Official Series Description


Lab Data Summary

Aggregate lab data for the WYOMING soil series. This aggregation is based on all pedons with a current taxon name of WYOMING, 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 WYOMING 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
13963PA0850071963PA085007Wyoming4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2136111,-80.0313889
13965PA0390121965PA039012Wyoming4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8383333,-80.0641667
14085PA0890241985PA089024Wyoming4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0358333,-75.3644444

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WYOMING 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 WYOMING 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 WYOMING 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 WYOMING 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 WYOMING 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 WYOMING 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 WYOMING 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 flats position figure.

Soil series sharing subgroup-level classification with WYOMING, 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. PA-2010-09-30-06 | Clinton County - 2007

    Typical pattern of soils and parent material throughout the Susquehanna Lowland Section (Soil Survey of Clinton County, Pennsylvania; 2007).

  2. PA-2012-03-12-23 | Bradford and Sullivan Counties - August 1986

    Typical pattern of soils and parent material in the Morris-Oquaga-Wellsboro map unit (Soil Survey of Bradford and Sullivan Counties, PA; 1986).

  3. PA-2012-03-13-45 | Lackawanna and Wyoming Counties - March 1982

    Typical pattern of soils and underlying material in the Oquaga-Lackawanna-Arnot association (Soil Survey of Lackawanna and Wyoming Counties, PA; 1982).

  4. PA-2012-03-13-47 | Lackawanna and Wyoming Counties - March 1982

    Typical pattern of soils and underlying material in the Wyoming-Pope association (Soil Survey of Lackawanna and Wyoming Counties, PA; 1982).

  5. PA-2012-03-13-55 | Luzerne County - October 1981

    Typical pattern of soils and underlying material in association 4 (Soil Survey of Luzerne County, PA; 1981).

  6. PA-2012-03-13-70 | Monroe County - August 1981

    Typical pattern of soils and underlying material in the Wyoming-Chenango-Pope map unit (Soil Survey of Monroe County, PA; 1981).

  7. PA-2012-03-14-08 | Northumberland County - March 1985

    Typical pattern of soils and underlying material in the Holly-Basher-Wheeling association (Soil Survey of Northumberland County, PA; 1985).

  8. PA-2012-03-14-24 | Union County - March 1985

    Typical pattern of soils and underlying material in the Holly-Basher-Monongahela association (Soil Survey of Union County, PA; 1985).

  9. PA-2012-03-14-33 | Wayne County - September 1985

    Typical pattern of soils and underlying material in the Holly-Basher-Wyoming association (Soil Survey of Wayne County, PA; 1985).

Map Units

Map units containing WYOMING 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
Wyoming gravelly sandy loam, rarely flooded, 0 to 5 percent slopesWyA1119538361l26hpa02719751:20000
Wyoming very gravelly loam, 0 to 3 percent slopesWyA2275544136l86spa03520021:24000
Wyoming very gravelly loam, 3 to 8 percent slopesWyB857544137l86tpa03520021:24000
Wyoming gravelly sandy loam, 3 to 8 percentWyB50552962089y73pa03919731:20000
Wyoming gravelly sandy loam, 8 to 15 percent slopesWyC41772962099y74pa03919731:20000
Wyoming gravelly sandy loam, 15 to 25 percent slopesWyD27522962109y75pa03919731:20000
Wyoming gravelly sandy loam, 0 to 3 percent slopesWyA15142962079y72pa03919731:20000
Wyoming gravelly sandy loam, 3 to 8 percent slopesWyB1642299367b1j0pa06919761:20000
Wyoming gravelly sandy loam, 8 to 15 percent slopesWyC793299368b1j1pa06919761:20000
Wyoming gravelly sandy loam, 15 to 25 percent slopesWyD684299369b1j2pa06919761:20000
Wyoming gravelly sandy loam, 0 to 3 percent slopesWyA428299366b1hzpa06919761:20000
Wyoming gravelly sandy loam, 25 to 45 percent slopesWyE255299370b1j3pa06919761:20000
Wyoming gravelly loam, 15 to 25 percent slopesWyD27852965059yjppa07919741:20000
Wyoming gravelly loam, 25 to 60 percent slopesWyF25272965069yjqpa07919741:20000
Wyoming gravelly sandy loam, occasionally floodedWy2581539147l30vpa08119811:20000
Wyoming gravelly sandy loam, 8 to 15 percent slopesWyC51542963879ydwpa08919751:20000
Wyoming gravelly sandy loam, 3 to 8 percent slopesWyB40922963869ydvpa08919751:20000
Wyoming gravelly sandy loam, 25 to 70 percent slopesWyE23562963899ydypa08919751:20000
Wyoming gravelly sandy loam, 15 to 25 percent slopesWyD19892963889ydxpa08919751:20000
Wyoming gravelly sandy loam, 0 to 3 percent slopesWyA19132963859ydtpa08919751:20000
Craigsville-Wyoming complex, 0 to 8 percent slopes, extremely stony9B242963939yf2pa08919751:20000
Wyoming gravelly sandy loam, 0 to 3 percent slopesWyA66539038l2xbpa09319801:20000
Wyoming gravelly sandy loam, 3 to 8 percent slopesWyB39539039l2xcpa09319801:20000
Wyoming gravelly sandy loam, 0 to 3 percent slopesWyA632539687l3l8pa09719801:20000
Wyoming gravelly sandy loam, 3 to 8 percent slopesWyB500539688l3l9pa09719801:20000
Wyoming very cobbly sandy loam, 3 to 8 percent slopes442B33232972299z91pa10319951:24000
Craigsville-Wyoming complex, 0 to 8 percent slopes, extremely stony9B19012972539z9tpa10319951:24000
Wyoming and Chenango soils, 0 to 8 percent slopes108B16942971839z7kpa10319951:24000
Wyoming very cobbly sandy loam, 8 to 15 percent slopes442C14082972309z92pa10319951:24000
Wyoming very cobbly sandy loam, 15 to 30 percent slopes442D5752972319z93pa10319951:24000
Wyoming and Chenango soils, 8 to 15 percent slopes108C4022971849z7lpa10319951:24000
Terrace escarpmentsTe4382970769z43pa11519681:20000
Craigsville-Wyoming complex, 0 to 8 percent slopes, extremely stony9B15319823bqswpa11519681:20000
Wyoming gravelly sandy loam, 3 to 8 percent slopesWyB11319949bqxypa11519681:20000
Wyoming gravelly loam, floodedWz28452971829z7jpa11719731:20000
Wyoming gravelly sandy loam, 30 to 50 percent slopesWyF21562971819z7hpa11719731:20000
Wyoming gravelly sandy loam, 20 to 30 percent slopesWyD10412971809z7gpa11719731:20000
Wyoming gravelly sandy loam, 12 to 20 percent slopesWyC10002971799z7fpa11719731:20000
Wyoming gravelly sandy loam, 3 to 8 percent slopesWyB93540962l4xdpa11919801:20000
Wyoming gravelly sandy loam, 8 to 15 percent slopesWyC23182966419yp2pa12719771:20000
Wyoming gravelly sandy loam, 3 to 8 percent slopesWyB17162966409yp1pa12719771:20000
Wyoming gravelly sandy loam, 15 to 25 percent slopesWyD11232966429yp3pa12719771:20000
Wyoming gravelly sandy loam, 25 to 45 percent slopesWyE3562966439yp4pa12719771:20000
Craigsville-Wyoming complex, 0 to 8 percent slopes, extremely stony9B41319874bqvjpa12719771:20000
Wyoming gravelly sandy loam, 3 to 8 percent slopesWyB3479301996b47tpa13119761:20000
Wyoming gravelly sandy loam, 8 to 15 percent slopesWyC2134301997b47vpa13119761:20000
Wyoming gravelly sandy loam, 15 to 25 percent slopesWyD1780301998b47wpa13119761:20000
Wyoming gravelly sandy loam, 0 to 3 percent slopesWyA1596301995b47spa13119761:20000
Wyoming gravelly sandy loam, 25 to 45 percent slopesWyE1266301999b47xpa13119761:20000
Wyoming gravelly sandy loam, 15 to 25 percent slopesWmD21672967999yv5pa61019781:20000
Wyoming gravelly sandy loam, 8 to 15 percent slopesWmC21522967989yv4pa61019781:20000
Wyoming gravelly sandy loam, 25 to 45 percent slopesWmF18082968009yv6pa61019781:20000
Wyoming very stony sandy loam, 3 to 15 percent slopesWoC17172968019yv7pa61019781:20000
Wyoming gravelly sandy loam, 3 to 8 percent slopesWmB11972967979yv3pa61019781:20000

Map of Series Extent

Approximate geographic distribution of the WYOMING 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 .