Official Series Description


Lab Data Summary

Aggregate lab data for the STURKIE soil series. This aggregation is based on all pedons with a current taxon name of STURKIE, 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 STURKIE 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
115BM90053761990MO053076Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8645833,-93.0422778
115BM90053771990MO053077Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9216944,-93.0135278
115BM90099021990MO099002Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672644,-92.3451678
115BM91167231991MO167148Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672222,-92.345
115BM94051031993MO051018Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.574492,-92.4351697
116AM93167091989MO167072Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7188889,-93.2261111
116AM90141041990MO141004Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6494444,-92.9229444
116AM94099271994MO099234Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.272832,-90.6453898
116AM97131171997MO131052Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2115848,-92.5313823
116AM98055341998MO055034Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0215547,-91.2032496
116AM99055051999MO055005Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0387124,-91.1219298
116AM99055111999MO055011Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0906936,-91.152185
116AM99131211999MO131020Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2749308,-92.4180788
116AM99131201999MO131021Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2731222,-92.4168357
116AM00221102000MO221273Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0992667,-90.70005
116AM07035512007MO035051Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8893889,-90.9089444
116A80P036778AR049002Sturkie1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.3474998,-91.6936111
116BM90057651990MO057065Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3666667,-93.8241667
116BM92057331992MO057033Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4241389,-93.7707722
116BM92057351992MO057035Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4224611,-93.7739417
116BM92057861992MO057086Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4032667,-93.8069056
116BM92057871992MO057087Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4013583,-93.8037111
116BM92167231992MO167312Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.458675,-93.4693056
116BM93057041993MO057006Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3819444,-93.8127778
116BM96039041995MO039066Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6377139,-93.9224914
116CM97221641997MO221127Sturkie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7621012,-90.8731979

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the STURKIE 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 STURKIE 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 STURKIE 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 STURKIE 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 STURKIE 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 STURKIE 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 STURKIE 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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Click the image to view it full size.

Soil series sharing subgroup-level classification with STURKIE, 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 STURKIE 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
Sturkie fine sandy loamSt1838522958kk5mal07119431:24000
Sturkie silt loam, 0 to 3 percent slopes, frequently flooded321604928046022wj9war04919791:20000
Sturkie silt loam, 0 to 3 percent slopes, frequently flooded597235657822wj9war06319801:20000
Sturkie silt loam, 1 to 3 percent slopes, occasionally flooded312464285627730m06ar06519791:20000
Sturkie silt loam, 0 to 3 percent slopes, frequently flooded32208628562802wj9war06519791:20000
Sturkie silt loam, 0 to 3 percent slopes, frequently flooded27102085645752wj9war13519811:20000
Sturkie silt loam, 0 to 3 percent slopes461771566440m0f8ar13719811:20000
Sturkie silt loam, 0 to 2 percent slopes, frequently flooded753785925364032qpzzmo01519861:24000
Sturkie silt loam, 0 to 2 percent slopes, frequently flooded75378179825364122qpzzmo02919881:24000
Sturkie silt loam, 0 to 2 percent slopes, frequently flooded753781111425364042qpzzmo03920011:24000
Sturkie silt loam, 1 to 3 percent slopes, frequently flooded7637844126730472rt1tmo03920011:24000
Sturkie silt loam, 0 to 2 percent slopes, frequently flooded75378157525364132qpzzmo05319931:24000
Sturkie silt loam, 0 to 2 percent slopes, occasionally flooded7545386225028612q29jmo05520031:24000
Sturkie silt loam, 0 to 2 percent slopes, frequently flooded75378600225364112qpzzmo05719961:24000
Sturkie silt loam, 0 to 2 percent slopes, frequently flooded75378217925364092qpzzmo07719791:24000
Sturkie silt loam, 0 to 2 percent slopes, frequently flooded7537869825364052qpzzmo08519881:24000
Sturkie silt loam, 0 to 2 percent slopes, occasionally flooded75453253325028622q29jmo09920001:24000
Sturkie silt loam, 0 to 2 percent slopes, frequently flooded7537849625364102qpzzmo10919791:24000
Sturkie silt loam, 0 to 2 percent slopes, frequently flooded75378147425364142qpzzmo13120011:24000
Sturkie silt loam, 0 to 2 percent slopes, occasionally flooded7545372725028632q29jmo13120011:24000
Sturkie silt loam, 0 to 2 percent slopes, frequently flooded753781342125364152qpzzmo13519621:24000
Sturkie silt loam, 1 to 3 percent slopes, frequently flooded76378568526882582rt1tmo13519621:24000
Sturkie silt loam, 0 to 2 percent slopes, frequently flooded75378652725364162qpzzmo14119961:24000
Sturkie silt loam, 0 to 2 percent slopes, frequently flooded7537864925364062qpzzmo15919901:24000
Sturkie silt loam, 0 to 2 percent slopes, frequently flooded753781101125364072qpzzmo16719931:24000
Sturkie silt loam, 0 to 2 percent slopes, frequently flooded75378485925364022qpzzmo16919841:24000
Sturkie silt loam, 0 to 2 percent slopes, frequently flooded75378148525364082qpzzmo18519841:24000
Sturkie silt loam, 1 to 3 percent slopes, frequently flooded763788825799122rt1tmo18519841:24000
Sturkie silt loam, 0 to 2 percent slopes, occasionally flooded754533425028652q29jmo18619821:24000
Sturkie silt loam, 0 to 2 percent slopes, occasionally flooded75453225028642q29jmo18719791:24000
Sturkie silt loam, 0 to 2 percent slopes, occasionally flooded7545335125028662q29jmo22120031:24000

Map of Series Extent

Approximate geographic distribution of the STURKIE 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 .