Official Series Description


Lab Data Summary

Aggregate lab data for the YERMO soil series. This aggregation is based on all pedons with a current taxon name of YERMO, 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 YERMO 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 YERMO 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 YERMO 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 YERMO 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 YERMO 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 YERMO 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 YERMO 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 YERMO 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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Click the image to view it full size.

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

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Click the image to view it full size.

Soil series sharing subgroup-level classification with YERMO, 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-2010-08-30-08 | Benton-Owens Valley Area, Parts of Inyo and Mono Counties - 2002

    Typical pattern of soils on the eastern side of the Owens Valley and in the Inyo Mountains (Soil Survey of Benton-Owens Valley Area, California, Parts of Inyo and Mono Counties; 2002).

Map Units

Map units containing YERMO 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
YERMO-KIMBERLINA, COOL, ASSOCIATION, SLOPING*17718200463996hktmca67119781:24000
TYPIC HAPLARGIDS-YERMO COMPLEX, 8 TO 30 PERCENT SLOPES*1687500463987hktbca67119781:24000
YERMO GRAVELLY SANDY LOAM, 30 TO 50 PERCENT SLOPES1762600463995hktlca67119781:24000
Yermo stony-Yermo complex, 5 to 15 percent slopes378bo1122300592dvkdca74019961:24000
Yermo stony-Yermo complex, cool, 5 to 15 percent slopes379bo56723908222l7v9ca76319841:24000
Yermo stony-Yermo complex, 5 to 15 percent slopes378bo22423908212l7v8ca76319841:24000
Yermo very gravelly sandy loam, 2 to 5 percent slopes375bo3323908202l7v7ca76319841:24000
Yermo gravelly sandy loam, 30 to 50 percent slopes17675848215xgmsca77719811:24000
Yermo stony-Yermo complex, cool, 5 to 15 percent slopes37911203488341jd4yca80219961:24000
Yermo stony-Yermo complex, 5 to 15 percent slopes3787966488340jd4xca80219961:24000
Yermo very gravelly sandy loam, 2 to 5 percent slopes3756585488337jd4tca80219961:24000
Yermo extremely gravelly sandy loam, 2 to 5 percent slopes3762232488338jd4vca80219961:24000
Yermo stony-Yermo complex, 0 to 5 percent slopes3771876488339jd4wca80219961:24000
Yermo, hot-Yermo-Arizo association2054130951607369nd0knv78519951:24000
Yermo-Greyeagle association221538476469110hr4lnv78519951:24000
Skelon-Yermo-Pinez complex, 0 to 4 percent slopes218124362469100hr48nv78519951:24000
Sanwell-Sanwell, warm-Yermo association245122532469159hr65nv78519951:24000
Yermo-Skelon association223017193469115hr4rnv78519951:24000
Yermo-Commski association205716363469078hr3knv78519951:24000
Yermo-Arizo association221412647469109hr4knv78519951:24000
Yermo-Greyeagle-Arizo association205312292469076hr3hnv78519951:24000
Yermo-Skelon-Pinez complex, 4 to 15 percent slopes218610825469103hr4cnv78519951:24000
Commski-Yermo association239310228469148hr5tnv78519951:24000
Ashmed-Yermo-Niavi association28109293607375nd0rnv78519951:24000
Yermo-Woda-Nowoy association20518049469074hr3fnv78519951:24000
Sanwell-Yermo association21727805469099hr47nv78519951:24000
Yermo-Bullfor association22127578469108hr4jnv78519951:24000
Casaga-Panor-Yermo association21627555469097hr45nv78519951:24000
Shorim-Yermo association22816546469133hr5bnv78519951:24000
Bacho-Yermo association24826158469163hr69nv78519951:24000
Greyeagle-Sanwell-Yermo association22635906469124hr51nv78519951:24000
Sezna-Yermo association28605465469217hr81nv78519951:24000
Greyeagle-Yermo-Strozi association22695051469129hr56nv78519951:24000
Yermo-Arizo complex, 2 to 4 percent slopes22163834469111hr4mnv78519951:24000
Scottcas-Yermo association28503290469216hr80nv78519951:24000
Orwash-Yermo-Arizo association24252653469154hr60nv78519951:24000
Casaga-Woda-Yermo association30222588469236hr8nnv78519951:24000
Bacho-Yermo-Arizo association28802504469219hr83nv78519951:24000
Longjim-Yermo-Dedas association22611846469123hr50nv78519951:24000
Lewdlac-Yermo association24711588469161hr67nv78519951:24000
Skelon-Yermo-Ashmed complex, 4 to 15 percent slopes21851559469102hr4bnv78519951:24000
Yermo-Skelon-Bluepoint association22331394469116hr4snv78519951:24000
Wechech-Nopah-Yermo association4030216469252hr95nv78519951:24000
Yermo-Arizo association83018421485158j8v8nv79619841:63360
Yermo-Arizo-Skelon association8335769485160j8vbnv79619841:63360
Scottcas-Skelon-Yermo association8814777485166j8vjnv79619841:63360
Skelon-Yermo-Arizo association8514212485161j8vcnv79619841:63360
Scottcas-Yermo association8801457485165j8vhnv79619841:63360
Yermo-Skelon association831913485159j8v9nv79619841:63360

Map of Series Extent

Approximate geographic distribution of the YERMO 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 .