Official Series Description


Lab Data Summary

Aggregate lab data for the DAVISON soil series. This aggregation is based on all pedons with a current taxon name of DAVISON, 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 DAVISON 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 DAVISON 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 DAVISON 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 DAVISON 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 DAVISON 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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Click the image to view it full size.

Competing Series

Soil series competing with DAVISON 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 DAVISON 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 DAVISON 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 DAVISON, 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. SD-2010-11-01-06 | Clay County - 2003

    Typical pattern of soils and underlying material in the Egan-Ethan-Trent association (Soil Survey of Clay County, South Dakota; 2003).

  2. SD-2010-11-01-10 | Minnehaha County - 2004

    Typical pattern of soils and parent material in the Egan-Ethan-Trent association (Soil Survey of Minnehaha County, South Dakota; 2004).

  3. SD-2012-03-14-03 | Bon Homme County - January 1983

    Pattern of soils and underlying material in the Clarno-Crossplain-Davison association (Soil Survey of Bon Homme County, SD; 1983).

  4. SD-2012-03-16-01 | Turner County - November 1982

    Pattern of soils and parent material in the Clarno-Crossplain-Davison association (Soil Survey of Turner County, SD; 1982).

Map Units

Map units containing DAVISON 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
Prosper-Davison loams, 0 to 3 percent slopesPrA1479354597cwzmsd00519761:20000
Clarno-Crossplain-Davison complex, 0 to 2 percent slopesCnA556814182542wkqcsd00919811:20000
Homme-Davison-Tetonka complex, 0 to 3 percent slopesHmA10648418275g17rsd00919811:20000
Onita-Davison complexOo767355059cxgjsd02319801:20000
Davison-Crossplain complexDa345417714g0nnsd02519921:20000
Egan-Chancellor-Davison complex, 0 to 3 percent slopesEaA24913445548gymjsd02719951:24000
Davison-Tetonka-Egan complex, 0 to 3 percent slopesDkA11448445544gymdsd02719951:24000
Davison-Chancellor complex, 0 to 3 percent slopesDhA2788445543gymcsd02719951:24000
Ethan-Davison-Tetonka complex, 0 to 6 percent slopesEuB1013445569gyn6sd02719951:24000
Hand-Davison loams, 0 to 3 percent slopesHdA28983529232yyglsd03519661:20000
Davison-Hand loams, 0 to 2 percent slopesDhA8323529122yygksd03519661:20000
Davison loam, nearly levelHaA10352607ctxfsd05919591:20000
Davison loamDc209356418cywcsd07319871:20000
Davison-Crossplain complexDc2768417471g0dtsd07719921:20000
Clarno-Davison loams, 2 to 5 percent slopesCeB12565418014g0zbsd08719761:20000
Hand-Davison loams, 2 to 6 percent slopesHcB79094180292xhd4sd08719761:20000
Clarno-Crossplain-Davison complex, 0 to 2 percent slopesCfA58024180152wkqcsd08719761:20000
Hand-Davison-Crossplain complex, 0 to 2 percent slopesHdA49044180302yygnsd08719761:20000
Davison-Crossplain clay loams, 0 to 2 percent slopesDd45418046g10csd08719761:20000
Worthing-Davison complex, 0 to 2 percent slopesWr8863446091gz61sd09919951:24000
Davison-Crossplain clay loams, 0 to 2 percent slopesDd3236446020gz3rsd09919951:24000
Davison-Crossplain clay loamsDc4357418312g18ysd10119851:20000
Davison loamDa367355318cxqwsd10719831:20000
Tetonka-Davison-Clarno complex, 0 to 2 percent slopesTcA15788354812cx6ksd11119781:20000
Shue-Davison loamy fine sandsSa7762354808cx6fsd11119781:20000
Davison loamDb929354773cx59sd11119781:20000
Davison variant silt loamDc593354774cx5bsd11119781:20000
Lawet-Davison loams, 0 to 2 percent slopesLp1786356677cz4qsd11519971:24000
Davison-Tetonka complex, 0 to 2 percent slopesDd1008356585cz1rsd11519971:24000
Davison loam, 0 to 2 percent slopesDb829356584cz1qsd11519971:24000
Clarno-Crossplain-Davison complex, 0 to 2 percent slopesCkA416864182152wkqcsd12519801:20000
Clarno-Davison loams, 2 to 5 percent slopesCmB1595418216g15vsd12519801:20000
Clarno-Crossplain-Davison complex, 0 to 2 percent slopesCkA509944180672wkqcsd13519771:20000
Clarno-Davison loams, 2 to 4 percent slopesCeB29487417946g0x4sd60219751:20000
Clarno-Crossplain-Davison complex, 0 to 2 percent slopesCeA109944179452wkqcsd60219751:20000
Hand-Davison loams, 2 to 6 percent slopesHdB109484179782xhd4sd60219751:20000
Davison loam, 0 to 3 percent slopesDbA3370417952g0xbsd60219751:20000
Davison-Onita complex, 2 to 6 percent slopesDcB2083119208g0xcsd60219751:20000

Map of Series Extent

Approximate geographic distribution of the DAVISON 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 .