, 4 to 15 percent slopes240D3174814055wb2vmt63720141:24000
Newlancreek-Absarook complex, 4 to 15 percent slopes, stony167D3112813822w9vbmt63720141:24000
Ticell-Vershal-Absarook complex, 2 to 8 percent slopes71C1375603553n81gmt63720141:24000
Absarook. stony-Castner, very stony complex, 4 to 15 percent slopes672D668817721wfx3mt63720141:24000
Newlancreek, very bouldery-Absarook, stony complex, 15 to 35 percent slopes167E547894127z0dtmt63720141:24000
Bacbuster-Bigbear-Vershal complex, 4 to 35 percent slopes5501E284461566445801mt6691:24000
Vershal, very cobbly - Sawicki, extremely stony - Absarook complex, 8 to 45 percent slopes5610E5845156732582wmt6691:24000
Absarook-Absarokee-Vershal complex, 4 to 25 percent slopes5545E3622699264rgmxmt6691:24000
Absarook, very stony-Whitlash, extremely cobbly-Meagher, very stony complex, 4 to 35 percent slopes7503E244215648457twmt6691:24000
Absarook-Corpening-like complex, 2 to 20 percent slopes5C21335834430zvqwy6171:24000
Absarook loam, 1 to 6 percent slopes2A08335833330zvcwy6171:24000
Absarook-Southbaldy-like-Corpening complex, 2 to 15 percent slopes5C16335832830zv6wy6171:24000
Joegale-like-Absarook-Wickes-like complex, 2 to 45 percent slopes4D04335832530zv3wy6171:24000
Absarook-Pesowyo-Tickell-like complex, 3 to 40 percent slopes4C01335832430zv2wy6171:24000
Absarook-Wickes-like-Reva-like complex, 6 to 60 percent slopes4D01335831630zttwy6171:24000
Pesowyo, very stony-Absarook-Hangmans complex, 3 to 45 percent slopes4D09335837131jymwy6171:24000

Map of Series Extent

Approximate geographic distribution of the ABSAROOK 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 .