Official Series Description


Lab Data Summary

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

Competing Series

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

Click the image to view it full size.

Geomorphic description summaries for the INYO 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with INYO, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. CA-2012-05-09-12 | Kern County, Northeastern Part, and Southeastern Part of Tulare County - 2007

    Map units in Short Canyon. Soil formation is affected by erosion from the mountains and deposition onto alluvial fans in map unit 242 (Inyo gravelly loamy coarse sand, 5 to 15 percent slopes) (Soil Survey of Kern County, Northeastern Part, and Southeastern Part of Tulare County, California; 2007).

Map Units

Map units containing INYO 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
Inyo loamy coarse sand, 5 to 15 percent slopes2426721467342hp9kca66820071:24000
Inyo gravelly loamy coarse sand, 0 to 9 percent slopes, occasionally flooded2245648467338hp9fca66820071:24000
Chollawell-Inyo complex, 5 to 15 percent slopes5145491467413hpcvca66820071:24000
Inyo-Kelval complex, 0 to 5 percent slopes, occasionally flooded2854585467377hpbpca66820071:24000
Inyo gravelly loamy coarse sand, 0 to 5 percent slopes2413300467341hp9jca66820071:24000
Inyo-Riverwash complex, 0 to 5 percent slopes, frequently flooded2161689467332hp97ca66820071:24000
Inyo-Urban land complex, 0 to 5 percent slopes44146014212871jpyzca66820071:24000
Inyo-Tips-Rock outcrop complex, 5 to 30 percent slopes247383467346hp9pca66820071:24000
Inyo-Urban land complex, 0 to 9 percent slopes42423714212851jpyxca66820071:24000
Inyo-Kelval-Urban land complex, 0 to 5 percent slopes48519914212931jpz5ca66820071:24000
Inyo-Urban land complex, 0 to 15 percent slopes44218014212881jpz0ca66820071:24000
Inyo-Riverwash complex, 0 to 5 percent slopes, frequently flooded216ne12922180912dg3bca67019771:24000
Inyo loamy coarse sand, 5 to 15 percent slopes36721634186030820fsyca68220071:24000
Chollawell-Inyo complex, 5 to 15 percent slopes4241966186030520fsvca68220071:24000
Inyo-Riverwash complex, 0 to 5 percent slopes, frequently flooded443681186030320fssca68220071:24000
Inyo loamy coarse sand, 0 to 9 percent slopes, occasionally flooded367076186030620fswca68220071:24000
Inyo loamy coarse sand, 0 to 5 percent slopes367168186030720fsxca68220071:24000
Inyo loamy coarse sand, 5 to 15 percent slopes3672nm8723715612klszca76019811:24000
Inyo gravelly loamy coarse sand, 0 to 5 percent slopes241ne3323710142kl7bca76019811:24000
Inyo gravelly loamy coarse sand, 0 to 9 percent slopes, occasionally flooded224ne523710132kl79ca76019811:24000
Inyo-Poleta complex, 0 to 2 percent slopes2242823488145jcymca80219961:24000
Inyo gravelly loamy coarse sand, 0 to 5 percent slopes2232650488143jcykca80219961:24000
Inyo-Westguard association, 0 to 2 percent slopes2251682488147jcypca80219961:24000
Inyo sand, 0 to 9 percent slopes221831488136jcybca80219961:24000
Inyo sand, 9 to 15 percent slopes222298488141jcyhca80219961:24000

Map of Series Extent

Approximate geographic distribution of the INYO 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 .