Official Series Description


Lab Data Summary

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

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 SCISM 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 SCISM series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the SCISM 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

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 SCISM, 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 SCISM 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
Scism silt loam, bedrock substratum, 2 to 4 percent slopes164977725191182q7tid00120121:24000
Scism silt loam, bedrock substratum, 0 to 2 percent slopes163605825191172q7sid00120121:24000
Dolman-Minveno-Scism complex, 0 to 8 percent slopes4113587425192362prhyid00120121:24000
Scism silt loam, 0 to 2 percent slopes160424225191142q7pid00120121:24000
Scism silt loam, bedrock substratum, 4 to 8 percent slopes165386025191192q7vid00120121:24000
Scism silt loam, 2 to 4 percent slopes161259125191152q7qid00120121:24000
Tadpole-Scism complex, 8 to 20 percent slopes4009117925192222prhhid00120121:24000
Scism silt loam, 4 to 8 percent slopes16259225191162q7rid00120121:24000
Scism silt loam, bedrock substratum, 8 to 12 percent slopes16648825191202q7wid00120121:24000
Scism silt loam, 0 to 1 percent slopesScA8394808552q47id66519671:20000
Scism silt loam, 1 to 3 percent slopesScB7052808562q48id66519671:20000
Minidoka-Scism silt loams, 3 to 7 percent slopesMnC6468808052q2mid66519671:20000
Scism silt loam, 3 to 7 percent slopesScC5107808572q49id66519671:20000
Scism silt loam, deep over basalt, 3 to 7 percent slopesSdC3992808612q4fid66519671:20000
Scism silt loam, deep over basalt, 1 to 3 percent slopesSdB3735808602q4did66519671:20000
Minidoka-Scism silt loams, 7 to 12 percent slopesMnD1200808062q2nid66519671:20000
Scism silt loam, 7 to 12 percent slopesScD838808582q4bid66519671:20000
Scism silt loam, deep over basalt, 7 to 12 percent slopesSdD429808622q4gid66519671:20000
Scism silt loam, deep over basalt, 0 to 1 percent slopesSdA418808592q4cid66519671:20000
Scism very fine sandy loam, 1 to 12 percent slopes14819470485987j9q0id67519921:24000
Scism silt loam, 5 to 20 percent slopes14710293485989j9q2id67519921:24000
Hardtrigger-Scism complex, 1 to 5 percent slopes747370486261j9zvid67519921:24000
Scism-Coonskin complex, 1 to 20 percent slopes1496954485991j9q4id67519921:24000
Scism silt loam, 0 to 4 percent slopes1411906725195002qybid68520121:24000
Tadpole-Scism complex, 8 to 20 percent slopes40095725196402prhhid68520121:24000

Map of Series Extent

Approximate geographic distribution of the SCISM 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 .