Official Series Description


Lab Data Summary

Aggregate lab data for the CORRAL soil series. This aggregation is based on all pedons with a current taxon name of CORRAL, 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 CORRAL 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
2381P0697S1981CA035005CORRAL5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5645981,-120.2404785

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CORRAL 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 CORRAL 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 CORRAL 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 CORRAL 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 CORRAL 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 CORRAL 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 CORRAL 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 CORRAL, 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 CORRAL 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
Corral sandy loam, 5 to 15 percent slopes164su5214689861l9lnca60319741:24000
Bucklake-Corral-Rubble land association, 30 to 50 percent slopes135su514689851l9lmca60319741:24000
Corral very cobbly loam, 5 to 30 percent slopes1669343487433jc6nca60820001:24000
Corral sandy loam, 5 to 15 percent slopes1646174487429jc6jca60820001:24000
Bucklake-Corral-Rubble land association, 30 to 50 percent slopes1353303487381jc4zca60820001:24000
Corral sandy loam, 0 to 2 percent slopes1622166487425jc6dca60820001:24000
Corral-Glenbrook complex, 15 to 50 percent slopes1682081487436jc6rca60820001:24000
Corral loam, 30 to 50 percent slopes165869487431jc6lca60820001:24000
Corral-Chalco complex, 0 to 2 percent slopes167437487435jc6qca60820001:24000
Corral sandy loam, 2 to 5 percent slopes163336487427jc6gca60820001:24000
Corral-Glenbrook complex, 15 to 50 percent slopes16817723268s8m7ca61419671:24000
Bucklake-Rock outcrop-Corral association3292107103473913qqpca68520061:24000
Davey-Corral association120614010474525hxs8nv75919951:24000
Bucklake-Rock outcrop-Corral association10801950474477hxqqnv75919951:24000
Old Camp-Corral association10621300474471hxqjnv75919951:24000
Corral-Mahala association10951200474482hxqwnv75919951:24000
Corral-Celeton-Bedwyr association8301775476675j00mnv77019951:24000
Jaybee-Corral-Oppio association3173382477462j0v0nv77119901:24000
Bucklake-Corral-Rubble land association5111810477497j0w4nv77119901:24000
Buffaran-Corral association5921799477522j0wynv77119901:24000
Verdico-Corral association5801506477518j0wtnv77119901:24000
Corral fine sandy loam, low precipitation, 2 to 15 percent slopes257109616897671tqbmor63520061:24000
Corral fine sandy loam, 2 to 15 percent slopes47C18011489314jf5bor63619911:24000
Corral fine sandy loam, low precipitation, 2 to 15 percent slopes48C13275489315jf5cor63619911:24000

Map of Series Extent

Approximate geographic distribution of the CORRAL 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 .