Official Series Description


Lab Data Summary

Aggregate lab data for the AXTELL soil series. This aggregation is based on all pedons with a current taxon name of AXTELL, 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 AXTELL 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
86A85P023484TX349001Axtell7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.0424995,-96.7324982
86A40A4477P1962TX257004AXTELL6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.4230537,-96.148056
86A40A4478P1962TX257005AXTELL5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.4083328,-96.1399994

Water Balance

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

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 AXTELL, 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-2012-02-17-08 | Love County - September 1966

    Diagram showing typical relief in the northwestern corner of the county and the relative positions of the soils in association 4 (Soil Survey of Love County, Oklahoma; September 1966).

  2. 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).

  3. TX-2010-11-03-17 | Gonzales County - 2006

    Pattern of soils and underlying material in the Edge-Rosanky general soil map unit (Soil Survey of Gonzales County, Texas; 2006).

  4. TX-2010-11-04-05 | McLennan County - 2001

    Pattern of soils in the Weswood-Yahola-Ships general soil map unit (Soil Survey of McLennan County, Texas; 2001).

  5. 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).

  6. TX-2012-03-21-51 | Navarro County - December 1974

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

  7. TX-2012-03-22-16 | Williamson County - January 1983

    Typical landscape pattern of the Axtell-Rosanky-Rader general soil map unit (Soil Survey of Williamson County, TX; 1983).

Map Units

Map units containing AXTELL 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
Axtell fine sandy loam, 5 to 12 percent slopesAtE83075751192shg7tx00119701:20000
Axtell fine sandy loam, 1 to 3 percent slopesAtB46915751172shg6tx00119701:20000
Axtell fine sandy loam, 2 to 5 percent slopes, moderately erodedAtC226905751182shgdtx00119701:20000
Axtell-Derly, occasionally ponded complex, 0 to 1 percent slopesAwA2375575120m9g8tx00119701:20000
Axtell fine sandy loam, 0 to 1 percent slopesAfA14553932662shg5tx02119721:24000
Axtell fine sandy loam, 1 to 3 percent slopesAxB7623910692shg6tx02719721:24000
Axtell fine sandy loam, 1 to 3 percent slopesAxB38123631742shg6tx04119931:20000
Axtell fine sandy loam, 1 to 4 percent slopesAxB38313634252shg9tx05119941:24000
Axtell-Urban land complex, 1 to 5 percent slopes134438364793d7ljtx11319751:20000
Axtell fine sandy loam, 1 to 3 percent slopes1122563647912shg6tx11319751:20000
Axtell fine sandy loam, 2 to 5 percent slopes, moderately eroded1214623647922shgdtx11319751:20000
Axtell fine sandy loam, 0 to 1 percent slopes105393647902shg5tx11319751:20000
Axtell fine sandy loam, 1 to 3 percent slopes882453654922shg6tx14519751:20000
Axtell fine sandy loam, 2 to 5 percent slopes, moderately eroded952303654932shgdtx14519751:20000
Axtell and Crockett soils, 2 to 8 percent slopes, severely eroded101620365427d87ztx14519751:20000
Axtell fine sandy loam, 0 to 1 percent slopes79843654912shg5tx14519751:20000
Axtell fine sandy loam, 1 to 5 percent slopesAxB42823753692shgctx16119861:24000
Axtell fine sandy loam, 5 to 12 percent slopesAxD10883753702shg7tx16119861:24000
Axtell gravelly fine sandy loam, 1 to 3 percent slopesAxB1421366542d9dytx17719971:24000
Axtell gravelly fine sandy loam, 5 to 12 percent slopesAxE1039366544d9f0tx17719971:24000
Axtell gravelly fine sandy loam, 3 to 5 percent slopesAxC970366543d9dztx17719971:24000
Axtell fine sandy loam, 1 to 5 percent slopesAxC125653667322shgctx18519881:24000
Axtell fine sandy loam, 5 to 12 percent slopesAxD21023667342shg7tx18519881:24000
Axtell fine sandy loam, 2 to 5 percent slopes, moderately erodedAxC28983667332shgdtx18519881:24000
Axtell loam, 1 to 5 percent slopes1288673675982shgbtx21319781:20000
Axtell loam, 5 to 12 percent slopes2231403676092shg8tx21319781:20000
Axtell fine sandy loam, 1 to 3 percent slopes1026823677212shg6tx21719751:20000
Axtell fine sandy loam, 2 to 5 percent slopes, moderately eroded1119373677222shgdtx21719751:20000
Axtell fine sandy loam, 0 to 1 percent slopes98803678002shg5tx21719751:20000
Axtell loam, 1 to 5 percent slopes1276883678702shgbtx23119781:24000
Axtell loam, 5 to 12 percent slopes295613678812shg8tx23119781:24000
Axtell fine sandy loam, 1 to 5 percent slopesAxB91733691712shgctx28919851:24000
Axtell fine sandy loam, 5 to 12 percent slopesAxD44583691722shg7tx28919851:24000
Axtell fine sandy loam, 0 to 1 percent slopesAxA19703691702shg5tx28919851:24000
Axtell fine sandy loam, 1 to 3 percent slopesAxB141173693832shg6tx29319911:24000
Axtell fine sandy loam, 0 to 1 percent slopesAxA34063693822shg5tx29319911:24000
Axtell fine sandy loam, 1 to 3 percent slopesAxB196143700742shg6tx30919921:24000
Axtell fine sandy loam, 1 to 3 percent slopesAxB2231300692shg6tx33119881:24000
Axtell fine sandy loam, 1 to 3 percent slopesAxB166103709102shg6tx34919681:24000
Axtell fine sandy loam, 3 to 5 percent slopesAxC6775370911dfywtx34919681:24000
Axtell fine sandy loam, 5 to 12 percent slopesAxE60073709132shg7tx34919681:24000
Axtell fine sandy loam, 2 to 5 percent slopes, moderately erodedAxC215873709122shgdtx34919681:24000
Axtell fine sandy loam, 1 to 5 percent slopes332483731572shgctx47719791:24000
Axtell fine sandy loam, 5 to 12 percent slopes417613731682shg7tx47719791:24000
Axtell fine sandy loam, 2 to 5 percent slopes, erodedAxC37800373521djp2tx49119811:20000
Axtell fine sandy loam, 1 to 3 percent slopesAxB7343735202shg6tx49119811:20000
Axtell fine sandy loam, 1 to 5 percent slopesAxC34453738092shgctx60019811:24000
Axtell fine sandy loam, 5 to 12 percent slopesAxD17103738112shg7tx60019811:24000
Axtell fine sandy loam, 2 to 5 percent slopes, moderately erodedAxC25343738102shgdtx60019811:24000
Axtell fine sandy loam, 1 to 4 percent slopesAxB150183744622shg9tx61219731:20000
Axtell fine sandy loam, 5 to 12 percent slopesAxD118763744642shg7tx61219731:20000
Axtell fine sandy loam, 2 to 5 percent slopes, moderately erodedAxC2107733744632shgdtx61219731:20000

Map of Series Extent

Approximate geographic distribution of the AXTELL 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 .