Official Series Description


Lab Data Summary

Aggregate lab data for the BOSQUE soil series. This aggregation is based on all pedons with a current taxon name of BOSQUE, 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 BOSQUE 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
86A81P031081TX027002Bosque7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.0047226,-97.3855591

Water Balance

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

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.

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

Competing Series

Soil series competing with BOSQUE 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 BOSQUE 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 BOSQUE 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 BOSQUE, 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-2010-11-04-03 | McLennan County - 2001

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

  3. TX-2012-03-19-17 | Austin and Waller Counties - March 1984

    Pattern of soils in the Frelsburg-Bleiblerville-Latium association (Soil Survey of Austin and Waller Counties, TX; 1984).

  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).

Map Units

Map units containing BOSQUE 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
Bosque loam, 0 to 1 percent slopes, occasionally floodedBo17830393277f67ctx02119721:24000
Bosque clay loam, 0 to 1 percent slopes, occasionally floodedBqA10890391071f3y6tx02719721:24000
Bosque clay loam, 0 to 1 percent slopes, frequently floodedBoA2636391072f3y7tx02719721:24000
Bosque loam, occasionally floodedBo5046363036d5rvtx03519771:24000
Bosque clay loam, occasionally floodedBo2149363491d67jtx05519721:20000
Bosque soils, frequently floodedBp1532363492d67ktx05519721:20000
Bosque clay loam, 0 to 1 percent slopes, occasionally floodedBoA1079364255d715tx08919971:24000
Bosque loam, occasionally floodedBo9289364357d74gtx09319741:20000
Bosque clay loam, 0 to 1 percent slopes, occasionally floodedBs20492391146f40mtx09919831:24000
Bosque clay loam, 0 to 1 percent slopes, rarely floodedBo10009391145f40ltx09919831:24000
Bosque loam, rarely floodedFl534365296d83rtx13919621:20000
Bosque loam, occasionally floodedBo15396365354d85mtx14319661:20000
Bosque sandy clay loam, occasionally floodedBo2288365689d8jftx14919911:24000
Bosque clay loam, 0 to 1 percent slopes, frequently floodedBoA4348366530d9dktx17719971:24000
Bosque-Tinn complex, 0 to 1 percent slopes, frequently floodedBpA15333664902ylmdtx17719971:24000
Bosque and Seguin soils, frequently floodedBo5769366839d9qjtx18719731:20000
Bosque clay loam, occasionally floodedBs15934376647dmxxtx19319941:24000
Bosque clay loam, rarely floodedBo7417376646dmxwtx19319941:24000
Bosque clay loam, occasionally floodedBo2916368031dbyztx23719921:24000
Bosque clay loam, occasionally floodedBh2279370078df30tx30919921:24000
Bosque clay loam, 0 to 1 percent slopes, occasionally floodedBeA22953706612s1qmtx33119881:24000
Bosque loam, occasionally flooded95213370798dfv7tx33719751:24000
Bosque soils, frequently flooded10988370754dfsttx33719751:24000
Bosque clay loam, 0 to 1 percent slopes, occasionally floodedBo15542390940f3sztx36319791:24000
Bosque loam, 0 to 1 percent slopes, occasionally floodedBo3550390865f3qktx36719731:20000
Bosque clay loam, occasionally floodedBy4041372164dh89tx42919851:24000
Bosque clay loam, frequently flooded821041373205djbwtx47719791:24000
Bosque clay loam, frequently floodedBe9062373813djzhtx60019811:24000
Bosque loam, 0 to 1 percent slopes, occasionally flooded129787390985f3vftx60219751:24000
Bosque loam, occasionally floodedBo8010374322dkhxtx60919751:20000

Map of Series Extent

Approximate geographic distribution of the BOSQUE 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 .