Official Series Description


Lab Data Summary

Aggregate lab data for the GIBBON soil series. This aggregation is based on all pedons with a current taxon name of GIBBON, 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 GIBBON 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
102C04N0896S04NE055001Gibbon5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3912506,-96.4096909
102C04N0899S2004NE055078Gibbon5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.267601,-96.2797699
102C04N0900S2004NE055094Gibbon5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.344429,-96.3216782
102C04N0901S2004NE055098Gibbon5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3532143,-96.3539963
102C04N0904S2004NE055103Gibbon5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3166809,-96.3296051
102C04N0917S2004NE153069Gibbon5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.172905,-96.3092422
107B04N0916S2004NE153017Gibbon5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1216431,-96.3011398
107B04N0918S2004NE153071Gibbon5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1036835,-96.3033524
7140A20921974NE121043Gibbon5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1911163,-97.8325729
7187P004685NE163205Gibbon7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.25,-98.9761124
7309KS15700609KS157006Gibbon4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8263893,-97.832222
7309KS157104909KS1571049Gibbon3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9423523,-97.8419647
n/a04N0913S1997NE153001Gibbon5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a04N0914S1997NE153004Gibbon5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a04N0915S1997NE153006Gibbon5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a04N0903S2004NE055100Gibbon5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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Soil series sharing subgroup-level classification with GIBBON, 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-2012-02-08-12 | Butler County - February 1982

    Typical pattern of soils in the Alda-Boel-Barney association and the Gibbon-Muir-Zook association and relationship of the soils to topography and parent material (Soil Survey of Butler County, Nebraska; February 1982).

  2. NE-2012-02-13-26 | Hayes County - August 1982

    The relationship of soils to topography and parent material in the Bridget-McCook-Gibbon association (Soil Survey of Hayes County, Nebraska; August 1982).

  3. NE-2012-02-13-99 | Sherman County - May 1990

    Typical pattern of soils and parent material in the Loup-Bolent-Barney and Gibbon-Wann-Saltine associations (Soil Survey of Sherman County, Nebraska; May 1990).

Map Units

Map units containing GIBBON 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
Gibbon loam, occasionally flooded352964114546422zt6vks02719831:24000
Gibbon loam, occasionally flooded352925126057502zt6vks02919721:24000
Gibbon silty clay loam, occasionally flooded3537548013818492zwl7ks08919811:24000
Gibbon loam, occasionally flooded3529112826056412zt6vks15719651:24000
Gibbon silty clay loam, occasionally flooded3537413819062zwl7ks15719651:24000
Gibbon silt loam, 0 to 2 percent slopes, occasionally flooded847027014269542y21hne00319751:20000
Gibbon silt loam, saline, 0 to 2 percent slopes, occasionally flooded84725674269552vwbmne00319751:20000
Gibbon silt loam, 0 to 2 percent slopes, occasionally flooded84709122166462y21hne01119661:20000
Leshara and Gibbon silt loams6350838717000661v21vne01919671:20000
Gibbon silt loam, rarely flooded8469362017000451v215ne01919671:20000
Gibbon silt loam, saline, rarely flooded847193817000191v20bne01919671:20000
Gibbon silt loam, occasionally flooded847012322282282dsnbne01919671:20000
Gibbon loam, rarely flooded84658522282192dsn1ne01919671:20000
Gibbon silty clay loam, occasionally flooded3537688416912781trxcne02319791:20000
Saltine-Gibbon silt loams, occasionally flooded6381280116913171trymne02319791:20000
Gibbon silt loam, 0 to 2 percent slopes, occasionally flooded847068522190322y21hne02319791:20000
Gibbon silt loam, 0 to 2 percent slopes, occasionally flooded8470422185462y21hne02719821:20000
Gibbon silt loam, occasionally flooded8470188016990262zwlbne02919801:20000
Gibbon silty clay loam, occasionally flooded353761322169812ddyjne03919731:20000
Gibbon loam, 0 to 2 percent slopes, occasionally flooded35295822170192y21gne03919731:20000
Saltine-Gibbon complex, occasionally flooded63802322170202ddzsne03919731:20000
Gibbon silt loam, occasionally flooded8470238816995941v1kmne04119801:20000
Gibbon loam, rarely flooded8465234916996791v1ncne04719751:20000
Gibbon loam, 0 to 2 percent slopes, occasionally flooded3529133674268852y21gne05319751:20000
Gibbon silty clay loam, occasionally flooded353710372426886gb6jne05319751:20000
Gibbon-Wann complex, occasionally flooded8480556322170982df29ne05319751:20000
Saltine-Gibbon complex, occasionally flooded63804688426912gb7cne05319751:20000
Gibbon variant soils, frequently flooded84751407426887gb6kne05319751:20000
Gibbon loamy sand, overwash, 0 to 2 percent slopes, occasionally flooded84684644268842vwblne05319751:20000
Gibbon-Wann complex, occasionally flooded84801144517109401vfcmne05520071:12000
Gibbon silty clay loam, occasionally flooded3537330517109411vfcnne05520071:12000
Novina-Gibbon complex, occasionally flooded853272617109611vfd9ne05520071:12000
Saltine-Gibbon silty clay loams, occasionally flooded638225617109701vfdlne05520071:12000
Gibbon loamy sand, overwash, 0 to 2 percent slopes, occasionally flooded84684417109422vwblne05520071:12000
Gibbon silt loam, rarely flooded8469206416919482zwl6ne06119741:20000
Gibbon silt loam, occasionally flooded8470701816997402zwl9ne06519751:20000
Gibbon silt loam, saline, 0 to 2 percent slopes, occasionally flooded847257816997422zwlcne06519751:20000
Gibbon silt loam, rarely flooded846964516997831v1rqne07119841:20000
Gibbon silt loam, rarely flooded8469333417001271v23tne07920031:12000
Gibbon loam, saline, rarely flooded846729217001281v23vne07920031:12000
Leshara and Gibbon silt loams635013822282402dsnqne07920031:12000
Gibbon silt loam, occasionally flooded8470134216992442zwlbne08519811:20000
Gibbon silt loam, rarely flooded84691680997013br5ne09319681:12000
Gibbon loam, occasionally flooded35297322289202dtcnne09319681:12000
Gibbon loam, rarely flooded8465110916918441tshmne09919821:20000
Gibbon loam, saline, rarely flooded8467103416918451tshnne09919821:20000
Gibbon silt loam, 0 to 2 percent slopes, occasionally flooded847016568491822y21hne10719891:20000
Gibbon silt loam, occasionally flooded, wet848263425704682rmj0ne10719891:20000
Gibbon silty clay loam, occasionally flooded35379452427402gbr5ne11919811:20000
Gibbon-Gayville silty clay loams, occasioanlly flooded84761994427403gbr6ne11919811:20000
Gibbon loam, occasionally flooded3529680717096391vd0nne12119781:20000
Gibbon silt loam, rarely flooded846912422282622dspfne12119781:20000
Gibbon-Gayville silty clay loams, occasioanlly flooded84762922282882dsq8ne12119781:20000
Gibbon silt loam, 0 to 2 percent slopes, occasionally flooded847018984274822y21hne12519581:20000
Gibbon loam, occasionally flooded352961022289982dtg5ne12519581:20000
Gibbon silt loam, saline, 0 to 2 percent slopes, occasionally flooded84723704274482vwbmne12519581:20000
Gibbon silt loam, occasionally flooded8470133516920622zwlhne12919741:20000
Gibbon silty clay loam, occasionally flooded35372526057122zwl7ne12919741:20000
Gibbon silt loam, occasionally flooded847045916989662zwlbne13519871:20000
Gibbon loam, saline, rarely flooded84673622194682dhjrne13719671:20000
Gibbon silt loam, 0 to 2 percent slopes, occasionally flooded84701222171742y21hne13919701:20000
Gibbon-Gayville silty clay loams, occasioanlly flooded84767233427637gbzrne14119841:20000
Gibbon silt loam, 0 to 2 percent slopes, occasionally flooded847055644276362y21hne14119841:20000
Gibbon silty clay loam, occasionally flooded353768122189972dh1kne14319671:20000
Gibbon silt loam, occasionally flooded84703122191192zwl9ne14519651:20000
Gibbon-Wann complex, occasionally flooded8480264917110051vffqne15320071:12000
Gibbon loamy sand, overwash, 0 to 2 percent slopes, occasionally flooded8468201617110072vwblne15320071:12000
Gibbon silty clay loam, occasionally flooded353795417110061vffrne15320071:12000
Novina-Gibbon complex, occasionally flooded853232117110241vfgbne15320071:12000
Gibbon silt loam, 0 to 2 percent slopes, occasionally flooded8470467516914202y21hne15519951:12000
Gibbon-Saltine loams, occasionally flooded8477203816914211ts1zne15519951:12000
Gibbon silt loam, rarely flooded8469511016999881v1zbne16319871:20000
Gibbon-Saltine silt loams, rarely flooded8478122916999891v1zcne16319871:20000
Gibbon silty clay loam, occasionally flooded35372898426828gb4nne16719801:20000
Gibbon silt loam, rarely flooded8469131216998871v1w2ne17519831:20000
Gibbon silty clay loam, occasionally flooded353741122173362df9zne17919701:20000
Gibbon silty clay loam, rarely flooded8473279716920042zwl8ne18119671:20000
Gibbon silt loam, occasionally flooded847073222290722zwlhne18119671:20000
Gibbon loam, occasionally flooded352910416998421v1tmne18319841:20000

Map of Series Extent

Approximate geographic distribution of the GIBBON 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 .