Official Series Description


Lab Data Summary

Aggregate lab data for the GATES soil series. This aggregation is based on all pedons with a current taxon name of GATES, 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 GATES 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
7178P01361974NE041003Gates6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5538889,-99.8927778
7185P02301984NE077041Gates7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.625,-98.4455556
n/a40A205360NE041002Gates6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GATES 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 GATES 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 GATES 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 GATES 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 GATES 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 GATES 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 GATES 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 GATES, 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-2012-02-08-07 | Blaine County - September 1993

    Typical pattern of soils and parent material in the Valentine-Hersh-Gates association (Soil Survey of Blaine County, Nebraska; September 1993).

  2. NE-2012-02-10-23 | Custer County - July 1982

    Typical pattern of soils in the Kenesaw-Hord-Gates association and relationship of soils to topography and parent material (Soil Survey of Custer County, Nebraska; July 1982).

  3. NE-2012-02-13-07 | Garfield County - February 1988

    Typical pattern of soils and parent material in the Valentine association (Soil Survey of Garfield County, Nebraska; February 1988).

  4. NE-2012-02-13-09 | Garfield County - February 1988

    Typical pattern of soils and parent material in the Hersh-Valentine-Gates association (Soil Survey of Garfield County, Nebraska; February 1988).

  5. NE-2012-02-13-16 | Greeley County - April 1993

    Typical pattern of soils and parent material in the Valentine association (Soil Survey of Greeley County, Nebraska; April 1993).

  6. NE-2012-02-13-17 | Greeley County - April 1993

    Typical pattern of soils and parent material in the Dunday-Anselmo-Valentine association (Soil Survey of Greeley County, Nebraska; April 1993).

  7. NE-2012-02-13-53 | Loup County - October 1990

    Typical pattern of soils and parent material in the Hersh-Gates-Valentine association (Soil Survey of Loup County, Nebraska; October 1990).

  8. NE-2012-02-14-19 | Wheeler County - September 1988

    Pattern of soils and parent material in the Coly-Uly association (Soil Survey of Wheeler County, Nebraska; September 1988).

Map Units

Map units containing GATES 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
Gates silt loam, 1 to 3 percent slopes90271347221608930ts7ne00119701:20000
Gates silt loam, 0 to 1 percent slopes9026209221608830ts6ne00119701:20000
Gates fine sandy loam, 0 to 3 percent slopes, hummocky90253221608730ts5ne00119701:20000
Hersh-Gates complex, 0 to 3 percent slopes2604250116994862ymc2ne00919881:20000
Gates-Hersh complex, 20 to 60 percent slopes904398516994842ymc0ne00919881:20000
Gates very fine sandy loam, 3 to 6 percent slopes903636016994832wgdlne00919881:20000
Gates very fine sandy loam, 11 to 17 percent slopes90391922191562wgdnne00919881:20000
Gates very fine sandy loam, 6 to 11 percent slopes, eroded90385122166622wgdmne01119661:20000
Gates silt loam, 1 to 3 percent slopes9027521222821230ts7ne01919671:20000
Gates silt loam, 3 to 6 percent slopes902877222821330rsxne01919671:20000
Gates-Hersh complex, 20 to 60 percent slopes90431327016995932ymc0ne04119801:20000
Gates very fine sandy loam, 3 to 6 percent slopes90361263216995892wgdlne04119801:20000
Gates very fine sandy loam, 17 to 30 percent slopes9041959716995922wgdpne04119801:20000
Gates very fine sandy loam, 6 to 11 percent slopes, eroded9038774616995902wgdmne04119801:20000
Gates very fine sandy loam, 11 to 17 percent slopes9039564216995912wgdnne04119801:20000
Gates silt loam, 11 to 30 percent slopes903396822281762zns3ne04119801:20000
Gates silt loam, 3 to 6 percent slopes, eroded902920722281742wgdgne04119801:20000
Gates silt loam, 6 to 11 percent slopes, eroded903012222281752wgdhne04119801:20000
Gates silt loam, 1 to 3 percent slopes90272422281732wgdfne04119801:20000
Hersh-Gates complex, 0 to 3 percent slopes2604426416997882ymc2ne07119841:20000
Gates very fine sandy loam, 3 to 6 percent slopes, eroded9037364616997802wgdkne07119841:20000
Gates very fine sandy loam, 11 to 30 percent slopes9040228016997822zns4ne07119841:20000
Gates very fine sandy loam, 1 to 3 percent slopes9035186616997792wgdjne07119841:20000
Gates very fine sandy loam, 6 to 11 percent slopes, eroded9038150816997812wgdmne07119841:20000
Hersh-Gates complex, 17 to 30 percent slopes2605639616999481v1y1ne07719871:20000
Gates-Hersh complex, 0 to 3 percent slopes9042577916999412ymbzne07719871:20000
Gates silt loam, 6 to 11 percent slopes, eroded9030516716999392wgdhne07719871:20000
Gates silt loam, 3 to 6 percent slopes, eroded9029360316999382wgdgne07719871:20000
Gates silt loam, 11 to 17 percent slopes, eroded9032279716999401v1xsne07719871:20000
Gates silt loam, 1 to 3 percent slopes90276915170012130ts7ne07920031:12000
Gates fine sandy loam, 0 to 3 percent slopes, hummocky90254125170012530ts5ne07920031:12000
Gates silt loam, 0 to 1 percent slopes90262804170012030ts6ne07920031:12000
Gates silt loam, 3 to 6 percent slopes90282525170012230rsxne07920031:12000
Gates silt loam, 6 to 11 percent slopes, eroded9030115017001241v23qne07920031:12000
Gates silt loam, 3 to 6 percent slopes, eroded902932417001231v23pne07920031:12000
Gates fine sandy loam, 0 to 3 percent slopes, hummocky90254222891630ts5ne09319681:12000
Hersh-Gates complex, 0 to 3 percent slopes2604521216995372ymc2ne11519861:20000
Gates silt loam, 3 to 6 percent slopes, eroded9029278216995302wgdgne11519861:20000
Hersh-Gates complex, 30 to 60 percent slopes2606231216995381v1htne11519861:20000
Gates silt loam, 6 to 11 percent slopes, eroded9030164316995312wgdhne11519861:20000
Gates silt loam, 1 to 3 percent slopes9027147116995292wgdfne11519861:20000
Gates silt loam, 11 to 30 percent slopes9033140616995322zns3ne11519861:20000
Gates-Hersh complex, 20 to 60 percent slopes90431022198202ymc0ne11519861:20000
Gates very fine sandy loam, 3 to 6 percent slopes9036522198192wgdlne11519861:20000
Gates very fine sandy loam, 3 to 6 percent slopes, eroded903758516998852wgdkne17519831:20000
Gates very fine sandy loam, 6 to 11 percent slopes, eroded903840516998862wgdmne17519831:20000
Gates very fine sandy loam, 1 to 3 percent slopes903585016998392wgdjne18319841:20000
Gates very fine sandy loam, 6 to 11 percent slopes, eroded903877816998412wgdmne18319841:20000
Gates very fine sandy loam, 3 to 6 percent slopes903665916998402wgdlne18319841:20000
Gates silt loam, 6 to 11 percent slopes, eroded90307122198972wgdhne18319841:20000
Gates-Hersh complex, 0 to 3 percent slopes9042422198982ymbzne18319841:20000

Map of Series Extent

Approximate geographic distribution of the GATES 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 .