Official Series Description


Lab Data Summary

Aggregate lab data for the GANNETT soil series. This aggregation is based on all pedons with a current taxon name of GANNETT, 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 GANNETT 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
6592P034991NE031024Gannett6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.4883347,-101.7102814
6592P034491NE075001Gannett7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9811096,-101.7600021
6592P034591NE075002Gannett7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.833889,-101.6777802

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GANNETT 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 GANNETT 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 GANNETT 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 GANNETT 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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Click the image to view it full size.

Competing Series

Soil series competing with GANNETT 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 GANNETT 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 GANNETT 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 GANNETT, 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. NE-2012-02-10-22 | Custer County - July 1982

    Typical pattern of soils and relationship of soils to topography and parent material in three associations: No. 8—Cozad association; No. 13—Ipage-Valentine association; No. 14—Boel-Barney-Gannett association (Soil Survey of Custer County, Nebraska; July 1982).

  2. NE-2012-02-13-29 | Holt County - March 1983

    Typical pattern of soils in the Elsmere-Ipage-Loup association and their relationship to topography and parent material (Soil Survey of Holt County, Nebraska; March 1983).

  3. NE-2012-02-13-33 | Hooker County - January 1964

    Diagram showing typical topography, soils, and parent materials in Hooker County. Symbols below soil names identify range sites, as follows: CS=Choppy Sands; WL=Wet Land; Sb=Subirrigated; Sv=Sandy; So=Sands; and TB=Thin Breaks (Soil Survey of Hooker County, Nebraska; January 1964).

Map Units

Map units containing GANNETT 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
Gannett mucky peat457948924347282ymc7ne00519731:24000
Gannett fine sandy loam, 0 to 1 percent slopes4575864270352zbdyne01119661:20000
Gannett fine sandy loam, 0 to 1 percent slopes45751704999892zbdyne01719871:20000
Gannett silt loam, overwash, frequently ponded4583279516990251v0z8ne02919801:20000
Gannett variant silt loam, occasionally flooded426314422195312dhlsne02919801:20000
Gannett mucky peat457924321003822ymc7ne03119951:24000
Gannett loam, 0 to 1 percent slopes457621301003812wgdtne03119951:24000
Gannett and Loup loams, occasionally flooded4260325116995881v1kfne04119801:20000
Gannett loam, 0 to 1 percent slopes457673516995871v1kdne04119801:20000
Gannett-Loup fine sandy loams, 0 to 3 percent slopes45851662516988421v0scne07519731:24000
Gannett-Loup fine sandy loams, drained, 0 to 3 percent slopes4586430916988431v0sdne07519731:24000
Loup-Gannett loamy fine sands, frequently ponded4676151416988451v0sgne07519731:24000
Loup-Gannett loamy fine sands, drained, 0 to 3 percent slopes467774316988461v0shne07519731:24000
Gannett mucky peat45797622192822ymc7ne07519731:24000
Gannett silt loam, occasionally flooded426233716992431v169ne08519811:20000
Gannett loam, 0 to 1 percent slopes457672461001012wgdtne08919811:20000
Gannett mucky peat457913941001022ymc7ne08919811:20000
Gannett silt loam, occasionally flooded42626722197462dhtqne11119711:24000
Gannett fine sandy loam, occasionally flooded4261316216993541v19wne11319691:24000
Gannett variant silt loam, occasionally flooded426318216989651v0xbne13519871:20000
Gannett mucky peat457911711005922ymc7ne16119921:20000
Gannett loam, 0 to 1 percent slopes45769081005912wgdtne16119921:20000
Gannett fine sandy loam, 0 to 2 percent slopesGa981352736cv1lsd00720041:20000
Gannett loam, 0 to 1 percent slopesT071A91613900692wgdtsd00720041:20000
Gannett mucky peatT072A54613900702ymc7sd00720041:20000
Gannett loam, 0 to 1 percent slopesT071A9413915552wgdtsd12119671:31680
Gannett mucky peatT072A8313915562ymc7sd12119671:31680
Gannett sandy loamGe49352990cv9ssd12119671:31680
Gannett loam, 0 to 1 percent slopesT071A21725827712wgdtsd61320111:24000
Gannett mucky peatT072A1125827722ymc7sd61320111:24000

Map of Series Extent

Approximate geographic distribution of the GANNETT 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 .