Official Series Description


Lab Data Summary

Aggregate lab data for the SKYLICK soil series. This aggregation is based on all pedons with a current taxon name of SKYLICK, 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 SKYLICK 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
4770C0032S1970UT039008Skylick7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5541649,-111.3416672

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SKYLICK 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 SKYLICK 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 SKYLICK 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 SKYLICK 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 SKYLICK 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 SKYLICK 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 SKYLICK 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 SKYLICK, 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 SKYLICK 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
Skylick loam, 15 to 35 percent slopes214909509308k2z9co6471:24000
Northwater-Skylick loams, 3 to 15 percent slopes253386509317k2zlco6471:24000
Callings-Skylick families complex, 5 to 40 percent slopes347B764214149671jhd3co6541:24000
Anvik-Skylick-Sawpit families complex, 5 to 40 percent slopes452B386114150301jhg4co6541:24000
Anvik-Skylick-Sligting association, 25 to 50 percent slopesAG11228114150751jhhlco6541:24000
Anvik-Skylick-Sligting association, 10 to 25 percent slopesAG1052514150741jhhkco6541:24000
Anvik-Skylick-Sligting association, 25 to 50 percent slopes1130135497939jq4kco65519841:24000
Anvik-Skylick-Sligting association, 10 to 25 percent slopes1015776497928jq46co65519841:24000
Callings-Skylick families complex, 5 to 40 percent slopes347B18731769551jhd3co66119681:31680
Dromedary, very stony-Skylick complex, 10 to 60 percent slopesELE119314245911jtdkut0131:24000
Skylick-Hoodle association, 15 to 50 percent slopes8111463481294j4tmut60119851:24000
Skylick sandy loam, 8 to 30 percent slopes675932504564jy18ut62419851:24000
Mortenson-Skylick association, very steepMKG4170482293j5vvut62719711:24000
Skylick silt loam, 30 to 70 percent slopesSSF3460482346j5xkut62719711:24000
Skylick silt loam, 4 to 30 percent slopesSSD900482345j5xjut62719711:24000
Skylick loam, 5 to 30 percent slopes8310255554081vncut63319831:24000
Lucky Star-Skylick families complex, 30 to 60 percent slopes560331288430gwyut6451:24000
Skylick-Roundy families complex, 5 to 40 percent slopes561C331288830gx2ut6451:24000
Skylick-Adel-Clayburn families complex, 15 to 60 percent slopesmt4815918331484030hl3ut6451:24000
Deer Creek-Skylick families complex, 20 to 50 percent slopes253B3360331285330gvxut6451:24000

Map of Series Extent

Approximate geographic distribution of the SKYLICK 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 .