Official Series Description


Lab Data Summary

Aggregate lab data for the KINGFISHER soil series. This aggregation is based on all pedons with a current taxon name of KINGFISHER, 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 KINGFISHER 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
80A88P045688OK047001Kingfisher6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5508347,-97.8730545
80A88P045788OK047002Kingfisher4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5508347,-97.8730545
84A01N1210S2001OK051001Kingfisher7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.9597664,-97.9791336

Water Balance

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

There are insufficient data to create the 3D mountains figure.

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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with KINGFISHER 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 KINGFISHER 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 KINGFISHER 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 KINGFISHER, 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. OK-2012-02-16-04 | Blaine County - February 1968

    Typical pattern of soils in associations 1, 3, 4, and 6 (Soil Survey of Blaine County, Oklahoma; February 1968).

  2. OK-2012-02-16-12 | Cleveland County - April 1987

    Typical pattern of soils and underlying material in the Renfrow-Grainola-Grant map unit and the Port-Weswood map unit (Soil Survey of Cleveland County, Oklahoma; April 1987).

Map Units

Map units containing KINGFISHER 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
Kingfisher-Vernon complex, 3 to 6 percent slopes54241353713824931hdlkks00719731:24000
Kingfisher silt loam, 1 to 3 percent slopes5422479913824912tq68ks00719731:24000
Kingfisher-Vernon complex, 1 to 3 percent slopes5423119513824921hdljks00719731:24000
Kingfisher-Ironmound complex, 5 to 8 percent slopes, shallow, erodedKgID230622376nwmnok00319711:24000
Kingfisher-Lucien complex, 3 to 8 percent slopes, erodedKhD28472381732dt6yok01119651:24000
Kingfisher silt loam, 1 to 3 percent slopesKfB70223817302tq68ok01119651:24000
Kingfisher-Huska complex, 1 to 3 percent slopesKlB1740381733dt6zok01119651:24000
Kingfisher silt loam, 0 to 1 percent slopesKfA1380381729dt6vok01119651:24000
Kingfisher-Grant complex, 3 to 5 percent slopesKgC1023381731dt6xok01119651:24000
Kingfisher silt loam, 3 to 5 percent slopesKfC201863819522tq69ok01719721:24000
Kingfisher silt loam, 1 to 3 percent slopesKfB161713819512tq68ok01719721:24000
Kingfisher-Ironmound complex, 1 to 5 percent slopes970753821532tq6cok02719841:24000
Kingfisher-Urban land-Ironmound complex, 1 to 5 percent slopes281393820952tq6gok02719841:24000
Kingfisher-Ironmound complex, 5 to 8 percent slopes, shallow, erodedGnD29974382494dv0jok04719651:24000
Kingfisher-Ironmound complex, 8 to 20 percent slopes, erodedGnE27568382496dv0lok04719651:24000
Kingfisher-Ironmound complex, 8 to 20 percent slopesGnE7419382495dv0kok04719651:24000
Kingfisher-Ironmound complex, 5 to 8 percent slopesGnD2701382493dv0hok04719651:24000
Kingfisher silt loam, 3 to 5 percent slopes, erodedKfC224183824982tq6bok04719651:24000
Kingfisher-Ironmound complex, 5 to 8 percent slopes, erodedKlD2244382499dv0pok04719651:24000
Kingfisher silt loam, 1 to 3 percent slopes2477633827122tq68ok05319831:24000
Kingfisher-Wakita complex, 1 to 3 percent slopes274819382715dv7nok05319831:24000
Grant-Kingfisher complex, 5 to 8 percent slopes, eroded213747382709dv7gok05319831:24000
Kingfisher silt loam, 3 to 5 percent slopes, eroded2634323827142tq6bok05319831:24000
Kingfisher-Wakita complex, 3 to 5 percent slopes, eroded282318382716dv7pok05319831:24000
Grant-Kingfisher complex, 5 to 8 percent slopes201654382708dv7fok05319831:24000
Kingfisher silt loam, 3 to 5 percent slopes2512993827132tq69ok05319831:24000
Grant-Kingfisher complex, 5 to 8 percent slopes, erodedGrKD28623469nxrxok07119651:24000
Kingfisher silt loam, 1 to 3 percent slopesKfB240693833932tq68ok07319601:24000
Kingfisher silt loam, 3 to 5 percent slopesKfC234433833942tq69ok07319601:24000
Kingfisher-Lucien complex, 5 to 8 percent slopes, erodedKgD310329383395dvylok07319601:24000
Kingfisher-Wakita complex, 1 to 3 percent slopesKhB2691383396dvymok07319601:24000
Kingfisher-Wakita complex, 3 to 5 percent slopesKhC1127383397dvynok07319601:24000
Kingfisher loam, 3 to 5 percent slopes, erodedKinC24275383634dw69ok08319941:12000
Kingfisher silt loam, 1 to 3 percent slopesKgfB8243836332tq68ok08319941:12000
Kingfisher-Ironmound complex, 5 to 8 percent slopes, shallow, erodedKgID25013835691hfq8ok09319651:24000
Kingfisher-Lucien complex, 1 to 5 percent slopesKgLC36363840672tq6fok10319941:24000
Kingfisher loam, 3 to 5 percent slopes, erodedKinC22642384070dwncok10319941:24000
Kingfisher silt loam, 1 to 3 percent slopesKgfB25833840692tq68ok10319941:24000
Kingfisher-Wakita complex, 1 to 5 percent slopesKgWC1226384068dwn9ok10319941:24000
Kingfisher-Ironmound complex, 1 to 5 percent slopesKgIC10803843132tq6cok10919961:12000
Ironmound-Kingfisher complex, 1 to 8 percent slopesIrKD544384308dwx1ok10919961:12000
Kingfisher-Urban land-Ironmound complex, 1 to 5 percent slopesKUIC4123843092tq6gok10919961:12000
Kingfisher-Loco complex, 5 to 12 percent slopesKk14291384864dxgzok13719601:24000

Map of Series Extent

Approximate geographic distribution of the KINGFISHER 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 .