Official Series Description


Lab Data Summary

Aggregate lab data for the HIXTON soil series. This aggregation is based on all pedons with a current taxon name of HIXTON, 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 HIXTON 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
10501P0210S2000WI063024Hixton5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9896126,-90.9574966
90B81P0094S1980WI017005Hixton4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1533333,-91.5536111

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HIXTON 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 HIXTON 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 HIXTON 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 HIXTON 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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Competing Series

Soil series competing with HIXTON 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 HIXTON 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 HIXTON 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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There are insufficient data to create the 3D mountains figure.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with HIXTON, 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. WI-2012-03-22-02 | Buffalo County - March 1962

    Soil associations and relief in Buffalo County. 1. Silty soils of the rolling limestone uplands and Steep stony and rocky land: Dubuque, Fayette, Steep stony and rocky land. 2. Loamy soils of the rolling to hilly sandstone uplands: Gale, Hixton. 3. Sandy soils of the rolling to hilly sandstone uplands: Boone, Hixton. 4. Sandy soils of stream terraces: Sparta, Plainfield. 5. Silty soils of stream terraces: Bertrand, Richwood. 6. Loamy terrace soils underlain by sand on stream terraces: Meridian, Tell. 7. Wet organic and mineral soils of bottom lands: Peat and Muck, Ettrick, Wallkill. 8. Soils of overflow bottom lands: Loamy alluvial lands, Marsh (Soil Survey of Bayfield County, WI; 1961).

  2. WI-2012-03-22-04 | Crawford County - December 1961

    Landscape of Crawford County showing the parent materials of the soils and relationships among major soil series (Soil Survey of Crawford County, WI; 1961).

  3. WI-2012-03-23-30 | Pepin County - March 1964

    Cross section showing the geology and the associated soils in Pepin County (Soil Survey of Pepin County, WI; 1964).

Map Units

Map units containing HIXTON 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
Hixton fine sandy loam, 20 to 40 percent slopes441G319409202fqt2ia12119681:15840
Hixton loam, 0 to 6 percent slopes23B8411886926bbvmi02519931:15840
Hixton fine sandy loam, 12 to 35 percent slopes, moderately erodedHb45722167462ddpymn04520081:12000
Hixton fine sandy loam, 2 to 11 percent slopes, moderately erodedHa9022167472ddpzmn04520081:12000
Gale-Hixton complex, shallow, 12 to 18 percent slopes, moderately erodedGhD227222163742dd9ymn15720081:12000
Hixton fine sandy loam, 12 to 18 percent slopes, moderately erodedHfD226922163802ddb4mn15720081:12000
Hixton fine sandy loam, 2 to 6 percent slopesHfB26222163822ddb6mn15720081:12000
Hixton fine sandy loam, 6 to 12 percent slopes, moderately erodedHfC220122163832ddb7mn15720081:12000
Gale-Hixton complex, shallow, 6 to 12 percent slopes, moderately erodedGhC217822163762ddb0mn15720081:12000
Gale-Hixton complex, shallow, 18 to 25 percent slopesGhE15322163752dd9zmn15720081:12000
Hixton fine sandy loam, 18 to 35 percent slopesHfE11922163812ddb5mn15720081:12000
Hixton silt loam, 2 to 6 percent slopes, moderately erodedHxB214694229382ysc4wi00119781:20000
Hixton silt loam, 12 to 20 percent slopes, moderately eroded213D2235526394432ysccwi01119601:20000
Hixton silt loam, 6 to 12 percent slopes, moderately eroded213C2202826394422ysc8wi01119601:20000
Hixton silt loam, 2 to 6 percent slopes, moderately eroded213B259326394412ysc4wi01119601:20000
Hixton silt loam, 20 to 30 percent slopes, moderately eroded213E218226394442yscfwi01119601:20000
Hixton silt loam, 6 to 12 percent slopes, moderately erodedHxC235454215302ysc8wi01719851:15840
Hixton silt loam, thin solum, 2 to 6 percent slopes, moderately erodedHnB228874215362ysc6wi01719851:15840
Hixton silt loam, 12 to 20 percent slopes, moderately erodedHxD223074215312ysccwi01719851:15840
Hixton silt loam, thin solum, 6 to 12 percent slopes, moderately erodedHnC216114215372ysc9wi01719851:15840
Hixton silt loam, 2 to 6 percent slopes, moderately erodedHxB28724215292ysc4wi01719851:15840
Hixton loam, 6 to 12 percent slopes, moderately erodedHbC222227535202yscbwi02519721:15840
Hixton loam, 12 to 20 percent slopes, moderately erodedHbD221007535212yscdwi02519721:15840
Hixton loam, 2 to 6 percent slopes, moderately erodedHbB214657535192ysc7wi02519721:15840
Dobie and Hixton silt loams, 6 to 12 percent slopes, moderately eroded273C277872518505n56fwi03320031:15840
Dobie and Hixton silt loams, 12 to 20 percent slopes, moderately eroded273D256982518506n56hwi03320031:15840
Dobie and Hixton silt loams, 2 to 6 percent slopes, moderately eroded273B249292518504n56cwi03320031:15840
Hixton silt loam, thin solum, 2 to 6 percent slopes, moderately eroded243B2486225184972ysc6wi03320031:15840
Dobie and Hixton silt loams, 20 to 30 percent slopes, moderately eroded273E218772518507n56kwi03320031:15840
Hixton silt loam, thin solum, 6 to 12 percent slopes, moderately eroded243C252325184982ysc9wi03320031:15840
Hixton silt loam, 6 to 12 percent slopes, moderately eroded213C213924982922ysc8wi03320031:15840
Hixton silt loam, 2 to 6 percent slopes, moderately eroded213B213624982912ysc4wi03320031:15840
Hixton silt loam, 12 to 20 percent slopes, moderately eroded213D2595930996752ysccwi03519741:15840
Hixton silt loam, 6 to 12 percent slopes, moderately eroded213C2473330996472ysc8wi03519741:15840
Hixton silt loam, 2 to 6 percent slopes, moderately eroded213B2400830996462ysc4wi03519741:15840
Hixton silt loam, 20 to 30 percent slopes, moderately eroded213E2385830996762yscfwi03519741:15840
Hixton silt loam, thin solum, 6 to 12 percent slopes, moderately eroded243C264330996492ysc9wi03519741:15840
Hixton silt loam, thin solum, 2 to 6 percent slopes, moderately eroded243B231730996482ysc6wi03519741:15840
Hixton loam, 12 to 30 percent slopes, erodedHhE247425443g8pzwi03919671:15840
Hixton fine sandy loam, 20 to 30 percent slopes, moderately erodedHfF27109424266g7h0wi04319591:20000
Hixton fine sandy loam, 15 to 20 percent slopes, moderately erodedHfE26640424263g7gxwi04319591:20000
Hixton fine sandy loam, 10 to 15 percent slopes, moderately erodedHfD22370424260g7gtwi04319591:20000
Hixton loam, 12 to 20 percent slopes, moderately erodedHxD213104242722yscdwi04319591:20000
Hixton loam, 20 to 30 percent slopes, moderately erodedHxF26864242772yz77wi04319591:20000
Hixton fine sandy loam, 6 to 10 percent slopes, moderately erodedHfC2426424258g7grwi04319591:20000
Hixton loam, 6 to 12 percent slopes, moderately erodedHxC21274242712yscbwi04319591:20000
Hixton fine sandy loam, 30 to 45 percent slopesHfG88424268g7h2wi04319591:20000
Hixton fine sandy loam, 2 to 6 percent slopes, moderately erodedHfB264424257g7gqwi04319591:20000
Hixton loam, 2 to 6 percent slopes, moderately erodedHmB27744252822ysc7wi04519691:12000
Hixton loam, 6 to 12 percent slopes, moderately erodedHmC27244252832yscbwi04519691:12000
Hixton sandy loam, 12 to 20 percent slopes, moderately erodedHtD21638424636g7vywi04919601:20000
Hixton sandy loam, 20 to 30 percent slopes, moderately erodedHtE2738424639g7w1wi04919601:20000
Hixton sandy loam, 6 to 12 percent slopes, moderately erodedHtC2242424634g7vwwi04919601:20000
Hixton sandy loam, 2 to 6 percent slopes, moderately erodedHtB231424632g7vtwi04919601:20000
Hixton silt loam, 6 to 12 percent slopes, moderately eroded213C2288624983042ysc8wi05319941:20000
Hixton silt loam, 12 to 20 percent slopes, moderately eroded213D2178424983052ysccwi05319941:20000
Hixton silt loam, 2 to 6 percent slopes, moderately eroded213B235124983032ysc4wi05319941:20000
Hixton silt loam, 2 to 6 percent slopes, moderately eroded213B286725614432ysc4wi05719871:15840
Hixton silt loam, 6 to 12 percent slopes, moderately eroded213C262125614442ysc8wi05719871:15840
Hixton silt loam, 20 to 30 percent slopes, moderately eroded213E282224983002yscfwi06320011:12000
Hixton silt loam, 12 to 20 percent slopes, moderately eroded213D249924982962ysccwi06320011:12000
Hixton loam, 12 to 20 percent slopes, moderately erodedHmD24684248282yscdwi06519641:15840
Hixton loam, 6 to 12 percent slopes, moderately erodedHmC23714248262yscbwi06519641:15840
Hixton sandy loam, 6 to 12 percent slopes, moderately erodedHtC2217424831g827wi06519641:15840
Hixton sandy loam, 12 to 20 percent slopes,moderately erodedHtD2180424832g828wi06519641:15840
Hixton loam, 20 to 30 percent slopes, moderately erodedHmE21424248292yz77wi06519641:15840
Hixton loam, 2 to 6 percent slopes, moderately erodedHmB21364248252ysc7wi06519641:15840
Hixton sandy loam, 2 to 6 percent slopes, moderately erodedHtB286424830g826wi06519641:15840
Hixton sandy loam, 20 to 30 percent slopes, moderately erodedHtE27114547441kts7wi06519641:15840
Hixton silt loam, 12 to 20 percent slopes, moderately eroded213D2137626851522ysccwi08119811:15840
Hixton silt loam, 6 to 12 percent slopes, moderately eroded213C2100326851512ysc8wi08119811:15840
Hixton silt loam, 20 to 30 percent slopes, moderately eroded213E21126851532yscfwi08119811:15840
Hixton silt loam, 20 to 30 percent slopes, moderately eroded213E235124983012yscfwi09119981:12000
Hixton silt loam, 12 to 20 percent slopes, moderately eroded213D213624982972ysccwi09119981:12000
Hixton silt loam, 6 to 12 percent slopes, moderately eroded213C26124982932ysc8wi09119981:12000
Hixton loam, till plain, 6 to 12 percent slopes, moderately eroded200C2100016974831tzcjwi09320061:12000
Hixton silt loam, meteorite crater, 6 to 12 percent slopes, moderately eroded211C243416974941tzcwwi09320061:12000
Hixton silt loam, meteorite crater, 12 to 20 percent slopes, moderately eroded211D221516974921tzctwi09320061:12000
Hixton silt loam, meteorite crater, 2 to 6 percent slopes, moderately eroded211B220616974931tzcvwi09320061:12000
Hixton silt loam, 12 to 20 percent slopes, moderately erodedHxD279944231602ysccwi11119771:15840
Hixton silt loam, 6 to 12 percent slopes, moderately erodedHxC269394231592ysc8wi11119771:15840
Hixton silt loam, 2 to 6 percent slopes, moderately erodedHxB225374231582ysc4wi11119771:15840
Hixton silt loam, 20 to 30 percent slopes, moderately erodedHxE224614231612yscfwi11119771:15840
Hixton silt loam, 12 to 20 percent slopes, moderately eroded213D22242226834452ysccwi12119691:15840
Hixton silt loam, 20 to 30 percent slopes, moderately eroded213E22224226834462yscfwi12119691:15840
Hixton silt loam, 6 to 12 percent slopes, moderately eroded213C2794226834422ysc8wi12119691:15840
Hixton silt loam, 2 to 6 percent slopes, moderately eroded213B2157126834412ysc4wi12119691:15840
Hixton silt loam, 20 to 30 percent slopes, moderately eroded213E263324983022yscfwi12319651:12000
Hixton silt loam, 12 to 20 percent slopes, moderately eroded213D262324982982ysccwi12319651:12000
Hixton silt loam, 6 to 12 percent slopes, moderately eroded213C25824982942ysc8wi12319651:12000
Hixton silt loam, cool, 2 to 6 percent slopes, moderately erodedHxcB219534264532ysc5wi14119711:20000

Map of Series Extent

Approximate geographic distribution of the HIXTON 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 .