Official Series Description


Lab Data Summary

Aggregate lab data for the SPROULISH soil series. This aggregation is based on all pedons with a current taxon name of SPROULISH, 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 SPROULISH 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
505N013104CA601271Sproulish6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0630556,-123.8519444
505N0133S2004CA023011Sproulish6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0811119,-123.9175034

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SPROULISH 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 SPROULISH 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 SPROULISH 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 SPROULISH 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 SPROULISH 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 SPROULISH 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 SPROULISH 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 SPROULISH, 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 SPROULISH 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
Canoecreek-Sproulish-Redwohly complex, 50 to 75 percent slopes, warm5751064424304392ml28ca60020171:24000
Sproulish-Canoecreek-Redwohly complex, 30 to 50 percent slopes, warm574900324304382ml27ca60020171:24000
Sproulish-Canoecreek-Redwohly complex, 30 to 50 percent slopes571374427476741v5vxca60020171:24000
Crazycoyote-Sproulish-Caperidge complex, 15 to 50 percent slopes567237118566031lpq2ca60020171:24000
Canoecreek-Sproulish-Redwohly complex, 50 to 75 percent slopes57295327476751v5w0ca60020171:24000
Sproulish-Canoecreek-Redwohly complex, 15 to 30 percent slopes57085427476731v5vwca60020171:24000
Sproulish-Canoecreek-Redwohly complex, 15 to 30 percent slopes, warm57358927476761v5w1ca60020171:24000
Sproulish-Canoecreek-Redwohly complex, 30 to 50 percent slopes, warm5745410917037312ml27ca60120111:24000
Canoecreek-Sproulish-Redwohly complex, 50 to 75 percent slopes, warm5754998017037272ml28ca60120111:24000
Crazycoyote-Sproulish-Canoecreek complex, 30 to 50 percent slopes55052361024279652mhhgca60120111:24000
Crazycoyote-Sproulish-Canoecreek complex, 50 to 75 percent slopes55061863924279682mhhkca60120111:24000
Sproulish-Canoecreek-Redwohly complex, 30 to 50 percent slopes5711750817037261v5vxca60120111:24000
Sproulish-Canoecreek-Redwohly complex, 15 to 30 percent slopes, warm5731278717037301v5w1ca60120111:24000
Canoecreek-Coyoterock-Sproulish complex, 15 to 50 percent slopes55081201825150252qds2ca60120111:24000
Sproulish-Canoecreek-Redwohly complex, 15 to 30 percent slopes5701073817037251v5vwca60120111:24000
Crazycoyote-Sproulish-Caperidge complex, 15 to 50 percent slopes5671050514806241lpq2ca60120111:24000
Sproulish-Gibsoncreek-Redwohly complex, 50 to 75 percent slopes5796957115146117n5xca60120111:24000
Canoecreek-Sproulish-Redwohly complex, 50 to 75 percent slopes572604617037291v5w0ca60120111:24000
Sproulish-Telegraph-Redwohly complex, 30 to 50 percent slopes5785676115146217n5yca60120111:24000
Gibsoncreek-Sproulish-Redwohly complex, 30 to 50 percent slopes5764684190639321zrkca60120111:24000
Redwohly-Gibsoncreek-Sproulish complex, 15 to 30 percent slopes5771587115146317n5zca60120111:24000
Canoecreek-Sproulish-Kingrange complex, 50 to 75 percent slopes550366924279212mhg1ca60120111:24000
Canoecreek-Kingrange-Sproulish complex, 15 to 50 percent slopes550244224279202mhg0ca60120111:24000
Gibsoncreek-Sproulish-Redwohly complex, 30 to 50 percent slopes576sh12633249549821zrkca69419931:24000
Redwohly-Gibsoncreek-Sproulish complex, 15 to 30 percent slopes577sh4229249549517n5zca69419931:24000
Canoecreek-Sproulish-Redwohly complex, 50 to 75 percent slopes, warm575sh132926004852ml28ca69419931:24000
Sproulish-Canoecreek-Redwohly complex, 30 to 50 percent slopes, warm574sh57324954972ml27ca69419931:24000
Sproulish-Gibsoncreek-Redwohly complex, 50 to 75 percent slopes579sh105249549917n5xca69419931:24000

Map of Series Extent

Approximate geographic distribution of the SPROULISH 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 .