Official Series Description


Lab Data Summary

Aggregate lab data for the VALMY soil series. This aggregation is based on all pedons with a current taxon name of VALMY, 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 VALMY 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
2440A3178S1961NV013002Valmy5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5634918,-117.8437576
2440A3181S1966NV013002VALMY7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0076675,-117.7051315

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the VALMY 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 VALMY 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 VALMY 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 VALMY 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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Competing Series

Soil series competing with VALMY 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 VALMY 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 VALMY 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 mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with VALMY, 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 VALMY 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
Valmy fine sandy loam, 2 to 8 percent slopes5821433103460513qlcca68520061:24000
Valmy-Langston-Paypoint association11411490474493hxr7nv75919951:24000
Valmy very fine sandy loam, 0 to 2 percent slopes1140350474492hxr6nv75919951:24000
Valmy very fine sandy loam, 0 to 2 percent slopes 1/7904601474800hy24nv76019941:24000
Valmy-Enko association59011408475061hybknv76519861:24000
Devilsgait-Valmy association4835400475045hyb1nv76519861:24000
Xipe-Valmy-Ocala association3403260475004hy8qnv76519861:24000
Valmy-Luap association5852880475060hybjnv76519861:24000
Ixian-Valmy association30012150474976hy7tnv76519861:24000
Valmy-Enko association2113294478262j1ntnv76619941:24000
Wendane-Sonoma-Valmy association11469115479041j2gynv76819851:63360
Orovada-Valmy association7052110479302j2rcnv76819851:63360
Batan-Wendane-Valmy association81310091475315hylrnv76919861:24000
Shabliss-Enko-Valmy association1707062475237hyj7nv76919861:24000
Bubus-Valmy association9316364475330hym7nv76919861:24000
Valmy fine sandy loam, 0 to 2 percent slopes600825475288hykwnv76919861:24000
Wendane-Sonoma-Valmy association11461955479419j2w4nv77519851:24000
Batan-Wendane-Valmy association1671675479490j2yfnv77519851:24000
Valmy fine sandy loam, 0 to 2 percent slopes 1/60022894475822hz43nv77719931:24000
Valmy-Bubus-Needle Peak complex, 0 to 2 percent slopes60413726475826hz47nv77719931:24000
Valmy-Goldrun complex, 0 to 8 percent slopes 1/6036828475825hz46nv77719931:24000
Preble-Valmy association4363285475730hz14nv77719931:24000
Valmy loam, 0 to 2 percent slopes 1/6061486475828hz49nv77719931:24000
Shabliss-Enko-Valmy association532683475776hz2mnv77719931:24000
Valmy-Bubus ashy very fine sandy loams, 0 to 4 percent slopes38323432708652v4z5nv77719931:24000
Tenply-Loveboldt complex, 0 to 2 percent slopes2821081023931862lb9kor64420211:24000
Valmy ashy loam, 2 to 8 percent slopes387180728446522v4znor64420211:24000
Bubus-Tenply-Loveboldt complex, 0 to 4 percent slopes230158024838832pcp8or64420211:24000
Valmy-Bubus ashy very fine sandy loams, 0 to 4 percent slopes383142628446372v4z5or64420211:24000
Outerkirk-Valmy ashy sandy loams, 0 to 15 percent slopes34026224874752phf4or64420211:24000

Map of Series Extent

Approximate geographic distribution of the VALMY 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 .