Official Series Description


Lab Data Summary

Aggregate lab data for the BRAZORIA soil series. This aggregation is based on all pedons with a current taxon name of BRAZORIA, 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 BRAZORIA 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
150A10N0974S10TX1573010Brazoria8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.5088882,-95.6299438
150A40A4673S1976TX039005Brazoria5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.3494453,-95.5561142
150A10N0975S2010TX1573011Brazoria8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.5088882,-95.6298904
150A11N0445S2010TX6002761Brazoria8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.8255005,-96.0138626
150A11N0446S2010TX6003681Brazoria8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.8254833,-96.0138611

Water Balance

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

Click the image to view it full size.

Geomorphic description summaries for the BRAZORIA 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 BRAZORIA, 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-2010-11-02-32 | Colorado County - 2006

    Pattern of soils and underlying material in the Norwood-Brazoria-Mohat general soil map unit (Soil Survey of Colorado County, Texas; 2006).

  2. TX-2010-11-04-02 | Matagorda County - 2001

    Typical pattern of soils and underlying material in the Brazoria-Norwood-Clemville general soil map unit (Soil Survey of Matagorda County, Texas; 2001).

  3. TX-2012-03-19-16 | Austin and Waller Counties - March 1984

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

Map Units

Map units containing BRAZORIA 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
Brazoria clay, 0 to 1 percent slopes, rarely flooded10422683630412v39ctx03919791:20000
Brazoria clay, 1 to 3 percent slopes, rarely flooded1123293630422v3cmtx03919791:20000
Brazoria clay, 0 to 1 percent slopes, rarely floodedBrA81383642562v39ctx08919971:24000
Brazoria clay, 0 to 1 percent slopes, rarely floodedMa638153659482v39ctx15719561:20000
Brazoria rarely flooded-Sumpf frequently flooded, occasionally ponded clayMe693365952d8sxtx15719561:20000
Brazoria clay, 0 to 1 percent slopes, rarely floodedBoA3994366739d9m9tx18519881:24000
Brazoria clay, depressional, occasionally flooded, occasionally pondedBp1462366741d9mctx18519881:24000
Brazoria clay, 1 to 3 percent slopes, rarely floodedBoB1000366740d9mbtx18519881:24000
Brazoria clay, 0 to 1 percent slopes, rarely floodedBr332593704932v39ctx32119911:24000
Brazoria clay, 0 to 1 percent slopes, rarely flooded910437373206djbxtx47719791:24000
Brazoria clay, 1 to 3 percent slopes, rarely flooded101510373136dj8ntx47719791:24000
Brazoria clay, 0 to 1 percent slopes, rarely floodedMe551423732622v39ctx48119681:20000
Brazoria clay, 0 to 1 percent slopes, rarely floodedBrA386013738152v39ctx60019811:24000
Brazoria clay, 1 to 3 percent slopes, rarely floodedBrB26483738162v3cmtx60019811:24000

Map of Series Extent

Approximate geographic distribution of the BRAZORIA 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 .