Official Series Description


Lab Data Summary

Aggregate lab data for the BURLESON soil series. This aggregation is based on all pedons with a current taxon name of BURLESON, 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 BURLESON 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
84B76-OK-48-176-OK095-48-1Burleson4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.0053139,-96.79415
84B76-OK-48-276-OK095-48-2Burleson4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.0052917,-96.7939389
87A78P000577TX051005Burleson4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.4916668,-96.476387
87A96P025496TX051002Burleson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.4893341,-96.4790802
87A96P025596TX051003Burleson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.4893341,-96.4790802
87A40A4578S1963TX051090Burleson3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.4913883,-96.4505539
n/a40A0250S1962TX085003Burleson8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A4577S1962TX085004Burleson6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aS89TX051004S89TX051004Burleson6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BURLESON 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 BURLESON 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 BURLESON 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 BURLESON 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 BURLESON 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 BURLESON 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 BURLESON 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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Click the image to view it full size.

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with BURLESON, 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-2010-11-02-10 | Brazos County - 2002

    Pattern of soils and underlying material on the flood plain along the Brazos River and on adjacent terraces. Included are the Burleson-Wilson, Ships, and Weswood general soil map units (Soil Survey of Brazos County, Texas; 2002).

  2. TX-2010-11-02-19 | Burleson County - 2005

    Typical pattern of soils in the Ships-Belk and Burleson general soil map units (Soil Survey of Burleson County, Texas; 2005).

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

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

  4. TX-2010-11-04-09 | Milam County - 2004

    Typical pattern of soils and underlying material in the Branyon-Burleson general soil map unit (Soil Survey of Milam County, Texas; 2004).

  5. TX-2012-03-20-42 | Ellis County - August 1964

    Geographical association of soils on benches. Burleson clay, terrace; Houston Black clay, terrace; and Lewisville soils are in soil association 1 (Soil Survey of Ellis County, TX; 1964).

  6. TX-2012-03-21-33 | Leon County - July 1989

    The Gladewater, Kaufman, and Nahatche soils are dominant on the terraces and flood plains of the Trinity River system (Soil Survey of Leon County, TX; 1989).

  7. TX-2012-03-21-53 | Navarro County - December 1974

    Typical pattern of soils in the Wilson-Burleson association (Soil Survey of Navarro County, TX; 1974).

  8. TX-2012-03-22-11 | Williamson County - January 1983

    Typical landscape pattern of the Branyon-Houston Black-Burleson general soil map unit (Soil Survey of Williamson County, TX; 1983).

Map Units

Map units containing BURLESON 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
Burleson clay, 1 to 3 percent slopes195343571331m5j1ok00519771:24000
Burleson clay, 0 to 1 percent slopes1811095713302ssg6ok00519771:24000
Burleson clay, 1 to 3 percent slopes16195293817952tbtxok01319741:24000
Burleson clay, 0 to 1 percent slopes1566133817942ssg6ok01319741:24000
Burleson clay, 3 to 5 percent slopes1743303817962ssg9ok01319741:24000
Burleson clay, 0 to 1 percent slopes4194538202430mz7ok01919771:24000
Burleson clay, 1 to 3 percent slopes1210515712012tbtxok02319771:24000
Burleson clay, 0 to 1 percent slopesBuA2333571586m5s8ok02919691:24000
Burleson clay, 1 to 3 percent slopesBuB2254571587m5s9ok02919691:24000
Burleson clay, 1 to 3 percent slopes8117638261530mz8ok04919821:24000
Burleson clay, 1 to 3 percent slopes41219438330430mz8ok06919761:24000
Burleson clay, 0 to 1 percent slopes3198038329330mz7ok06919761:24000
Heiden-Burleson complex, 3 to 5 percent slopesDdC8372383704dw8kok08519631:24000
Burleson clay, 1 to 3 percent slopes38229383905dwh1ok09519781:24000
Burleson clay, 1 to 3 percent slopes6423538396830mz8ok09919821:24000
Burleson clay, 1 to 3 percent slopesBuB374338460330mz8ok12319671:24000
Burleson clay, 0 to 1 percent slopesBu10415751242ssg6tx00119701:20000
Burleson clay, 1 to 3 percent slopesBuB12453932782tbtxtx02119721:24000
Burleson clay, 0 to 1 percent slopesBuA38803910782ssg6tx02719721:24000
Wilson-Burleson complex, 0 to 1 percent slopesWnbA280731300392s1rytx02719721:24000
Wilson-Burleson complex, 1 to 3 percent slopesWnbB238931300662s1rztx02719721:24000
Burleson clay, 1 to 3 percent slopesBuB13923910792tbtxtx02719721:24000
Burleson clay, 1 to 3 percent slopes, gravellyBugB29631300382s1qrtx02719721:24000
Burleson clay, 0 to 1 percent slopesBuA30313631802ssg6tx04119931:20000
Burleson clay, 1 to 3 percent slopesBuB23093631812tbtxtx04119931:20000
Burleson clay, 3 to 5 percent slopesBuC8723631822ssg9tx04119931:20000
Burleson clay, 0 to 1 percent slopesBuA44303634302ssg6tx05119941:24000
Burleson clay, 1 to 3 percent slopesBuB11713634312tbtxtx05119941:24000
Burleson clay, 3 to 5 percent slopesBuC4423634322ssg9tx05119941:24000
Burleson clay, 1 to 3 percent slopesBuB57283634972tbtxtx05519721:20000
Burleson clay, 0 to 1 percent slopesBuA18133634962ssg6tx05519721:20000
Burleson clay, 1 to 3 percent slopesBcB114533640602tbtxtx08519651:20000
Burleson clay, 0 to 1 percent slopesBcA44483640592ssg6tx08519651:20000
Burleson clay, 0 to 1 percent slopesBuA29963642582ssg6tx08919971:24000
Burleson clay, 1 to 3 percent slopesBuB2373642592tbtxtx08919971:24000
Burleson clay, 0 to 1 percent slopes1858813647982ssg6tx11319751:20000
Burleson clay, 1 to 3 percent slopes1948493647992tbtxtx11319751:20000
Burleson clay, 1 to 3 percent slopes22136223649722tbtxtx12119751:24000
Burleson clay, 0 to 1 percent slopes2185973649712ssg6tx12119751:24000
Burleson clay, 0 to 1 percent slopesBuA99113652842ssg6tx13919621:20000
Burleson clay, 1 to 3 percent slopesBtB45733652832tbtxtx13919621:20000
Burleson clay, depressionalBy323365286d83ftx13919621:20000
Burleson clay, 0 to 1 percent slopes16110143654332ssg6tx14519751:20000
Burleson clay, 1 to 3 percent slopes1726093654342tbtxtx14519751:20000
Burleson clay, 0 to 1 percent slopesBuA41423655052ssg6tx14719891:24000
Burleson clay, 0 to 1 percent slopesBuA15613656922ssg6tx14919911:24000
Burleson clay, 0 to 1 percent slopesBuA5933753732ssg6tx16119861:24000
Burleson clay, 0 to 1 percent slopesBsA13533667432ssg6tx18519881:24000
Burleson gravelly clay, 1 to 3 percent slopesByB21493668442ssgbtx18719731:20000
Burleson gravelly clay, 0 to 1 percent slopesByA1106366843d9qntx18719731:20000
Burleson clay, 0 to 1 percent slopesBuA7613668422ssg6tx18719731:20000
Burleson clay, 0 to 1 percent slopes519493676392ssg6tx21319781:20000
Burleson clay, 0 to 1 percent slopes2233553677342ssg6tx21719751:20000
Wilson-Burleson complex, 0 to 1 percent slopes813116367799dbqhtx21719751:20000
Burleson clay, 1 to 3 percent slopes2310223677352tbtxtx21719751:20000
Burleson clay, 0 to 1 percent slopes587093678972ssg6tx23119781:24000
Burleson clay, 0 to 1 percent slopesBuA15493681552ssg6tx25119811:20000
Burleson clay, 1 to 3 percent slopesBuB13763681562tbtxtx25119811:20000
Burleson clay, 0 to 1 percent slopesBuA15943691762ssg6tx28919851:24000
Burleson clay, 1 to 3 percent slopesBuB10883691772tbtxtx28919851:24000
Burleson clay, 0 to 2 percent slopesBuA61083693852ssg7tx29319911:24000
Burleson clay, 0 to 1 percent slopesBuA124503700822ssg6tx30919921:24000
Burleson clay, 0 to 1 percent slopesBuA13143702732ssg6tx31319891:24000
Burleson clay, 0 to 2 percent slopesBurA157603706642ssg7tx33119881:24000
Burleson clay, 0 to 1 percent slopesBuA163231300712ssg6tx33119881:24000
Burleson clay, 1 to 3 percent slopesBuB68031300722tbtxtx33119881:24000
Wilson-Burleson complex, 0 to 1 percent slopesWnbA39431300732s1rytx33119881:24000
Wilson-Burleson complex, 1 to 3 percent slopesWnbB25031300962s1rztx33119881:24000
Burleson clay, 1 to 3 percent slopesBu21225755722tbtxtx33919671:20000
Burleson clay, 0 to 1 percent slopesBuA226163709172ssg6tx34919681:24000
Burleson clay, 1 to 3 percent slopesBuB146563709182tbtxtx34919681:24000
Burleson clay, 1 to 3 percent slopesBuB259653714312tbtxtx38719721:24000
Burleson clay, 0 to 1 percent slopesBuA23343714302ssg6tx38719721:24000
Burleson clay, 0 to 1 percent slopesBuA10663716972ssg6tx39519961:24000
Burleson clay, 0 to 1 percent slopesBuA12323723632ssg6tx43919791:20000
Burleson gravelly clay, 1 to 3 percent slopesBtB34263921722ssgbtx45319691:20000
Burleson gravelly clay, 3 to 5 percent slopesBtC2916392173f52rtx45319691:20000
Burleson clay, 1 to 3 percent slopesBsB26183921712tbtxtx45319691:20000
Burleson clay, 0 to 1 percent slopesBsA9613921702ssg6tx45319691:20000
Burleson clay, 0 to 1 percent slopes125403731382ssg6tx47719791:24000
Burleson clay, 1 to 3 percent slopes134723731392tbtxtx47719791:24000
Burleson clay, 0 to 1 percent slopesBuA183203735292ssg6tx49119811:20000
Burleson clay, 1 to 3 percent slopesBuB36203735302tbtxtx49119811:20000
Wilson-Burleson complex, 1 to 3 percent slopesWnbB157631301302s1rztx49119811:20000
Wilson-Burleson complex, 0 to 1 percent slopesWnbA106631301052s1rytx49119811:20000
Burleson clay, 1 to 3 percent slopes, gravellyBugB21431301042s1qrtx49119811:20000
Burleson clay, 0 to 1 percent slopesBuA29753738192ssg6tx60019811:24000
Burleson clay, 1 to 3 percent slopesBuB228743744662tbtxtx61219731:20000
Burleson clay, 0 to 1 percent slopesBuA87863744652ssg6tx61219731:20000
Burleson clay, 0 to 1 percent slopes850383933382ssg6tx61419751:20000

Map of Series Extent

Approximate geographic distribution of the BURLESON 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 .