Official Series Description


Lab Data Summary

Aggregate lab data for the WHOLAN soil series. This aggregation is based on all pedons with a current taxon name of WHOLAN, 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 WHOLAN were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
2478P014177NV015002Wholan8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6990852,-117.3284302
2482P032881NV015306Wholan8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7882538,-117.3584366
28B83P079183NV015011Wholan7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3283348,-116.6711121

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the WHOLAN series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the WHOLAN series and siblings. 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 WHOLAN 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 .

Click the image to view it full size.

Click the image to view it full size.

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.

Competing Series

Soil series competing with WHOLAN share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the WHOLAN series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the WHOLAN 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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

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 WHOLAN, 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. NV-2012-05-09-14 | Lander County, South Part - November 1991

    General soil map units representative of those on a semibolson that is an externally drained intermontane basin (Soil Survey of Lander County, Nevada, South Part; November 1991).

Map Units

Map units containing WHOLAN 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
Orovada-Roseworth-Wholan complex, 1 to 5 percent slopes11710603485921j9mwid67519921:24000
Wholan silt loam, slightly alkaliWnA2610476195hzj4nv61219681:24000
Wholan silt loam, 0 to 2 percent slopesWlA981476192hzj1nv61219681:24000
Wholan silt loam, overflow, 0 to 2 percent slopesWmA804476194hzj3nv61219681:24000
Wholan silt loam, 2 to 4 percent slopesWlB200476193hzj2nv61219681:24000
Wholan silt loam, 0 to 2 percent slopes7152825474787hy1qnv76019941:24000
Wholan silt loam, rarely flooded, 0 to 2 percent slopes 1/7162224474788hy1rnv76019941:24000
McConnel-Rasille-Wholan association63342315479287j2qwnv76819851:63360
Orovada-Rasille-Wholan association70028985479297j2r6nv76819851:63360
Wholan-Rasille association, nonalkaline117817740479046j2h3nv76819851:63360
Creemon-Wholan association29112460479163j2lwnv76819851:63360
Rotinom-Wholan association202194604790892whmsnv76819851:63360
McConnel-Wholan association6384220479291j2r0nv76819851:63360
Wholan-Rasille association, alkaline11773125479045j2h2nv76819851:63360
Wholan silt loam, alkaline11731420479044j2h1nv76819851:63360
Wholan very fine sandy loam, rarely flooded, 0 to 2 percent slopes102011410475169hyg1nv76919861:24000
Knott-Sodhouse-Wholan association123054114751932whlynv76919861:24000
Hessing-Wholan-Dun Glen association47011495476593hzxznv77019951:24000
Slaw-Juva-Wholan association3409111476548hzwjnv77019951:24000
Pineval-Rebel-Wholan association4916215476602hzy8nv77019951:24000
Wholan-Defler association4505832476590hzxwnv77019951:24000
Juva-Wholan-Stumble association4605361476591hzxxnv77019951:24000
Watoopah-Buckaroo-Wholan association2413866476508hzv7nv77019951:24000
Rebel-Wholan-Pineval association5923189476628hzz3nv77019951:24000
Buckaroo-Celeton-Wholan association1582512476453hzsgnv77019951:24000
Wholan silt loam11705392479429j2wgnv77519851:24000
Wholan, strongly alkaline-Rasille association11773885479431j2wjnv77519851:24000
Wholan-Rasille association11782665479432j2wknv77519851:24000
Wholan silt loam, sandy substratum1174510479430j2whnv77519851:24000
Wholan-Clowfin association1013174479760j374nv77619831:63360
Wholan silt loam, cool, occasionally flooded*100521479758j372nv77619831:63360
Knott-Sodhouse-Wholan association1230111574754572whlynv77719931:24000
Wholan-Bliss-Enko association10237206475363hyn9nv77719931:24000
Wholan silt loam, 0 to 2 percent slopes 1/10253140475365hyncnv77719931:24000
Weso-Wholan complex16211934475589hywlnv77719931:24000
Wholan very fine sandy loam, 0 to 2 percent slopes10201042475361hyn7nv77719931:24000
Rotinom-Wholan association22303954808582whmsnv78119941:24000

Map of Series Extent

Approximate geographic distribution of the WHOLAN 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 .