Official Series Description


Lab Data Summary

Aggregate lab data for the AUSTIN soil series. This aggregation is based on all pedons with a current taxon name of AUSTIN, 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 AUSTIN 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
86AS08TX027-005S08TX027005Austin5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.9177246,-97.4700928
86A09N0993S09TX3090011Austin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.8258858,-97.0807648
86A40A4535S1962TX309001AUSTIN6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.4083328,-97.1999969
86A40A4536S1962TX309002AUSTIN6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.3999996,-97.1944427
86AS78TX041006S78TX027006Austin2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.0450001,-97.3644409

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the AUSTIN 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 AUSTIN 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 AUSTIN 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 AUSTIN 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with AUSTIN 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 AUSTIN 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 AUSTIN 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 AUSTIN, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. TX-2010-11-03-01 | Fannin County - 2001

    Pattern of soils and parent material in the Fairlie-Dalco general soil map unit (Soil Survey of Fannin County, Texas; 2001).

  2. TX-2010-11-03-03 | Fannin County - 2001

    Pattern of soils and parent material in the Whitewright-Howe general soil map unit (Soil Survey of Fannin County, Texas; 2001).

  3. TX-2012-03-20-41 | Ellis County - August 1964

    Block diagram showing relation of eight soil associations in Ellis County to the underlying materials and surface relief (Soil Survey of Ellis County, TX; 1964).

  4. TX-2012-03-20-43 | Ellis County - August 1964

    Representative pattern of soils in soil association 2. Ellis and Houston clays occupy the more sloping areas; Houston Black clay occupies the nearly level areas (Soil Survey of Ellis County, TX; 1964).

  5. TX-2012-03-20-44 | Ellis County - August 1964

    Relation of soils in soil association 4 to the underlying chalky bedrock. Eddy soils and Stephen silty clay soils are in soil association 4 (Soil Survey of Ellis County, TX; 1964).

  6. TX-2012-03-20-45 | Ellis County - August 1964

    Geographical association of soils on sloping and gently sloping blackland. Austin silty clay and Houston Black clay soils are in soil association 5 (Soil Survey of Ellis County, TX; 1964).

  7. TX-2012-03-22-14 | Williamson County - January 1983

    Typical landscape pattern of the Austin-Houston Black-Castephen general soil map unit (Soil Survey of Williamson County, TX; 1983).

Map Units

Map units containing AUSTIN 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
Austin silty clay, 1 to 3 percent slopesAsB191433910662vtgjtx02719721:24000
Austin silty clay, 2 to 5 percent slopes, moderately erodedAsC189133910672vtgktx02719721:24000
Austin-Urban land complex, 2 to 5 percent slopesAuC30073910682sshctx02719721:24000
Austin-Whitewright complex, 2 to 6 percent slopes, erodedAwD363731300342s1qttx02719721:24000
Austin silty clay, 0 to 1 percent slopesAsA38631300332s1qstx02719721:24000
Whitewright-Austin complex, 1 to 5 percent slopesBsC9172390452f397tx02920001:24000
Austin silty clay, 2 to 5 percent slopes, moderately erodedAuC84803904482vtgktx02920001:24000
Austin silty clay, 1 to 3 percent slopesAuB80033904472vtgjtx02920001:24000
Austin silty clay, 2 to 5 percent slopes, moderately erodedAuC2320053640572vtgktx08519651:20000
Austin silty clay, 1 to 3 percent slopesAuB255253640562vtgjtx08519651:20000
Austin silty clay, 5 to 8 percent slopes, moderately erodedAuD2134973640582vv4vtx08519651:20000
Austin-Urban land complex, 0 to 2 percent slopes819293364866d7nwtx11319751:20000
Austin silty clay, 1 to 3 percent slopes5164323648332vtgjtx11319751:20000
Austin-Urban land complex, 2 to 5 percent slopes9127003648682sshctx11319751:20000
Austin-Lewisville complex, 5 to 8 percent slopes, erode d73965364855d7njtx11319751:20000
Austin silty clay, 2 to 5 percent slopes, moderately eroded638713648442vtgktx11319751:20000
Austin silty clay, 1 to 3 percent slopesAuB426443652752vtgjtx13919621:20000
Austin silty clay, 2 to 5 percent slopes, moderately erodedAuC2152303652762vtgktx13919621:20000
Austin silty clay, 5 to 8 percent slopes, moderately erodedAuD229563652772vv4vtx13919621:20000
Whitewright and Austin soils, 2 to 5 percent slopes erodedBkC2742365280d837tx13919621:20000
Austin silty clay, 1 to 3 percent slopes518223654702vtgjtx14519751:20000
Austin silty clay, 2 to 5 percent slopes, moderately eroded616453654812vtgktx14519751:20000
Austin silty clay loam, 1 to 3 percent slopesAuB6130365497d8b7tx14719891:24000
Austin silty clay, 2 to 5 percent slopes, moderately eroded9161423667232vtgktx18119771:20000
Austin silty clay, 1 to 3 percent slopes8128943667202vtgjtx18119771:20000
Austin-Urban land complex, 2 to 5 percent slopes1018583666442sshctx18119771:20000
Austin silty clay, 1 to 3 percent slopesAuB19853668352vtgjtx18719731:20000
Austin silty clay, 2 to 5 percent slopes, moderately erodedAuC318813668362vtgktx18719731:20000
Austin silty clay, 1 to 3 percent slopes7103603677862vtgjtx21719751:20000
Austin silty clay, 2 to 5 percent slopes, moderately eroded859803677972vtgktx21719751:20000
Austin silty clay, 1 to 3 percent slopesAsB78323700722vtgjtx30919921:24000
Austin-Urban land complex, 1 to 3 percent slopesAuC5141370073df2vtx30919921:24000
Austin silty clay, 1 to 5 percent slopesAuC14283705352vv4stx32519721:24000
Austin silty clay, 1 to 3 percent slopesAuB6137371427dghjtx38719721:24000
Urban land, Austin, and Whitewright soils, 1 to 8 percent slopesUtD9910393255f66ntx45319691:20000
Austin-Urban land complex, 2 to 5 percent slopesUsC80313932542sshctx45319691:20000
Austin silty clay, 2 to 5 percent slopes, moderately erodedAsC274143921582vtgktx45319691:20000
Austin silty clay, 1 to 3 percent slopesAsB64153921572vtgjtx45319691:20000
Austin-Whitewright complex, 3 to 5 percent slopes, moderately erodedAtC23300392159f529tx45319691:20000
Austin-Whitewright complex, 5 to 8 percent slopes, moderately erodedAtD21198392160f52btx45319691:20000
Austin silty clay, 1 to 3 percent slopesAsB257163735182vtgjtx49119811:20000
Austin-Whitewright complex, 2 to 6 percent slopes, erodedAwD3189413735192s1qttx49119811:20000
Austin silty clay, 0 to 1 percent slopesAsA8443735172s1qstx49119811:20000
Austin-Castephen complex, 1 to 3 percent slopesAuB2924378702dq26tx60419811:20000
Austin-Castephen complex, 2 to 5 percent slopes, erodedAuC3696378703dq27tx60419811:20000
Austin silty clay, 1 to 3 percent slopes46448393334f696tx61419751:20000

Map of Series Extent

Approximate geographic distribution of the AUSTIN 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 .