Official Series Description


Lab Data Summary

Aggregate lab data for the SAGERTON soil series. This aggregation is based on all pedons with a current taxon name of SAGERTON, 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 SAGERTON 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
78B40A4542MLRA78-Sagerton-TX263-2092Sagerton5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.0194435,-100.9749985
78BS09TX353101S09TX353101Sagerton6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.5177078,-100.4754105
78BS09TX353102S09TX353102Sagerton6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.5175133,-100.47612
78C82P0611MLRA78-Tillman-TX207-004Sagerton8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.2063904,-99.6891632
78CS08TX441101S08TX441101Sagerton6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.3395844,-100.0480423
80B84P078193TX503001Sagerton8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.3886108,-98.7816696

Water Balance

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

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with SAGERTON, 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-2010-11-05-05 | Young County - 2009

    Pattern of soils and underlying material in the Sagerton general soil map unit (Soil Survey of Young County, Texas; 2009).

  2. TX-2012-03-21-47 | McCulloch County - November 1974

    Pattern of soils in Pedernales-Sagerton-Clairemont association (Soil Survey of McCulloch County, TX; 1974).

Map Units

Map units containing SAGERTON 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
Sagerton clay loam, moist, 0 to 1 percent slopesSaA151773627332t00ptx02319711:24000
Sagerton clay loam, moist, 1 to 3 percent slopesSaB120573627342t00qtx02319711:24000
Sagerton-Rotan complex, 1 to 3 percent slopesSrB2802962336f6m0tx03319701:24000
Sagerton loam, 1 to 3 percent slopes3822165363613d6cgtx05919791:24000
Sagerton loam, 0 to 1 percent slopes371618363612d6cftx05919791:24000
Sagerton clay loam, 0 to 1 percent slopesOcA375233639892t00jtx08119681:24000
Sagerton clay loam, 1 to 3 percent slopesOcB277323639902t00ktx08119681:24000
Sagerton clay loam, warm, 1 to 3 percent slopesOcB268933640282t00htx08319681:24000
Sagerton clay loam, warm, 0 to 1 percent slopesOcA66473640272t00gtx08319681:24000
Lueders-Sagerton complexEl61139364099d6w4tx08719651:20000
Sagerton silty clay loam, 1 to 3 percent slopesLcB6251364103d6w8tx08719651:20000
Sagerton silty clay loam, 3 to 5 percent slopesLcC1138364104d6w9tx08719651:20000
Sagerton clay loam, warm, 1 to 3 percent slopesSaB3083644472t00htx09519851:24000
Sagerton clay loam, 0 to 1 percent slopesScA52573646142t00jtx10119691:20000
Sagerton clay loam, 1 to 3 percent slopesScB50263646152t00ktx10119691:20000
Sagerton-Rotan complex, 1 to 3 percent slopesSrB4457393638f6m0tx11520041:24000
Sagerton clay loam, 0 to 1 percent slopesSaA1676960132t00jtx15320041:24000
Sagerton loam, 1 to 3 percent slopesOtB154403669552t00mtx19119651:20000
Sagerton loam, 0 to 1 percent slopesOtA62783669542t00ltx19119651:20000
Sagerton clay loam, moist, 1 to 3 percent slopesOcB142893671542t00qtx19719651:20000
Sagerton clay loam, moist, 0 to 1 percent slopesOcA96793671532t00ptx19719651:20000
Sagerton clay loam, moist, 0 to 1 percent slopesOtA585563682462t00ptx25319661:20000
Sagerton clay loam, moist, 1 to 3 percent slopesOtB327503682472t00qtx25319661:20000
Sagerton clay loam, 1 to 3 percent slopesOcB448553684962t00ktx26319681:31680
Sagerton clay loam, 0 to 1 percent slopesOcA86233684952t00jtx26319681:31680
Sagerton clay loam, moist, 0 to 1 percent slopes31136983687332t00ptx27519751:24000
Sagerton clay loam, moist, 1 to 3 percent slopes3221153687342t00qtx27519751:24000
Sagerton clay loam, warm, 1 to 3 percent slopesSaB29343699712t00htx30719701:24000
Sagerton clay loam, warm, 0 to 1 percent slopesSaA20213699702t00gtx30719701:24000
Sagerton clay loam, 1 to 3 percent slopesOcB102323707332t00ktx33519651:20000
Sagerton clay loam, 0 to 1 percent slopesOcA81383707322t00jtx33519651:20000
Sagerton clay loam, 1 to 3 percent slopesSaB240003708952t00ktx34519721:24000
Sagerton clay loam, 0 to 1 percent slopesSaA56633708942t00jtx34519721:24000
Sagerton clay loam, 1 to 3 percent slopes40113743710102t00ktx35319791:24000
Sagerton clay loam, 0 to 1 percent slopes39104203710082t00jtx35319791:24000
Sagerton clay loam, 0 to 1 percent slopesOcA278723717792t00jtx39919651:20000
Sagerton clay loam, 1 to 3 percent slopesOcB168273717802t00ktx39919651:20000
Sagerton clay loam, warm, 1 to 3 percent slopesSaB216793719762t00htx41119801:24000
Sagerton clay loam, warm, 0 to 1 percent slopesSaA116513719752t00gtx41119801:24000
Sagerton clay loam, 1 to 3 percent slopesOcB526313720202t00ktx41519661:24000
Sagerton clay loam, 0 to 1 percent slopesOcA246523720192t00jtx41519661:24000
Sagerton loam, 1 to 3 percent slopesOlB159563720222t00mtx41519661:24000
Sagerton loam, 0 to 1 percent slopesOlA49683720212t00ltx41519661:24000
Sagerton clay loam, 1 to 3 percent slopesOtB28563722482t00ktx43119741:31680
Sagerton clay loam, moist, 0 to 1 percent slopesSaA681743915482t00ptx44119711:20000
Sagerton clay loam, moist, 1 to 3 percent slopesSaB361923915492t00qtx44119711:20000
Sagerton-Urban land complex, 0 to 3 percent slopesSeB6624391550f4fntx44119711:20000
Sagerton clay loam, moist, 1 to 3 percent slopesSaB172813727132t00qtx44719911:24000
Sagerton clay loam, moist, 0 to 1 percent slopesSaA128603727122t00ptx44719911:24000
Sagerton clay loam, 0 to 1 percent slopesOlA18006372751dhw7tx45119711:20000
Sagerton clay loam, 1 to 3 percent slopesOlB2655372752dhw8tx45119711:20000
Sagerton-Urban land complex, 0 to 3 percent slopesOuB210372753dhw9tx45119711:20000
Sagerton loam, 1 to 3 percent slopesSaB22416373773djy6tx50320031:24000
Sagerton loam, 0 to 1 percent slopesSaA6286373772djy5tx50320031:24000
Sagerton clay loam, warm, 1 to 3 percent slopes67181503910452t00htx60219751:24000
Sagerton clay loam, warm, 0 to 1 percent slopes6652933910442t00gtx60219751:24000
Sagerton-Urban land complex, 0 to 3 percent slopes681758391046f3xdtx60219751:24000

Map of Series Extent

Approximate geographic distribution of the SAGERTON 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 .