Official Series Description


Lab Data Summary

Aggregate lab data for the BRACKETT soil series. This aggregation is based on all pedons with a current taxon name of BRACKETT, 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 BRACKETT 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
81C87P005286TX053001Brackett7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.9861107,-98.1422195
81C12N7661S11TX209001Brackett7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.1130562,-98.1412201
85S99TX099003S99TX099003Brackett5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.3534775,-97.7651825

Water Balance

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

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 BRACKETT, 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-2010-11-03-51 | Lampasas County - 1991

    Typical pattern of soils and underlying material in the Sunev-Rumley-Oakalla general soil map unit (Soil Survey of Lampasas County, Texas; 1991).

  2. TX-2010-11-03-52 | Lampasas County - 1991

    Typical pattern of soils and underlying material in the Brackett-Lampasas general soil map unit (Soil Survey of Lampasas County, Texas; 1991).

  3. TX-2010-11-03-75 | Mason County -

  4. 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).

  5. TX-2012-03-20-21 | Comal and Hays Counties - June 1984

    Pattern of soils in the Brackett-Comfort-Real general soil map unit (Soil Survey of Comal and Hays Counties, TX; 1984).

  6. TX-2012-03-20-26 | Coryell County - May 1985

    Typical pattern of soils in the Eckrant-Real-Rock outcrop map unit and the Slidell-Topsey-Brackett map unit (Soil Survey of Coryell County, TX; 1985).

  7. TX-2012-03-21-17 | Johnson County - October 1985

    Typical pattern of soils and parent material in the Aledo-Bolar map unit (Soil Survey of Johnson County, TX; 1985).

  8. TX-2012-03-21-43 | McCulloch County - November 1974

    Pattern of soils in Tarrant-Kavett association (Soil Survey of McCulloch County, TX; 1974).

  9. TX-2012-03-21-50 | Menard County - February 1967

    Soils of the Knippa-Uvalde soil association (Soil Survey of Menard County, TX; 1967).

  10. 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 BRACKETT 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
Brackett loam, 5 to 20 percent slopes25652383282dvtyok06919761:24000
Brackett loam, 8 to 12 percent slopesBKE1557339107530ytztx02719721:24000
Brackett gravelly clay loam, 12 to 20 percent slopesBrE238523904512yly2tx02920001:24000
Brackett-Eckrant association, 20 to 60 percent slopesBtE170473904532yly3tx02920001:24000
Brackett gravelly clay loam, 3 to 12 percent slopesBrD109553904502t2m5tx02920001:24000
Brackett-Eckrant association, 8 to 40 percent slopesBtF7852636298430yv4tx03519771:24000
Brackett gravelly clay loam, 1 to 5 percent slopesBtC10813630372szpstx03519771:24000
Hext-Oplin-Brackett association, hilly2012743363594d6bvtx05919791:24000
Brackett-Karnes complex, 1 to 12 percent slopesBsE9536364359d74jtx09319741:20000
Brackett-Bolar complex, 1 to 5 percent slopesBrC6940364358d74htx09319741:20000
Brackett soils, 8 to 30 percent slopesBTF34023643492szpttx09319741:20000
Brackett loam, 8 to 20 percent slopesBtE177736522730yv2tx13319721:20000
Brackett stony loam, 1 to 8 percent slopesBrD1751365226d81htx13319721:20000
Brackett-Purves complexBt25195365356d85ptx14319661:20000
Brackett-Dugout complex, 8 to 40 percent slopesBrF22742365355d85ntx14319661:20000
Brackett-Tarrant association, hillyBtE22790366175d913tx17119701:20000
Brackett soils, hillyBrE15333366174d912tx17119701:20000
Brackett soils, 1 to 8 percent slopesBrC114473661732t26gtx17119701:20000
Brackett-Pidcoke gravelly clay loams, 1 to 5 percent slopesByC2146437665130kndtx19319941:24000
Brackett-Maloterre complex, 2 to 12 percent slopesBxD2061337665030knctx19319941:24000
Brackett gravelly clay loam, 8 to 30 percent slopesBtE11546376649dmxztx19319941:24000
Brackett gravelly clay loam, 1 to 5 percent slopesBtC40373766482szpstx19319941:24000
Brackett-Rock outcrop complex, 5 to 30 percent slopes20525536773230knjtx21719751:20000
Brackett-Rock outcrop complex, 5 to 30 percent slopesBrE705636815430knjtx25119811:20000
Brackett-Real association, 10 to 30 percent slopes5890063684632t271tx25919791:31680
Doss-Brackett association, 1 to 8 percent slopes97297536846730gjstx25919791:31680
Brackett association, 1 to 8 percent slopes4246123684622t26htx25919791:31680
Real-Brackett complex, hillyRbF28998368559dcj0tx26719801:31680
Brackett gravelly clay loam, 3 to 8 percent slopesBrD152609368849dctctx28119901:24000
Brackett-Rock outcrop complex, 10 to 30 percent slopesBrE26265368850dctdtx28119901:24000
Brackett gravelly clay loam, 1 to 5 percent slopesBrC159936884830yv0tx28119901:24000
Brackett-Tarrant association, steepBUE10617369931ddy8tx30719701:24000
Brackett soils, 1 to 8 percent slopesBtC62663699362t26gtx30719701:24000
Brackett loam, 1 to 5 percent slopesBsC4245369935ddydtx30719701:24000
Aledo-Brackett complex, 5 to 20 percent slopesAdE548137007130ytvtx30919921:24000
Kerrville, Brackett, and Tarrant soils, 12 to 40 percent slopes, very rockyKTG10769370410dffqtx31920111:24000
Tarrant-Brackett association, hillyTb22652370615dfnbtx32719651:20000
Brackett soils, 1 to 8 percent slopesBaC28533705972t26gtx32719651:20000
Brackett-Maloterre complex, 2 to 12 percent slopesBsE2636939086730knctx36719731:20000
Brackett-Maloterre soils, 12 to 30 percent slopesBsG438839086830ytxtx36719731:20000
Brackett-Urban land complex, 3 to 12 percent slopesBrE451390866f3qltx36719731:20000
Maloterre, Aledo, and Brackett soils, 3 to 20 percent slopesMaC839537239330knrtx43919791:20000
Brackett clay loam, 3 to 8 percent slopesBrD143337236130yv1tx43919791:20000
Brackett-Rock outcrop complex, 1 to 12 percent slopesBlD1100183921672yltztx45319691:20000
Brackett-Rock outcrop-Real complex, 8 to 30 percent slopesBoF570113921682t2m3tx45319691:20000
Brackett soils and Urban land, 12 to 30 percent slopesBrF32073921692yltytx45319691:20000
Urban land and Brackett soils, 1 to 12 percent slopesUuE2662393256f66ptx45319691:20000
Brackett gravelly clay loam, 3 to 12 percent slopesBkE158733735252t2m5tx49119811:20000
Brackett association, 1 to 8 percent slopesBktD42623735242t26htx49119811:20000
Brackett-Rock outcrop-Real complex, 8 to 30 percent slopesBkrG17603735262t2m3tx49119811:20000
Brackett-Aledo complex, 5 to 20 percent slopesByE1800937365430yv3tx49719841:20000
Brackett association, 1 to 8 percent slopes61701453739422t26htx60119771:31680
Brackett-Real association, 10 to 30 percent slopes71572143739432t271tx60119771:31680
Bolar-Brackett complex, 1 to 8 percent slopes689912391037f3x3tx60219751:24000
Brackett-Tarrant complex, 8 to 30 percent slopes14513539098730knptx60219751:24000
Hext-Brackett complex, 1 to 8 percent slopes374659391012f3w9tx60219751:24000
Brackett gravelly clay loam, 1 to 8 percent slopes13443039098630ytytx60219751:24000
Brackett-Rock outcrop-Comfort complex, 1 to 8 percent slopesBtD1103803787082ylv1tx60419811:20000
Brackett-Rock outcrop-Real complex, 8 to 30 percent slopesBtG1046333787092t2m3tx60419811:20000
Brackett soils, 8 to 30 percent slopesBtF117383743232szpttx60919751:20000

Map of Series Extent

Approximate geographic distribution of the BRACKETT 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 .