Official Series Description


Lab Data Summary

Aggregate lab data for the ABSTED soil series. This aggregation is based on all pedons with a current taxon name of ABSTED, 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 ABSTED were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
58B40A3099S1966WY019012Absted3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8086128,-106.4719467
58B40A3811S1977WY005003ABSTED7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2844429,-105.101387
58B40A3813S1977WY005005ABSTED8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0883331,-105.4616699
58B40A3817S1977WY005009ABSTED8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0888901,-105.422226

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ABSTED 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 ABSTED 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 ABSTED 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 ABSTED 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 mountains figure.

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Competing Series

Soil series competing with ABSTED 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 ABSTED series and competing. 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 ABSTED 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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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 ABSTED, 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 ABSTED 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
Absted clay loam, 0 to 3 percent slopesAb11665954782w4ppco62619741:24000
Absted silt loamAa2866355081cxh7sd04719801:24000
Absted silt loamAb52422580999cy1wsd61120111:24000
Absted-Bone complex, 0 to 3 percent slopes10141903491762zj57wy01119781:24000
Absted-Bone complex, moist, 0 to 3 percent slopesP002A17625474342qt0hwy01119781:24000
Absted-Cambria loams, 0 to 3 percent slopes1017877349515cqppwy02719931:24000
Absted-Arvada complex, 0 to 3 percent slopes1005799349513cqpmwy02719931:24000
Absted-Forkwood association19465152052536xwy04319761:24000
Absted-Bone complex, 0 to 6 percent slopes132179349381cqkcwy04519841:24000
Absted-Arvada complex, 0 to 3 percent slopes15233416148371r6cjwy04519841:24000
Keyner-Absted-Slickspots complex, 0 to 6 percent slopes186687916697042v08twy60920061:24000
Absted-Arvada-Slickspots complex, 0 to 6 percent slopes101132929206402v093wy60920061:24000
Absted-Arvada-Bone complex, 0 to 6 percent slopes1006416697781t1jtwy60920061:24000
Petrie-Bone-Absted complex, 0 to 6 percent slopesPE133693509012yv7qwy61919711:24000
Briggsdale-Bidman complex, rollingBRD8901350815cs1mwy61919711:24000
Absted-Wyarno complex, slopingADC8156350805cs19wy61919711:24000
Stoneham-Absted complexSTa5874350937cs5kwy61919711:24000
Absted-Wyarno complex, gently slopingADB2210350804cs18wy61919711:24000
Absted-Bone complexAB1845350803cs17wy61919711:24000
Lohsman-Orella complex, hillyLTD1543350879cs3pwy61919711:24000
Absted clayAa377350810cs1gwy61919711:24000
Keyner-Absted-Slickspots complex, 0 to 6 percent slopes209898045023072v08twy62519851:24000
Arvada-Absted-Slickspots complex, 0 to 6 percent slopes112702815021902v099wy62519851:24000
Ulm-Absted complex, 0 to 6 percent slopes2932490502429jvtdwy62519851:24000
Absted-Forkwood complex, 3 to 15 percent slopes -- Draft70215263753tswy6291:24000
Absted-Slickspots complex, 0 to 6 percent slopes1038203359309d1wmwy63319871:24000
Absted-Haverdad association, moist, 0 to 6 percent slopes1023487339847cdmtwy63319871:24000
Absted-Haverdad, rarely flooded very fine sandy loams, 0 to 6 percent slopes1011798339845cdmrwy63319871:24000
Absted-Arvada-Slickspots complex, 0 to 6 percent slopes253263329206412v093wy70520031:24000
Absted-Slickspots complex, 0 to 6 percent slopes25252817504wfp3wy70520031:24000
Absted-Arvada-Bone complex, 0 to 6 percent slopes10157399351479csr1wy70919831:24000
Absted-Arvada complex, 0 to 3 percent slopes22393414278411jxsdwy70919831:24000
Arvada-Absted-Slickspots complex, 0 to 6 percent slopes2504114279072v099wy70919831:24000
Absted-Bone complex, 0 to 6 percent slopes2412714278981jxv7wy70919831:24000
Absted-Slickspots complex, 0 to 6 percent slopes665133016740941t611wy71920131:24000
Absted-Haverdad, rarely flooded very fine sandy loams, 0 to 6 percent slopes66454516740951t612wy71920131:24000

Map of Series Extent

Approximate geographic distribution of the ABSTED 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 .