Official Series Description


Lab Data Summary

Aggregate lab data for the BRAXTON soil series. This aggregation is based on all pedons with a current taxon name of BRAXTON, 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 BRAXTON were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

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

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

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Competing Series

Soil series competing with BRAXTON 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 BRAXTON 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 BRAXTON 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 BRAXTON, 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. KY-2012-01-27-34 | Clark County - 1964

    Major soil series in soil association 1, their relationship to the landscape, and the parent rocks from which the soils formed (Soil Survey of Clark County, Kentucky; 1964).

  2. KY-2012-01-27-45 | Clark County - 1964

    Geolgic cross section of Clark County, showing some of the principal soils and their relation to the rock formations (Soil Survey of Clark County, Kentucky; 1964).

  3. KY-2012-01-27-68 | Fayette County - February 1968

    Relationship of soils to topography and underlying material in association 3. Unshaded areas represent caverns or sinkholes in the limestone bedrock (Soil Survey of Fayette County, Kentucky; February 1968).

  4. TN-2012-03-19-20 | Maury County - October 1959

    Sketch showing relative positions of soils in the Braxton-Maury-Armour assciation (Soil Survey of Maury County, TN; 1959).

  5. TN-2012-03-19-37 | Wayne County - 2000

    Typical pattern of soils and parent material in the Braxton-Talbott-Rock outcrop general soil map unit (Soil Survey of Wayne County, TN; 2000).

Map Units

Map units containing BRAXTON 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
Lyerly-Barfield-Braxton-Rock outcrop complex, 2 to 25 percent slopesLrD10402531501kv26ga61920121:24000
Braxton-Talbott-Lyerly complex, 2 to 6 percent slopes, very rockyBtB298425676462q79gga61920121:24000
Braxton-Talbott-Lyerly complex, 6 to 10 percent slopes, very rockyBtC296625676472q79hga61920121:24000
Braxton silt loam, 2 to 5 percent slopes, erodedBrB24434529363krv7tn00319981:24000
Braxton silt loam, 5 to 12 percent slopes, erodedBrC23457529364krv8tn00319981:24000
Braxton silty clay loam, 12 to 20 percent slopes, severely erodedBxD3775529365krv9tn00319981:24000
Talbott-Braxton-Rock outcrop complex, 20 to 35 percent slopesTrE8732526691kp21tn00719871:24000
Talbott-Braxton-Rock outcrop complex, 6 to 20 percent slopesTrD3739526690kp20tn00719871:24000
Talbott-Braxton complex, 6 to 12 percent slopesTaC922526688kp1ytn00719871:24000
Talbott-Braxton complex, 12 to 20 percent slopesTaD830526689kp1ztn00719871:24000
Talbott-Braxton complex, 2 to 6 percent slopesTaB276526687kp1xtn00719871:24000
Braxton silt loam, 5 to 12 percent slopesBrC5875526420kns9tn01920001:24000
Braxton silt loam, 12 to 20 percent slopes, erodedBrD25819526421knsbtn01920001:24000
Braxton-Talbott-Rock outcrop complex, 20 to 35 percent slopes, erodedBtE24823526426knshtn01920001:24000
Braxton silt loam, 20 to 35 percent slopes, erodedBrE23420526422knsctn01920001:24000
Braxton-Talbott-Rock outcrop complex, 12 to 20 percent slopes, erodedBtD22428526425knsgtn01920001:24000
Braxton-Urban land complex, 5 to 20 percent slopesBuD2163526427knsjtn01920001:24000
Braxton silt loam, 2 to 5 percent slopesBrB1985557556lq5ptn01920001:24000
Braxton silt loam, 35 to 50 percent slopes, erodedBrF21422526423knsdtn01920001:24000
Talbott-Rock outcrop-Braxton complex, 20 to 40 percent slopesToE3413523901kl51tn03519981:24000
Talbott-Braxton-Rock outcrop complex, 5 to 20 percent slopesTbD925523900kl50tn03519981:24000
Braxton silty clay loam, 5 to 12 percent slopes, severely erodedBtC34240527284kpp5tn05519651:15840
Braxton cherty silt loam, 5 to 12 percent slopes, erodedBrC23163527280kpp1tn05519651:15840
Braxton cherty silty clay loam, 5 to 12 percent slopes, severely erodedBsC32445527282kpp3tn05519651:15840
Braxton cherty silty clay loam, 12 to 20 percent slopes, severely erodedBsD32281527283kpp4tn05519651:15840
Braxton cherty silt loam, 12 to 20 percent slopes, erodedBrD21995527281kpp2tn05519651:15840
Braxton cherty silt loam, 2 to 5 percent slopes, erodedBrB2887527279kpp0tn05519651:15840
Braxton silty clay loam, 12 to 20 percent slopes, severely erodedBtD3832527285kpp6tn05519651:15840
Talbott cherty silt loam, 12 to 25 percent slopes (Braxton)TbE1388327652bzyftn07119611:15840
Talbott silt loam, 12 to 25 percent slopes (Braxton)TsE1049327659bzyntn07119611:15840
Talbott cherty silt loam, 5 to 12 percent slopes (Braxton)TbD1046327651bzydtn07119611:15840
Talbott silt loam, 5 to 8 percent slopes (Braxton)TsC649327657bzyltn07119611:15840
Talbott silt loam, 8 to 12 percent slopes (Braxton)TsD625327658bzymtn07119611:15840
Talbott cherty silt loam, 25 to 35 percent slopes (Braxton)TbF488327653bzygtn07119611:15840
Talbott silty clay, 8 to 25 percent slopes, severely eroded (Braxton)TtE3439327661bzyqtn07119611:15840
Talbott cherty silty clay, 12 to 25 percent slopes, severely eroded (Braxton cr-sicl)TcE3335327655bzyjtn07119611:15840
Talbott silty clay, 5 to 8 percent slopes, severely eroded (Braxton)TtC3258327660bzyptn07119611:15840
Talbott cherty silty clay, 5 to 12 percent slopes, severely eroded (Braxton)TcD3253327654bzyhtn07119611:15840
Talbott silt loam, 2 to 5 percent slopes (Braxton)TsB66327656bzyktn07119611:15840
Braxton silt loam, 2 to 5 percent slopes, erodedBtB29608524061klb6tn11719991:24000
Braxton-Talbott-Rock outcrop complex, 2 to 12 percent slopes, erodedBxC29497524063klb8tn11719991:24000
Braxton silt loam, 5 to 12 percent slopes, erodedBtC22548524062klb7tn11719991:24000
Braxton cherty silty clay loam, severely eroded sloping phaseBg13136527741kq4xtn11919551:20000
Braxton silty clay loam, eroded sloping phaseBk6718527743kq4ztn11919551:20000
Braxton cherty silty clay, severely eroded moderately steep phaseBf3818527740kq4wtn11919551:20000
Braxton silt loam, eroded gently sloping phaseBh3212527742kq4ytn11919551:20000
Braxton silty clay loam, eroded moderately steep phaseBl1780527744kq50tn11919551:20000
Braxton-Talbott complex, 15 to 35 percent slopesBtE1542560607ltc3tn13520001:24000
Braxton-Talbott complex, 15 to 35 percent slopes, severely erodedBtE31085560608ltc4tn13520001:24000
Braxton-Talbott complex, 5 to 15 percent slopesBtC590560605ltc1tn13520001:24000
Braxton-Talbott complex, 5 to 15 percent slopes, severely erodedBtC3461560606ltc2tn13520001:24000
Colbert-Talbott-Braxton complex, 5 to 12 percent slopes, erodedCtC2586529606ks32tn15319951:24000
Colbert-Talbott-Braxton complex, 12 to 20 percent slopes, erodedCtD2490529607ks33tn15319951:24000
Braxton gravelly silt loam, 12 to 20 percent slopes, erodedBxD2498529811ks9ptn15919921:24000
Braxton gravelly silt loam, 5 to 12 percent slopes, erodedBxC2279529810ks9ntn15919921:24000
Braxton silt loam, 5 to 12 percent slopesBrC50416896241tq60tn17919551:15840
Braxton-Urban land complex, 5 to 20 percent slopesBuD35116896291tq65tn17919551:15840
Braxton-Talbott-Rock outcrop complex, 20 to 35 percent slopes, erodedBtE218316896281tq64tn17919551:15840
Braxton silt loam, 12 to 20 percent slopes, erodedBrD210816896251tq61tn17919551:15840
Braxton-Talbott-Rock outcrop complex, 12 to 20 percent slopes, erodedBtD210616896271tq63tn17919551:15840
Braxton silt loam, 20 to 35 percent slopes, erodedBrE21316896261tq62tn17919551:15840
Braxton silt loam, 2 to 5 percent slopesBrB516896231tq5ztn17919551:15840
Braxton-Talbott complex, 15 to 35 percent slopesBsE7270328005c09ttn18119961:24000
Braxton-Talbott complex, 15 to 35 percent slopes, stonyBtE2325328006c09vtn18119961:24000
Braxton-Talbott complex, 5 to 15 percent slopesBsC2305328004c09stn18119961:24000
Braxton silt loam, 5 to 12 percent slopesBrC725328000c09ntn18119961:24000
Braxton silty clay loam, 5 to 12 percent slopes, severely erodedBrC3435328001c09ptn18119961:24000
Braxton silt loam, 12 to 20 percent slopesBrD286328002c09qtn18119961:24000
Braxton silty clay loam, 12 to 20 percent slopes, severely erodedBrD3262328003c09rtn18119961:24000
Braxton-Talbott-Gullied land complex, 5 to 20 percent slopesBxC250328007c09wtn18119961:24000
Braxton silt loam, 2 to 5 percent slopesBrB170327999c09mtn18119961:24000
Braxton cherty silt loam, 5 to 12 percent slopes, erodedBrC22467523473kkq7tn18719611:15840
Braxton cherty silt loam, 2 to 5 percent slopes, erodedBrB2841523472kkq6tn18719611:15840
Braxton cherty silt loam, 12 to 20 percent slopes, erodedBrD2714523474kkq8tn18719611:15840
Braxton cherty silty clay loam, 5 to 12 percent slopes, severely erodedBsC3614523475kkq9tn18719611:15840
Braxton cherty silty clay loam, 12 to 20 percent slopes, severely erodedBsD3336523476kkqbtn18719611:15840

Map of Series Extent

Approximate geographic distribution of the BRAXTON 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 .