Official Series Description


Lab Data Summary

Aggregate lab data for the KINGSLEY soil series. This aggregation is based on all pedons with a current taxon name of KINGSLEY, 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 KINGSLEY 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
103UMN1913S1975MN0371913Kingsley2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7767372,-93.1875534
103UMN2398S1977MN037001(2398)Kingsley2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7348404,-93.2485809
90B40A1761S1974MN163003Kingsley7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.9747162,-92.9385376
91BUMN1234S1971MN0031234Kingsley3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3994598,-93.4598846

Water Balance

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

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

Soil series sharing subgroup-level classification with KINGSLEY, 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

No block diagrams are available.

Map Units

Map units containing KINGSLEY 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
Emmert complex, 12 to 25 percent slopesEpD1196395922f8zpmn00319721:15840
Kingsley fine sandy loam, 6 to 12 percent slopes, erodedKmC2851395941f909mn00319721:15840
Kingsley fine sandy loam, 2 to 6 percent slopesKmB827395940f908mn00319721:15840
Kingsley fine sandy loam, 12 to 18 percent slopesKmD521395942f90bmn00319721:15840
Emmert complex, 4 to 12 percent slopesEpC181395921f8znmn00319721:15840
Urban land-Kingsley complex, 15 to 25 percent slopesUkD146114630217gthmn00319721:15840
Kingsley fine sandy loam, 18 to 30 percent slopesKmE111395943f90cmn00319721:15840
Kingsley-Mahtomedi-Spencer complex, 8 to 15 percent slopes895C7024396903fb0bmn03719801:15840
Kingsley sandy loam, 8 to 15 percent slopes342C6844396839f9y8mn03719801:15840
Urban land-Kingsley complex, 3 to 15 percent slopes861C5787396892f9zzmn03719801:15840
Kingsley-Mahtomedi complex, 15 to 25 percent slopes896E5686396904fb0cmn03719801:15840
Kingsley sandy loam, 3 to 8 percent slopes342B3648396838f9y7mn03719801:15840
Kingsley-Mahtomedi-Spencer complex, 3 to 8 percent slopes895B3040396902fb09mn03719801:15840
Kingsley sandy loam, 15 to 25 percent slopes342E2192396840f9y9mn03719801:15840
Kingsley-Mahtomedi complex, 25 to 40 percent slopes896F1314396905fb0dmn03719801:15840
Kingsley-Lester complex, 6 to 12 percent slopes888C1012396897fb04mn03719801:15840
Kingsley-Lester complex, 2 to 6 percent slopes888B773396896fb03mn03719801:15840
Kingsley sandy loam, 25 to 40 percent slopes342F644396841f9ybmn03719801:15840
Urban land-Kingsley complex, 15 to 25 percent slopes861E413396893fb00mn03719801:15840
Kingsley-Lester complex, 12 to 18 percent slopes888D336396898fb05mn03719801:15840
Koronis-Kingsley complex, 2 to 6 percent slopesL58B1575413391fw56mn05320011:12000
Koronis-Kingsley complex, 6 to 12 percent slopes, erodedL58C21237434666gl9hmn05320011:12000
Kingsley-Gotham complex, 6 to 12 percent slopesL42C954452781h64vmn05320011:12000
Koronis-Kingsley-Malardi complex, 18 to 35 percent slopesL62E764399488fdpqmn05320011:12000
Koronis-Kingsley-Malardi complex, 6 to 12 percent slopes, erodedL62C2714432654gj6lmn05320011:12000
Kingsley-Gotham complex, 12 to 18 percent slopesL42D660452782h64wmn05320011:12000
Kingsley-Gotham complex, 25 to 35 percent slopesL42F602452788h652mn05320011:12000
Kingsley-Gotham complex, 2 to 6 percent slopesL42B460452780h64tmn05320011:12000
Kingsley-Gotham complex, 18 to 25 percent slopesL42E443452787h651mn05320011:12000
Koronis-Kingsley complex, 12 to 18 percent slopes, erodedL58D2321434667gl9jmn05320011:12000
Koronis-Kingsley complex, 18 to 25 percent slopesL58E234434668gl9kmn05320011:12000
Koronis-Kingsley-Malardi complex, 2 to 6 percent slopesL62B139399470fdp4mn05320011:12000
Koronis-Kingsley-Malardi complex, 12 to 18 percent slopes, erodedL62D2135399484fdplmn05320011:12000
Urban land-Kingsley complex, 3 to 15 percent slopes861C957016772841t9bymn12319781:15840
Urban land-Hayden-Kingsley complex, 3 to 15 percent slopes860C635816772821t9bwmn12319781:15840
Kingsley sandy loam, 6 to 12 percent slopes342C185816772381t99gmn12319781:15840
Kingsley sandy loam, 2 to 6 percent slopes342B85216772371t99fmn12319781:15840
Urban land-Hayden-Kingsley complex, 15 to 25 percent slopes860D81516772831t9bxmn12319781:15840
Kingsley sandy loam, 12 to 18 percent slopes342D71516772391t99hmn12319781:15840
Urban land-Kingsley complex, 15 to 25 percent slopes861D61816772851t9bzmn12319781:15840
Mahtomedi-Kingsley complex, 12 to 25 percent slopes896D47616772891t9c3mn12319781:15840
Mahtomedi-Kingsley complex, 3 to 12 percent slopes896C41016772881t9c2mn12319781:15840
Mahtomedi-Kingsley complex, 25 to 40 percent slopes896F28716772901t9c4mn12319781:15840
Kingsley sandy loam, 18 to 30 percent slopes342E12816772401t99jmn12319781:15840
Kingsley, Mahtomedi and Hayden complex, 18 to 25 percent slopesBdE21129427935gc9cmn13919881:20000
Kingsley, Mahtomedi and Hayden complex, 6 to 12 percent slopes, moderately erodedBdC2190427932gc98mn13919881:20000
Kingsley, Mahtomedi and Hayden complex, 12 to 18 percent slopes, moderately erodedBdD2174427934gc9bmn13919881:20000
Kingsley, Mahtomedi and Hayden complex, 12 to 18 percent slopesBdD172427933gc99mn13919881:20000
Kingsley, Mahtomedi and Hayden complex, 2 to 6 percent slopesBdB123427930gc96mn13919881:20000
Kingsley, Mahtomedi and Hayden complex, 6 to 12 percent slopesBdC112427931gc97mn13919881:20000
Kingsley, Mahtomedi and Hayden complex, 25 to 50 percent slopesBdF74427936gc9dmn13919881:20000
Kingsley, Mahtomedi and Hayden complex, 18 to 25 percent slopesBeE362427938gc9gmn13919881:20000
Kingsley, Mahtomedi and Hayden complex, 12 to 18 percent slopes, severely erodedBeD338427937gc9fmn13919881:20000
Kingsley sandy loam, 6 to 12 percent slopes342C611016771031t953mn16319781:15840
Urban land-Kingsley complex, 3 to 15 percent slopes861C353116771491t96lmn16319781:15840
Kingsley sandy loam, 2 to 6 percent slopes342B249116771021t952mn16319781:15840
Kingsley sandy loam, 12 to 18 percent slopes342D213316771041t954mn16319781:15840
Mahtomedi-Kingsley complex, 3 to 12 percent slopes896C117716771531t96qmn16319781:15840
Mahtomedi-Kingsley complex, 12 to 25 percent slopes896D59616771541t96rmn16319781:15840
Urban land-Hayden-Kingsley complex, 3 to 15 percent slopes860C45116771471t96jmn16319781:15840
Kingsley sandy loam, 18 to 30 percent slopes342E25716771051t955mn16319781:15840
Urban land-Hayden-Kingsley complex, 15 to 25 percent slopes860D9116771481t96kmn16319781:15840
Mahtomedi-Kingsley complex, 25 to 40 percent slopes896F9016771551t96smn16319781:15840
Urban land-Kingsley complex, 15 to 25 percent slopes861D4716771501t96mmn16319781:15840
Kingsley-Gotham complex, 6 to 12 percent slopes896C388433784gkd1mn17119981:12000
Kingsley-Gotham complex, 2 to 6 percent slopes896B335433785gkd2mn17119981:12000

Map of Series Extent

Approximate geographic distribution of the KINGSLEY 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 .