Official Series Description


Lab Data Summary

Aggregate lab data for the OMEGA soil series. This aggregation is based on all pedons with a current taxon name of OMEGA, 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 OMEGA 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
90A40A173768MN017005Omega4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.5499992,-92.5333328
9240A173868MN017008Omega4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.4333344,-92.5
93B40A1923S1966MI013003Omega5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.6524963,-88.5922775
93B40A1924S1966MI103001Omega5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.3488846,-87.4152908

Water Balance

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

Competing Series

Soil series competing with OMEGA 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 OMEGA 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 OMEGA 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 OMEGA, 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. WI-2012-03-22-01 | Bayfield County - April 1961

    General soil areas: (1) Red clays and pink sands (Ontonagon, Superior, Orienta, Bibon); (2) Rolling and hilly pink stony sandy loams (Gogebic, Cloquet); (3) Rolling and hilly pink sands (Vilas, Omega, Hiawatha); (4) Nearly level pink sands (Omega, Vilas); (5) Undulating and rolling pink stony silt loams, loams, and sandy loams (Freeon, Gogebic, Cloquet); (6) Undulating pink fine sandy loams (Pence); and (7) Wet soils (Peat) (Soil Survey of Bayfield County, WI; 1961).

Map Units

Map units containing OMEGA 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
Omega loamy fine sand, 2 to 6 percent slopes188B4299432872gjfmmn00119961:20000
Omega loamy fine sand, 6 to 12 percent slopes188C1382432873gjfnmn00119961:20000
Omega loamy sand, 12 to 25 percent slopes188E474432874gjfpmn00119961:20000
Omega loamy sand, 2 to 12 percent slopes188C16966396341f9f6mn01719731:20000
Omega loamy sand, 0 to 2 percent slopes18811289396340f9f5mn01719731:20000
Ahmeek-Omega complex, 2 to 12 percent slopes975C9659396382f9gjmn01719731:20000
Omega loamy sand, 12 to 25 percent slopes188E3864396342f9f7mn01719731:20000
Ahmeek-Omega complex, 12 to 25 percent slopes975E1634396383f9gkmn01719731:20000
Ahmeek-Omega complex, 0 to 2 percent slopes975867396381f9ghmn01719731:20000
Omega fine sand, 6 to 12 percent slopesOgC64421201g494wi09519781:15840
Omega fine sand, 12 to 20 percent slopesOgD9421202g495wi09519781:15840
Omega fine sand, 2 to 6 percent slopesOgB3421200g493wi09519781:15840

Map of Series Extent

Approximate geographic distribution of the OMEGA 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 .