Official Series Description


Lab Data Summary

Aggregate lab data for the WARDBAY soil series. This aggregation is based on all pedons with a current taxon name of WARDBAY, 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 WARDBAY 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
28B89P057189NV007006Wardbay7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1394463,-114.8916702

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WARDBAY 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 WARDBAY 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 WARDBAY 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 WARDBAY 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 WARDBAY 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 WARDBAY 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 WARDBAY 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 hills figure.

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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 WARDBAY, 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-2012-05-09-27 | Western White Pine County Area, Parts of White Pine and Eureka Counties - 1998

    The location of individual map unit components on a bolson landscape (Soil Survey of Western White Pine County Area, Nevada, Parts of White Pine and Eureka Counties; 1998).

Map Units

Map units containing WARDBAY 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
Wardbay-Adobe-Haunchee association MLRA 28B1374347226340062wbknnv62119711:24000
Wardbay-Hardol-Adobe association137265426340052rhhxnv62119711:24000
Wardbay-Canyoung-Rock outcrop association5140129724061202lrrsnv70820091:24000
Wardbay-Haunchee-Bakerpeak association524091024061242lrrxnv70820091:24000
Wardbay-Basinpeak association532036024061372lrsbnv70820091:24000
Canyoung-Zarark-Wardbay association510235024098172lwm1nv70820091:24000
Wardbay-Haunchee-Muiral association420028124061172lrrpnv70820091:24000
Wardbay-Haunchee-Muiral association4200216624061622lrt4nv70920121:24000
Wardbay-Zarark-Bakerpeak association5240185924061692tzggnv70920121:24000
Wardbay-Canyoung-Rock outcrop association514064924061652lrt7nv70920121:24000
Canyoung-Zarark-Wardbay association51026925157452tzgfnv70920121:24000
Wardbay-Haunchee-Lorgana association13702026125898452t6grnv76420211:24000
Halacan-Wardbay-Haunchee association3070699727728302t6wcnv76420211:24000
Haunchee-Halacan-Wardbay association1181384232708392zzg3nv76420211:24000
Wardbay-Adobe-Haunchee association MLRA 28B530272504783702wbknnv76619941:24000
Haunchee-Halacan-Wardbay association118126417478597j20mnv76619941:24000
Adobe-Wardbay-Hardol association51118586478367j1s6nv76619941:24000
Adobe-Wardbay-Haunchee association115013495478588j20bnv76619941:24000
Hardzem-Haunchee-Wardbay, cool association12308777478612j213nv76619941:24000
Pookaloo-Tecomar-Wardbay association16315685478675j234nv76619941:24000
Haunchee-Muiral-Wardbay association mlra 28b52046904783692wbhvnv76619941:24000
Adobe-Cavehill-Wardbay association5124332478368j1s7nv76619941:24000
Hardol-Rock outcrop-Wardbay association12013912478604j20vnv76619941:24000
Haunchee-Halacan-Wardbay association118116832708982w2t7nv76719861:24000
Haunchee-Wardbay-Hardzem association11742404422156142dcjfnv77820131:24000
Wardbay-Zarark-Bakerpeak association52401590122157442dcnmnv77820131:24000
Wardbay-Successloop-Haunchee association1378799122158362dcrlnv77820131:24000
Zarark-Wardbay-Amelar association4561794625708312qzp6nv77820131:24000
Muiral-Piar-Wardbay association4322643222158402dcrqnv77820131:24000
Cavemountain-Wardbay-Halacan association5322620024856272pfhjnv77820131:24000
Zarark-Wardbay-Grink association4362562022158462dcrxnv77820131:24000
Wardbay-Zarark-Successloop association4360532522158452dcrwnv77820131:24000
Halacan-Adobe-Wardbay association4574456325898322r359nv77820131:24000
Wardbay-Adobe-Zarark association1374418222156382dck6nv77820131:24000
Hardzem-Haunchee-Wardbay association mlra 28b1430138322156472t6gsnv77820131:24000
Adobe-Zarark-Wardbay association336228122156942dcm0nv77820131:24000
Halacan-Wardbay-Haunchee association307010539480007j3h3nv77920041:24000
Haunchee-Muiral-Wardbay association34504636480079j3kfnv77920041:24000
Muiral-Haunchee-Wardbay association33682232480063j3jxnv77920041:24000
Haunchee-Wardbay-Rock outcrop association33642191480061j3jvnv77920041:24000
Wardbay-Halacan-Haunchee association11611023479940j3dynv77920041:24000
Adobe-Haunchee-Wardbay association3362989480060j3jtnv77920041:24000
Wardbay-Haunchee-Muiral association1162704479941j3dznv77920041:24000
Wardbay-Hardol-Adobe association1160553479939j3dxnv77920041:24000
Hardzem-Haunchee-Wardbay association3385275749226t4mlnv77920041:24000
Wardbay-Hardol-Adobe association137229931480248j3qwnv78019901:24000
Hardzem-Haunchee-Wardbay association mlra 28b1430298124802682t6gsnv78019901:24000
Wardbay-Adobe-Haunchee association MLRA 28B1374119664802502wbknnv78019901:24000
Wardbay-Haunchee-Hardol association137010049480246j3qtnv78019901:24000
Haunchee-Wardbay-Hardzem association11748876480182j3nrnv78019901:24000
Haunchee-Muiral-Wardbay association mlra 28b155052574802902wbhvnv78019901:24000
Zark-Wardbay-Grink association43629828172652tzjcnv78019901:24000
Wardbay-Zarak-Successloop association43603628172642tzjbnv78019901:24000
Haunchee-Wardbay-Hardzem association11728481139j4nmnv78420061:24000
Halacan-Wardbay-Haunchee association78191213897141hn3hut61119921:24000

Map of Series Extent

Approximate geographic distribution of the WARDBAY 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 .