Official Series Description


Lab Data Summary

Aggregate lab data for the BUNYAN soil series. This aggregation is based on all pedons with a current taxon name of BUNYAN, 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 BUNYAN 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
80B82P0297S1981TX143004BUNYAN6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.5083351,-98.401947
8582P0298S1981TX143005BUNYAN6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.1338882,-98.3147202

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BUNYAN 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 BUNYAN 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 BUNYAN 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 BUNYAN 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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Competing Series

Soil series competing with BUNYAN 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 BUNYAN 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 BUNYAN 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 BUNYAN, 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

No block diagrams are available.

Map Units

Map units containing BUNYAN 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
Pulaski and Bunyan soils, 0 to 1 percent slopes, frequently flooded3631694382020dtj7ok01919771:24000
Bunyan loam, 0 to 1 percent slopes, occasionally flooded37704382013dtj0ok01919771:24000
Pulaski and Bunyan soils, 0 to 1 percent slopes, frequently floodedLv9482383723dw95ok08519631:24000
Bunyan loam, 0 to 1 percent slopes, frequently floodedPs1113383732dw9gok08519631:24000
Bunyan loam, 0 to 1 percent slopes, occasionally floodedPr535383731dw9fok08519631:24000
Bunyan fine sandy loam, frequently flooded202855364970d7s7tx12119751:24000
Bunyan fine sandy loam, 0 to 1 percent slopes, occasionally floodedBu7247365228d81ktx13319721:20000
Bunyan soils, frequently floodedBy6578365229d81ltx13319721:20000
Bunyan fine sandy loam, occasionally floodedBu19247365357d85qtx14319661:20000
Bunyan soils, frequently floodedBy4276365358d85rtx14319661:20000
Bunyan fine sandy loam, frequently flooded151932365432d884tx14519751:20000
Bunyan and Whitesboro soils, frequently flooded1616375366650d9jftx18119771:20000
Santo and Bunyan soils, 0 to 1 percent slopes, frequently floodedSb16353390963f3tqtx36319791:24000
Santo and Bunyan soils, 0 to 1 percent slopes, frequently floodedYb19475390925f3shtx36719731:20000
Bunyan fine sandy loam, 0 to 1 percent slopes, occasionally floodedBu3823390869f3qptx36719731:20000
Bunyan soils, frequently floodedBy2849371937dh0ztx41119801:24000
Bunyan fine sandy loam, occasionally floodedBu1198374324dkhztx60919751:20000

Map of Series Extent

Approximate geographic distribution of the BUNYAN 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 .