Official Series Description


Lab Data Summary

Aggregate lab data for the SKUTUM soil series. This aggregation is based on all pedons with a current taxon name of SKUTUM, 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 SKUTUM 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 SKUTUM 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 SKUTUM 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 SKUTUM 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 SKUTUM 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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Competing Series

Soil series competing with SKUTUM 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 SKUTUM 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 SKUTUM 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 terrace figure.

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

Soil series sharing subgroup-level classification with SKUTUM, 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 SKUTUM 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
Skutum fine sandy loam, 5 to 20 percent slopes353040498400jqmfco63519791:24000
Mancos-Skisams-Skutum complex, 1 to 15 percent slopes5717341507201k0sbco67220031:24000
Primeaux-Goodski-Skutum families, complex, 20 to 50 percent slopes8401757427334502slrmid7131:24000
Faim-Skutum family, very deep, complex, 10 to 45 percent slopes820593727334302slqtid7131:24000
Broad Canyon-Skutum family, high effective precipitation, complex, 15 to 45 percent slopes850194627334602slryid7131:24000
Northorn family-Pontuge-Skutum family, complex, 25 to 60 percent slopes950132929638622wv2kid7131:24000
Cavemountain-Bischoff familly-Skutum family, complex, 25 to 60 percent slopes954114129638602wv2mid7131:24000
Faim-Skutum family, very deep, complex, 10 to 45 percent slopes8208131634312slqtid7161:24000
Primeaux-Goodski-Skutum families, complex, 20 to 50 percent slopes8404628586462slrmid75819981:24000
Monaberg, very stony-Kimpton, stony-Skutum families, complex, 2 to 153150D32227246382sh7ymt6321:24000
Agassiz-Skutum-Lizzant complex, 25 to 70 percent slopesDRG1979528102622trdnut0131:24000
Skutum loam, 15 to 30 percent slopes17025350508214k1v0ut61319991:24000
Ant Flat-Henefer-Skutum complex, 8 to 30 percent slopes10522890508145k1rsut61319991:24000
Skutum loam, 30 to 60 percent slopes17119131508213k1tzut61319991:24000
Skutum-Uinta association, 15 to 30 percent slopes17213122508212k1tyut61319991:24000
Skutum loam, 2 to 15 percent slopes1697810508215k1v1ut61319991:24000
Skutum-Uinta association, 30 to 60 percent slopes1737062508217k1v3ut61319991:24000
Sessions-Skutum loams, 2 to 15 percent slopes1674345508209k1tvut61319991:24000
Sevier-Skutum association, 5 to 35 percent slopes1293887504358jxtmut63619841:24000
Skutum fine sandy loam, 10 to 35 percent slopes1353050504365jxtvut63619841:24000
Skutum very fine sandy loam, 1 to 6 percent slopes1341783504364jxttut63619841:24000
Whiteman-Skutum association, 10 to 70 percent slopes1591510504391jxvput63619841:24000
Skutum-Routt, extremely stony families, complex, 3 to 25 percent slopes1503718791193vk9cut6511:24000
Faim-Skutum family, very deep, complex, 10 to 45 percent slopes82046128586632slqtwy62319711:20000
Northorn family-Pontuge-Skutum family, complex, 25 to 60 percent slopes9501430834872wv2kwy62319711:20000

Map of Series Extent

Approximate geographic distribution of the SKUTUM 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 .