Official Series Description


Lab Data Summary

Aggregate lab data for the BLANKET soil series. This aggregation is based on all pedons with a current taxon name of BLANKET, 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 BLANKET 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
84B40A461172TX143001Blanket5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.503334,-98.1374969
8596P031296TX143013Blanket7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.1171684,-98.15522

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BLANKET 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 BLANKET 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 BLANKET 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 BLANKET 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 BLANKET 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 BLANKET 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 BLANKET 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.

Click the image to view it full size.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with BLANKET, 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-2012-03-22-23 | Wise County - May 1989

    Typical pattern of the Venus-Aledo-Somervell general soil map unit (Soil Survey of Wise County, TX; 1989).

Map Units

Map units containing BLANKET 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
Blanket silt loam, 1 to 3 percent slopes6323989313824592wtvfks00719731:24000
Blanket silt loam, 0 to 1 percent slopes6322399713824582wtvcks00719731:24000
Blanket silty clay loam, 1 to 3 percent slopes, eroded6324195213824602wtvgks00719731:24000
Blanket silt loam, 1 to 3 percent slopes632340513812392wtvfks03319871:24000
Blanket silty clay loam, 1 to 3 percent slopes, eroded63241413812402wtvgks03319871:24000
Blanket silt loam, 1 to 3 percent slopes6323940114448242wtvfks09519771:24000
Blanket silt loam, 0 to 1 percent slopes6322689314448232wtvcks09519771:24000
Blanket silty clay loam, 1 to 3 percent slopes, eroded6324105914448252wtvgks09519771:24000
Blanket silt loam, 1 to 3 percent slopes63231113804882wtvfks09719831:24000
Blanket silty clay loam, 1 to 3 percent slopes, eroded6324613804892wtvgks09719831:24000
Blanket silt loam, 1 to 3 percent slopes63233272914451812wtvfks15119651:24000
Blanket silt loam, 0 to 1 percent slopes63222297314451802wtvcks15119651:24000
Blanket silty clay loam, 1 to 3 percent slopes, eroded6324882714451822wtvgks15119651:24000
Blanket silt loam, 0 to 1 percent slopes63224983814440112wtvcks17319761:24000
Blanket silt loam, 1 to 3 percent slopes63234640714440122wtvfks17319761:24000
Blanket silt loam, 0 to 1 percent slopes6322542914436802wtvcks18519751:24000
Blanket loam, 1 to 3 percent slopesBlalB64873643482y2srtx09319741:20000
Blanket loam, 0 to 1 percent slopesBlalA38413643472y2sstx09319741:20000
Blanket clay loam, 1 to 3 percent slopesBaB103623653492tc1ktx14319661:20000
Blanket clay loam, 0 to 1 percent slopesBaA15103653482tc1jtx14319661:20000
Blanket clay loam, 1 to 5 percent slopes, severely erodedBlaC31543653502zh6stx14319661:20000
Owens-Blanket association, undulatingOBC3248369956ddz2tx30719701:24000
Blanket clay loam, 1 to 3 percent slopesBlB20483699322tc1ktx30719701:24000
Blanket clay loam, 0 to 1 percent slopesBbA24713909362tc1jtx36319791:24000
Blanket clay loam, 1 to 3 percent slopesBbB36523908572tc1ktx36719731:20000
Blanket clay loam, 1 to 3 percent slopesBkB18003736492tc1ktx49719841:20000
Blanket clay loam, 1 to 3 percent slopesBbB33463743782tc1ktx60919751:20000

Map of Series Extent

Approximate geographic distribution of the BLANKET 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 .