Official Series Description


Lab Data Summary

Aggregate lab data for the AUSABLE soil series. This aggregation is based on all pedons with a current taxon name of AUSABLE, 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 AUSABLE 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
94A92P031291MI039001Ausable6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7133331,-84.6624985

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the AUSABLE 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 AUSABLE 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 AUSABLE 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 AUSABLE 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 AUSABLE 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 AUSABLE 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 AUSABLE 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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Click the image to view it full size.

Soil series sharing subgroup-level classification with AUSABLE, 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 AUSABLE 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
Ausable muck, frequently flooded8724501903786d37mi00119931:20000
Ausable muck, frequently flooded8722121913106f29mi00719981:12000
Ausable-Winterfield-Tawas complex, 0 to 2 percent slopes, frequently floodedAusaaA73404460317s5mi00919761:15840
Thunderbay, Colonville, and Ausable soils, 0 to 2 percent slopes, frequently floodedThuabA5070340445631b26mi01119641:20000
Ausable-Winterfield-Tawas complex, 0 to 2 percent slopes, frequently floodedAusaaA2883404452317s5mi02919701:15840
Ausable-Winterfield-Tawas complex, 0 to 2 percent slopes, frequently floodedAusaaA1263404461317s5mi03119881:15840
Ausable-Bowstring mucks, frequently flooded2324241896956cd6mi03919931:15840
Ausable-Winterfield-Tawas complex, 0 to 2 percent slopes, frequently floodedAusaaA10363404454317s5mi04719681:20000
Ausable, frequently flooded-Tawas complex, 0 to 1 percent slopes42349914559441kw0ymi05320071:24000
Ausable, frequently flooded-Tawas complex, 0 to 1 percent slopes804230324833872pc58mi06119891:20000
Ausable, frequently flooded-Tawas complex, 0 to 1 percent slopes42118924525342nb20mi07119921:20000
Ausable-Bowstring mucks, frequently flooded2395661906406dcpmi07919981:12000
Ausable muck, frequently flooded876301907226dgbmi07919981:12000
Ausable muck, frequently flooded8739961923436g4mmi11919971:12000
Thunderbay, Colonville, and Ausable soils, 0 to 2 percent slopes, frequently floodedThuabA37340445931b26mi12919871:15840
Ausable, frequently flooded-Tawas complex, 0 to 1 percent slopes804265616745031t6g7mi13120071:24000
Ausable-Bowstring mucks, frequently flooded23316241387835pmi13520031:12000
Ausable muck, frequently flooded87186241422836tmi13520031:12000
Ausable-Bowstring mucks, frequently flooded2330871914616f75mi13719981:12000
Ausable muck, frequently flooded8715581910366dsgmi14319991:12000
Ausable-Bowstring mucks, frequently flooded231271909726dqdmi14319991:12000
Ausable, Deford, and Tawas mucks, frequently flooded651720014570231kx4rmi15320071:24000
Totagatic-Bowstring-Ausable complex, 0 to 2 percent slopes, frequently flooded3A236114740017hyxwi00720051:12000
Totagatic-Bowstring-Ausable complex, 0 to 2 percent slopes, frequently flooded3A5891816923wf2cwi01320041:12000
Totagatic-Bowstring-Ausable complex, 0 to 2 percent slopes, frequently flooded3A274313859931hj7gwi03120051:12000
Totagatic-Bowstring-Ausable complex, 0 to 2 percent slopes, frequently flooded3A154416883061tnthwi05120061:12000
Totagatic-Bowstring-Ausable complex, 0 to 2 percent slopes, frequently flooded3A69324276962mh6swi09519781:15840
Fordum-Ausable complex, 0 to 2 percent slopes, frequently flooded5555A17124276972mh6twi09519781:15840
Totagatic-Bowstring-Ausable complex, 0 to 2 percent slopes, frequently flooded3A628625335nzq3wi11320061:12000
Totagatic-Bowstring-Ausable complex, 0 to 2 percent slopes, frequently flooded3A3257449064h28ywi12920021:12000

Map of Series Extent

Approximate geographic distribution of the AUSABLE 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 .