Official Series Description


Lab Data Summary

Aggregate lab data for the WHITNEY soil series. This aggregation is based on all pedons with a current taxon name of WHITNEY, 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 WHITNEY 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
1787P048987CA019041Whitney7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0086098,-119.9486084
n/a91P089591FN260001Whitney6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties49.6333351,-112.8000031

Water Balance

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

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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with WHITNEY 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 WHITNEY 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 WHITNEY 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 flats position figure.

Soil series sharing subgroup-level classification with WHITNEY, 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 WHITNEY 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
Whitney and Rocklin sandy loams, 3 to 8 percent slopesWrB11174462743hjj6ca64419591:24000
Whitney sandy loams, 15 to 30 percent slopes, erodedWmD26628462740hjj3ca64419591:24000
Whitney sandy loams, 3 to 8 percent slopesWmB4455462736hjhzca64419591:24000
Whitney sandy loams, 8 to 15 percent slopesWmC4160462737hjj0ca64419591:24000
Whitney sandy loams, 8 to 15 percent slopes, erodedWmC23432462738hjj1ca64419591:24000
Whitney sandy loams, 15 to 30 percent slopesWmD2710462739hjj2ca64419591:24000
Whitney and Rocklin sandy loams, 8 to 15 percent slopesWrC1982462744hjj7ca64419591:24000
Whitney and Rocklin sandy loams, 0 to 3 percent slopesWrA847462742hjj5ca64419591:24000
Whitney sandy loams, 30 to 45 percent slopes, erodedWmE2441462741hjj4ca64419591:24000
Whitney and Rocklin soils, 3 to 8 percent slopes, erodedWmB26081463213hk0cca64819591:20000
Whitney fine sandy loam, 15 to 30 percent slopes, erodedWhD24920463207hk05ca64819591:20000
Whitney fine sandy loam, 3 to 8 percent slopesWhB3189463203hk01ca64819591:20000
Whitney fine sandy loam, 8 to 15 percnt slopesWhC3149463205hk03ca64819591:20000
Whitney and Rocklin soils, 8 to 15 percent slopes, erodedWmC21464463214hk0dca64819591:20000
Whitney fine sandy loam, 8 to 15 percent slopes, erodedWhC2907463206hk04ca64819591:20000
Whitney sandy loam, 15 to 30 percent slopes, erodedWkD2758463212hk0bca64819591:20000
Whitney sandy loam, 3 to 8 percent slopesWkB697463209hk07ca64819591:20000
Whitney sandy loam, 8 to 15 percent slopesWkC440463210hk08ca64819591:20000
Whitney fine sandy loam, 30 to 45 percent slopes, erodedWhE2267463208hk06ca64819591:20000
Whitney fine sandy loam, 3 to 8 percent slopes, erodedWhB2159463204hk02ca64819591:20000
Whitney sandy loam, 8 to 15 percent slopes, er0dedWkC291463211hk09ca64819591:20000
Whitney fine sandy loam, 3 to 8 percent slopesWfB7093463550hkc7ca65119591:20000
Whitney and Rocklin sandy loams, 3 to 8 percent slopesWrB6132463557hkcgca65119591:20000
Whitney and Rocklin sandy loams, 8 to 15 percent slopesWrC5288463558hkchca65119591:20000
Whitney-Trigo fine sandy loams, 3 to 8 percent slopesWtB5109463559hkcjca65119591:20000
Cometa-Whitney sandy loams, 3 to 8 percent slopesCwB2075463375hk5lca65119591:20000
Cometa-Whitney sandy loams, 8 to 15 percent slopesCwC1152463376hk5mca65119591:20000
Whitney fine sandy loam, 8 to 15 percent slopesWfC1030463551hkc8ca65119591:20000
Whitney sandy loam, 15 to 30 percent slopes, erodedWnD713463555hkcdca65119591:20000
Whitney and Rocklin gravelly sandy loams, 3 to 15 percent slopeWoC463463556hkcfca65119591:20000
San Joaquin-Whitney sandy loams, 0 to 8 percent slopesScB394463510hk9yca65119591:20000
Whitney loam, 3 to 8 percent slopesWmB87463553hkcbca65119591:20000
Whitney loam, 0 to 3 percent slopesWmA55463552hkc9ca65119591:20000
Whitney loam, 8 to 15 percent slopesWmC19463554hkccca65119591:20000

Map of Series Extent

Approximate geographic distribution of the WHITNEY 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 .