Official Series Description


Lab Data Summary

Aggregate lab data for the DENTON soil series. This aggregation is based on all pedons with a current taxon name of DENTON, 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 DENTON 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
8540A4514S1963TX099001Denton7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.5308342,-97.6074982
8540A4530S1963TX099002Denton7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.5505562,-97.6302795
8540A4515S1963TX099003Denton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.5505562,-97.628891
85S82TX099001S1982TX099001Denton5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.5338688,-97.6451035

Water Balance

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

Click the image to view it full size.

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 DENTON, 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. OK-2012-02-17-09 | Love County - September 1966

    Diagram showing relief typical of the central part of the county and the relative positions of the soils in association 7 (Soil Survey of Love County, Oklahoma; September 1966).

  2. TX-2010-11-03-22 | Hamilton County - 2007

    Pattern of soils and underlying material in the Denton-Bolar-Oglesby and Eckrant-Evant general soil map units (Soil Survey of Hamilton County, Texas; 2007).

  3. 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).

  4. TX-2010-11-04-06 | McLennan County - 2001

    Pattern of soils in the Crawford-Purves and Slidell-Sanger general soil map units (Soil Survey of McLennan County, Texas; 2001).

  5. TX-2012-03-20-22 | Comal and Hays Counties - June 1984

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

  6. TX-2012-03-20-25 | Comal and Hays Counties - June 1984

    Pattern of soils in the Krum-Medlin-Eckrant general soil map unit (Soil Survey of Comal and Hays Counties, TX; 1984).

  7. TX-2012-03-20-28 | Coryell County - May 1985

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

  8. TX-2012-03-22-12 | Williamson County - January 1983

    Typical landscape pattern of the Oakalla-Sunev and the Denton-Eckrant-Doss general soil map units (Soil Survey of Williamson County, TX; 1983).

Map Units

Map units containing DENTON 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
Denton silty clay, 1 to 3 percent slopesDeB371263910852tc47tx02719721:24000
Denton silty clay, 0 to 1 percent slopesDeA4583910842tc46tx02719721:24000
Denton silty clay, 1 to 3 percent slopesDnB291543629912tc47tx03519771:24000
Denton silty clay, 3 to 5 percent slopesDnC179333629922tc48tx03519771:24000
Denton silty clay, 3 to 5 percent slopesDnC125013643702tc48tx09319741:20000
Denton silty clay, 1 to 3 percent slopesDnB124223643692tc47tx09319741:20000
Denton silty clay, 1 to 3 percent slopesDeB262063911522tc47tx09919831:24000
Bolar-Denton complex 3 to 5 percent slopesBdC1347736535230knbtx14319661:20000
Denton silty clay, 1 to 3 percent slopesDeB100073653642tc47tx14319661:20000
Denton silty clay, dry, 1 to 3 percent slopesDnB118253661802t26ktx17119701:20000
Denton silty clay, 3 to 5 percent slopesDnC10539366181d919tx17119701:20000
Denton silty clay, 3 to 5 percent slopes, erodedDnC21929366182d91btx17119701:20000
Denton silty clay, 1 to 3 percent slopesDnB61593766582tc47tx19319941:24000
Denton clay, 1 to 3 percent slopes3310373677462tc45tx21719751:20000
Denton silty clay, 1 to 3 percent slopesDnB1493681632tc47tx25119811:20000
Denton silty clay, 1 to 3 percent slopes6110063684642t26ltx25919791:31680
Denton silty clay, 3 to 5 percent slopes718713684652t26rtx25919791:31680
Denton silty clay, dry, 1 to 3 percent slopesDnB18373685202t26ktx26519831:31680
Denton silty clay, 1 to 3 percent slopesDeB129573700862tc47tx30919921:24000
Denton clay, 1 to 3 percent slopesDeB114613908722tc45tx36719731:20000
Denton silty clay, 1 to 3 percent slopesDeB10693922372t26ltx45319691:20000
Denton silty clay, 3 to 5 percent slopesDeC5243922382t26rtx45319691:20000
Denton silty clay, 1 to 3 percent slopesDnB302713735412t26ltx49119811:20000
Denton silty clay, 3 to 5 percent slopesDnC30763735422t26rtx49119811:20000
Denton silty clay, 0 to 1 percent slopesDnA5393735402tc46tx49119811:20000
Denton silty clay, 1 to 3 percent slopes2757953910012tc47tx60219751:24000
Denton silty clay, 1 to 3 percent slopesDeB105653787162t26ltx60419811:20000
Denton silty clay, 1 to 5 percent slopes, moderately erodedDeC38683906942xmt7tx60419811:20000
Denton clay, 1 to 3 percent slopesDeB20723743292tc45tx60919751:20000
Denton silty clay, 3 to 5 percent slopesDeC5363743312tc48tx60919751:20000

Map of Series Extent

Approximate geographic distribution of the DENTON 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 .