Official Series Description


Lab Data Summary

Aggregate lab data for the BASTSIL soil series. This aggregation is based on all pedons with a current taxon name of BASTSIL, 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 BASTSIL 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
86A40A4657S1975TX113003BASTSIL6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.6121025,-96.671669

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BASTSIL 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 BASTSIL 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 BASTSIL 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 BASTSIL 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 BASTSIL 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 BASTSIL series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the BASTSIL 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

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 BASTSIL, 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-2010-11-03-23 | Hamilton County - 2007

    Pattern of soils and underlying material in the Minwells-Bastsil and Bosque-Frio-Venus general soil map units (Soil Survey of Hamilton County, Texas; 2007).

  2. TX-2010-11-03-41 | Jack County - 2005

    Typical pattern of soils and underlying material in the Exray-Truce-Bonti general soil map unit (Soil Survey of Jack County, Texas; 2005).

  3. TX-2010-11-04-05 | McLennan County - 2001

    Pattern of soils in the Weswood-Yahola-Ships general soil map unit (Soil Survey of McLennan County, Texas; 2001).

  4. TX-2012-03-20-29 | Coryell County - May 1985

    Typical pattern of soils in the Bosque-Frio-Lewisville map unit and the Bastsil-Minwells map unit (Soil Survey of Coryell County, TX; 1985).

  5. TX-2012-03-22-21 | Wise County - May 1989

    Typical pattern of the Bastsil-Silawa and the Pulexas-Balsora-Deleon general soil map units (Soil Survey of Wise County, TX; 1989).

Map Units

Map units containing BASTSIL 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
Bastsil fine sandy loam, 0 to 2 percent slopesBaA12013910702vtj2tx02719721:24000
Bastsil fine sandy loam, 2 to 5 percent slopes, moderately erodedBsC244932211802xmf4tx03519771:24000
Bastsil fine sandy loam, 1 to 3 percent slopesBsB37132211792xmf2tx03519771:24000
Bastsil fine sandy loam, 3 to 5 percent slopesBsC32432211732xmf0tx03519771:24000
Bastsil loamy fine sand, 1 to 3 percent slopesBtB14432211772xmf7tx03519771:24000
Bastsil fine sandy loam, 0 to 1 percent slopesBsA2432211782xmdytx03519771:24000
Bastsil fine sandy loam, 1 to 5 percent slopes963713639182xmf1tx07719771:24000
Bastsil loamy fine sand, 1 to 5 percent slopes1724363638682xmf8tx07719771:24000
Bastsil loamy fine sand, 1 to 3 percent slopesBtB1932211812xmf7tx09319741:20000
Bastsil fine sandy loam, 1 to 3 percent slopesBaB59943911432xmf2tx09919831:24000
Bastsil-Urban land complex, 0 to 2 percent slopes1542053647952vv53tx11319751:20000
Bastsil fine sandy loam, 0 to 2 percent slopes1414563647942vtj2tx11319751:20000
Bastsil fine sandy loam, 0 to 3 percent slopes936553650422xmdztx12119751:24000
Bastsil fine sandy loam, 3 to 5 percent slopes109503649592xmf0tx12119751:24000
Bastsil fine sandy loam, 1 to 3 percent slopesBsB67732211902xmf2tx13319721:20000
Bastsil loamy fine sand, 1 to 3 percent slopesBtB1332211892xmf7tx13319721:20000
Bastsil fine sandy loam, 2 to 5 percent slopes, moderately erodedBsC2332211912xmf4tx13319721:20000
Bastsil fine sandy loam, 1 to 3 percent slopesBsB68083653662xmf2tx14319661:20000
Bastsil fine sandy loam, 3 to 5 percent slopesBsC19713653672xmf0tx14319661:20000
Bastsil fine sandy loam, 2 to 5 percent slopes, moderately erodedBsC2153532212102xmf4tx14319661:20000
Bastsil loamy fine sand, 1 to 3 percent slopesBtB65532212092xmf7tx14319661:20000
Bastsil fine sandy loam, 0 to 1 percent slopesBsA6013653652xmdytx14319661:20000
Bastsil loamy fine sand, 1 to 3 percent slopesBaB22363766432xmf7tx19319941:24000
Bastsil fine sandy loam, 2 to 5 percent slopes, moderately erodedBaC29853766442xmf4tx19319941:24000
Bastsil fine sandy loam, 3 to 5 percent slopesBsC31132212192xmf0tx19319941:24000
Bastsil fine sandy loam, 1 to 3 percent slopesBsB6132212182xmf2tx19319941:24000
Bastsil loamy fine sand, 0 to 3 percent slopes1394293677242xmf6tx21719751:20000
Bastsil fine sandy loam, 1 to 3 percent slopes1418633677252vv52tx21719751:20000
Bastsil fine sandy loam, 1 to 5 percent slopesBaC234283680282xmf1tx23719921:24000
Bastsil loamy fine sand, 1 to 5 percent slopesBslBC21031804472xmf8tx23719921:24000
Bastsil loamy fine sand, 1 to 5 percent slopesBaB9473688442xmf8tx28119901:24000
Bastsil fine sandy loam, 0 to 2 percent slopesBaA67783700752vtj2tx30919921:24000
Bastsil-Urban land complex, 0 to 2 percent slopesBaB22373700762vv53tx30919921:24000
Bastsil fine sandy loam, 0 to 2 percent slopesBaA7013706582vtj2tx33119881:24000
Bastsil loamy fine sand, 1 to 3 percent slopesBtB207032212372xmf7tx36719731:20000
Bastsil fine sandy loam, 3 to 5 percent slopesBsC34632212382xmf0tx36719731:20000
Bastsil-Urban land complex, 0 to 5 percent slopesBfC87703723542xmf3tx43919791:20000
Bastsil fine sandy loam, 0 to 3 percent slopesBfB60343724402xmdztx43919791:20000
Bastsil fine sandy loam, 0 to 3 percent slopesBfB150613736482xmdztx49719841:20000
Bastsil loamy fine sand, 0 to 3 percent slopesBdB66183736472xmf5tx49719841:20000
Bastsil fine sandy loam, 1 to 3 percent slopesBsB68432212732xmf2tx60919751:20000
Bastsil loamy fine sand, 1 to 3 percent slopesBtB52432212722xmf7tx60919751:20000
Bastsil fine sandy loam, 3 to 5 percent slopesBsC13032212822xmf0tx60919751:20000
Bastsil fine sandy loam, 2 to 5 percent slopes, moderately erodedBsC22632212742xmf4tx60919751:20000

Map of Series Extent

Approximate geographic distribution of the BASTSIL 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 .