Official Series Description


Lab Data Summary

Aggregate lab data for the SLICKROCK soil series. This aggregation is based on all pedons with a current taxon name of SLICKROCK, 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 SLICKROCK 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
4A75C0073S1975OR039008Slickrock7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.1136894,-124.1209259

Water Balance

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

Competing Series

Soil series competing with SLICKROCK 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 SLICKROCK 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 SLICKROCK 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.

Click the image to view it full size.

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 SLICKROCK, 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 SLICKROCK 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
Preacher-Bohannon-Slickrock complex, 35 to 60 percent slopes13614629854352vwzor00320041:24000
Slickrock gravelly medial loam, 3 to 25 percent slopes1466424854342vwyor00320041:24000
Slickrock gravelly loam, 3 to 25 percent slopes66D13546241022y7or05319771:20000
Slickrock gravelly loam, 25 to 50 percent slopes66E4216241122y8or05319771:20000
Bohannon-Slickrock gravelly loams, dissected, 37 to 50 percent slopesBtF1896914259771jvv8or60119681:20000
Slickrock gravelly loam, 25 to 37 percent slopesSsE1316014260321jvx1or60119681:20000
Bohannon-Slickrock gravelly loams, 35 to 50 percent slopesBsF658714259741jvv5or60119681:20000
Slickrock gravelly loam, dissected, 25 to 37 percent slopesStE646114260341jvx3or60119681:20000
Slickrock gravelly loam, dissected, 37 to 50 percent slopesStF377014260351jvx4or60119681:20000
Slickrock gravelly loam, 37 to 50 percent slopesSsF329014260331jvx2or60119681:20000
Bohannon-Slickrock gravelly loams, dissected, 25 to 37 percent slopesBtE273014259761jvv7or60119681:20000
Bohannon-Slickrock gravelly loams, 25 to 35 percent slopesBsE249214259731jvv4or60119681:20000
Bohannon-Slickrock gravelly loams, dissected, 50 to 75 percent slopesBtG229214259781jvv9or60119681:20000
Slickrock loam, 10 to 25 percent slopesSoD153114260291jvwyor60119681:20000
Slickrock gravelly loam, 0 to 25 percent slopesSsD84814260311jvx0or60119681:20000
Bohannon-Slickrock gravelly loams, 50 to 75 percent slopesBsG67814259751jvv6or60119681:20000
Slickrock loam, dissected, 10 to 25 percent slopesSrD48114260301jvwzor60119681:20000
Slickrock gravelly loam, seeped, 10 to 35 percent slopesSuE30114260361jvx5or60119681:20000
Preacher-Bohannon-Slickrock complex, 50 to 75 percent slopes112G11111862581233ror63719811:20000
Slickrock gravelly loam, 3 to 25 percent slopes124D176862600234cor63719811:20000
Slickrock gravelly loam, 25 to 50 percent slopes124F174862601234dor63719811:20000
Slickrock gravelly medial loam, 3 to 25 percent slopes325E94414215061jq61or63719811:20000
Preacher-Bohannon-Slickrock complex, 35 to 60 percent slopes307F55314214991jq5tor63719811:20000
Preacher-Bohannon-Slickrock complex, 35 to 60 percent slopes50G881646471825bpor63819901:20000
Slickrock gravelly medial loam, 3 to 25 percent slopes325E4514216391jqbbor63819901:20000

Map of Series Extent

Approximate geographic distribution of the SLICKROCK 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 .