Official Series Description


Lab Data Summary

Aggregate lab data for the BEAUMONT soil series. This aggregation is based on all pedons with a current taxon name of BEAUMONT, 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 BEAUMONT 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
150A40A456255TX071091Beaumont3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.7875004,-94.913887
150A40A024859TX245001Beaumont6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.9705556,-94.1038889
150A40A456159TX245002Beaumont6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.9536111,-94.1186111
150A91P003090TX245021Beaumont7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.9774972,-94.3305556
150A40A4560S1955TX071090Beaumont3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.7357998,-94.3890991
150A12N7635S2012TX0711005Beaumont7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.8169583,-94.4339667
150A12N7636S2012TX0711006Beaumont7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.8174417,-94.4341694
150A12N7959S2012TX2911015Beaumont7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.9454,-94.4856389

Water Balance

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

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

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Competing Series

Soil series competing with BEAUMONT 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 BEAUMONT 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 BEAUMONT 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 BEAUMONT, 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-2010-11-03-27 | Hardin County - 2006

    Pattern of soils and underlying material in the Aris-League-Labelle general soil map unit (Soil Survey of Hardin County, Texas; 2006).

  2. TX-2012-03-21-11 | Jefferson County - February 1965

    Relative position of the major soils of the coast prairie and coast marsh (Soil Survey of Jefferson County, TX; 1965).

Map Units

Map units containing BEAUMONT 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
Beaumont clay, 0 to 1 percent slopesBeaA251523637832pfj7tx07119691:24000
Beaumont silty clay, 0 to 1 percent slopes, rarely floodedBebA2459827607332sycvtx07119691:24000
Beaumont-Urban land complex, 0 to 1 percent slopesBecA53327607342thnbtx07119691:24000
Beaumont clay, 0 to 1 percent slopesBeaA53003796692pfj7tx19919981:24000
Beaumont clay, 0 to 1 percent slopesBeaA166083673712pfj7tx20119731:20000
Beaumont-Urban land complex, 0 to 1 percent slopesBecA597328882392thnbtx20119731:20000
Beaumont clay, 0 to 1 percent slopesBeaA548193692532pfj7tx29119861:24000
Beaumont clay, 0 to 1 percent slopesBeaA326113748812pfj7tx62319961:24000
Beaumont silty clay, 0 to 1 percent slopes, rarely floodedBebA1890928885272sycvtx62319961:24000
Beaumont-Urban land complex, 0 to 1 percent slopesBecA32128885282thnbtx62319961:24000

Map of Series Extent

Approximate geographic distribution of the BEAUMONT 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 .