Official Series Description


Lab Data Summary

Aggregate lab data for the MIKESELL soil series. This aggregation is based on all pedons with a current taxon name of MIKESELL, 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 MIKESELL 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 MIKESELL 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 MIKESELL 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 MIKESELL 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 MIKESELL 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 flats position figure.

Competing Series

Soil series competing with MIKESELL 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 MIKESELL 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 MIKESELL 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 hills figure.

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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 MIKESELL, 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 MIKESELL 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
Mikesell stony silt loam, 10 to 35 percent slopes43B750119324417802myw3id65020111:24000
Harkness-Sedgway-Mikesell complex, 20 to 50 percent slopes5114136829242s8zid71119831:24000
Toponce-Mikesell-Beaverdam family, complex, 15 to 45 percent slopes8141249127444312stpyid7131:24000
Quietus family-Mikesell-Namela family, very stony surface, complex, 5 to 30 percent slopes1051549429808412x003id7131:24000
Mikesell-Kingmine family, very stony surface, complex, 5 to 40 percent slopes970302529682412wxbrid7131:24000
Mikesell-Herd-Frisco families, complex, 20 to 60 percent slopes375512984239535zid7131:24000
Mikesell family-Vertic Haplocryalfs complex, 20 to 50 percent slopes2351030938825349id7131:24000
Harkness-Sedgway-Mikesell complex, 20 to 50 percent slopesHSG1098600000n4bvid7161:24000
Toponce-Mikesell-Beaverdam family, complex, 15 to 45 percent slopes81418031634522stpyid7161:24000
Mikesell stony silt loam, 10 to 35 percent slopes43B75080725185812qj1pid75819981:24000
Mikesell-Ericson-Odark, stony families, complex, 4 to 15 percent slopes201D444430051172v7zxmt60019691:24000
Nettleton and Mikesell clay loams, hillyNM44111468964xvlmt60019691:24000
Kegsprings family, stony-Mikesell family-Risingwolf, dry complex, 15 to 35 percent slopes253E301430051042x3qvmt60019691:24000
Swifton-Mikesell association, hillySV20341469244xwhmt60019691:24000
Mikesell clay loam, hillyMy16921468934xvhmt60019691:24000
Mikesell family-Worock-Apikuni complex 4 to 15 percent slopes200D73230051022v7zqmt60019691:24000
Worock-Mikesell complex, 15 to 45 percent slopes15936918596734xcqmt60520071:24000
Mikesell clay loam, 15 to 45 percent slopes8018185964220f3gmt60520071:24000
Mikesell family-Worock-Apikuni complex 4 to 15 percent slopes200D1530051272v7zqmt61919881:24000
Mikesell-Tiberlin-Cowood complex, 8 to 70 percent slopes5516F2793231rvxlmt62319881:24000
Worock-Mikesell stony loams, 8 to 35 percent slopes15E37391477084ypsmt63019911:24000
Mikesell stony loam, 8 to 35 percent slopes515E18491478414yv2mt63019911:24000
Mikesell-Swiftcurrent loams, 25 to 60 percent slopes296F9541477774ys0mt63019911:24000
Storm, stony-Mikesell, very stony-Sigbird, extremely stony, 8 to 35 percent slopes6335E530129682302wxbfmt6321:24000
Mikesell, very stony-Gateview families, complex, 25 to 65 percent slopes6237G204028324422v10tmt6321:24000
Mikesell-Ericson-Odark, stony families, complex, 4 to 15 percent slopes201D15929110992v7zxmt6321:24000
Mikesell family-Worock-Apikuni complex 4 to 15 percent slopes200D7429952322v7zqmt6321:24000
Worock-Mikesell complex, 15 to 45 percent slopes159172771464354xcqmt63619831:24000
Mikesell clay loam, 15 to 45 percent slopes80108501465084xg2mt63619831:24000
Mikesell clay loam, 45 to 60 percent slopes8161591465094xg3mt63619831:24000
Whitore-Mikesell, warm-Rock outcrop complex, 25 to 60 percent slopes15421121464304xckmt63619831:24000
Shadow, warm-Mikesell-Worock complex, 45 to 70 percent slopes1259021463984xbjmt63619831:24000
Kegsprings family, stony-Mikesell family-Risingwolf, dry complex, 15 to 35 percent slopes253E1159028482662x3qvmt66320171:24000
Mikesell-Ericson-Odark, stony families, complex, 4 to 15 percent slopes201D779628518412v7zxmt66320171:24000
Mikesell family-Worock-Apikuni complex 4 to 15 percent slopes200D605028518362v7zqmt66320171:24000
Mikesell-Tiberlin-Cowood complex, 8 to 70 percent slopes5516F1483711065rvxlmt6691:24000
Mikesell-Ouselfal families complex, 5 to 15 percent slopesNS371222624960852pv3fut6471:24000
Mikesell-Ouselfal families complex, 15 to 30 percent slopesNS372120024960862pv3gut6471:24000
Toponce-Mikesell-Beaverdam family, complex, 15 to 45 percent slopes81413428586712stpywy62319711:20000
Mikesell-Herd-Frisco families, complex, 20 to 60 percent slopes37573083460535zwy62319711:20000
Mikesell-Herd-Frisco families, complex, 20 to 60 percent slopes3758541152023535zwy66320121:24000
Mikesell family-Vertic Haplocryalfs complex, 20 to 50 percent slopes23557951519715349wy66320121:24000
Mikesell family-Vertic Haplocryalfs complex, 20 to 50 percent slopes23531697055349wy7231:24000

Map of Series Extent

Approximate geographic distribution of the MIKESELL 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 .