Official Series Description


Lab Data Summary

Aggregate lab data for the BOSKET soil series. This aggregation is based on all pedons with a current taxon name of BOSKET, 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 BOSKET 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
131AM99017391990MO017007Bosket4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1480064,-89.9250946
131AM91143011991MO143001Bosket4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.6752777,-89.5595016
131AM99017581999MO017084Bosket4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1305199,-89.8941498
131AM03023032003MO023003Bosket4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5717239,-90.553009
131AM03069272003MO069013Bosket4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.4876099,-89.9600601
131AM03207162003MO207019Bosket4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0880318,-89.9128799
131AM05143992005MO143001Bosket4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8267288,-89.5764084
131A40A4929S1961TN045012Bosket4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.1341667,-89.4544449
131A40A4930S1961TN045013Bosket5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.1538887,-89.4480591
134M99017481999MO017078Bosket4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0568924,-89.9597626
n/a40A4771S1944MS135007BOSKET4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

Competing Series

Soil series competing with BOSKET 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 BOSKET 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 BOSKET 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 BOSKET, 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. MO-2012-02-06-22 | Butler County and Part of Ripley County - November 1983

    Typical pattern of soils and parent material in the Tuckerman-Bosket association (Soil Survey of Butler County and Part of Ripley County, Missouri; November 1983).

  2. MS-2012-04-26-09 | De Soto County - September 1959

    Soil associations in De Soto County (Soil Survey of De Soto County, Mississippi; September 1959).

  3. MS-2012-04-27-01 | Quitman County - December 1958

    Soil associations, Quitman County, Miss. (Soil Survey of Quitman County, Mississippi; December 1958).

  4. MS-2012-04-27-09 | Tunica County - May 1956

    Soil association map of Tunica County, Miss (Soil Survey of Tunica County, Mississippi; May 1956).

  5. MS-2012-04-27-10 | Bolivar County - December 1958

    Soil associations in Bolivar County: 1. Alluvial soils; 2. Commerce-Robinsonville-Crevasse; 3. Forestdale-Dundee-Bosket; 4. Brittain-Pearson-Dexter; 5. Dowling-Alligator-Sharkey (Soil Survey of Bolivar County, Mississippi; December 1958).

Map Units

Map units containing BOSKET 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
Bosket fine sandy loam, gently undulating157079564047lxy2ar02119751:20000
Bosket fine sandy loam, undulating162157564048lxy3ar02119751:20000
Bosket fine sandy loam, 0 to 3 percent slopesBoU292955657962wn5dar06719711:20000
Bosket fine sandy loam, 0 to 1 percent slopesBoA102945657952wn5car06719711:20000
Bosket fine sandy loam, 0 to 3 percent slopesBoB103705645232wn5dar07519731:20000
Bosket fine sandy loam, 0 to 1 percent slopesBoA7605645222wn5car07519731:20000
Bosket fine sandy loam, gently undulatingBkB7505565959lzxrar09519741:20000
Bosket fine sandy loam, 0 to 1 percent slopesBkA39725659582wn5car09519741:20000
Bosket fine sandy loam, 0 to 3 percent slopes4173505645062wn5dar12119761:20000
Bosket-Dubbs fine sandy loam, gently undulatingBdB2000564429lybdar12319641:20000
Bosket-Dubbs fine sandy loam, undulatingBdC1800564430lybfar12319641:20000
Bosket-Dubbs fine sandy loams, 0 to 1 percent slopesBdA280564428lybcar12319641:20000
Bosket fine sandy loam, 1 to 5 percent slopes8200659024977802pqqnmo01720041:24000
Bosket loam, 0 to 3 percent slopes, occasionally flooded82007175712023rwxhmo01720041:24000
Bosket fine sandy loam, 1 to 5 percent slopes, rarely flooded82020362689833z0hymo01720041:24000
Bosket fine sandy loam, 0 to 1 percent slopes, rarely flooded8201846025716932pqqxmo03119781:24000
Bosket fine sandy loam, 1 to 5 percent slopes8200611024977792pqqnmo03119781:24000
Bosket fine sandy loam, 0 to 1 percent slopes82017424978332pqqwmo03119781:24000
Bosket fine sandy loam, 0 to 1 percent slopes820171291226898382pqqwmo06919771:24000
Bosket fine sandy loam, 0 to 1 percent slopes, rarely flooded8201840324978352pqqxmo06919771:24000
Bosket fine sandy loam, 0 to 1 percent slopes, frequently flooded8608320025010292q0j0mo06919771:24000
Bosket fine sandy loam, 0 to 5 percent slopes903031426898512r03gmo06919771:24000
Bosket fine sandy loam, 0 to 1 percent slopes82017535724978322pqqwmo13319781:24000
Bosket fine sandy loam, 0 to 1 percent slopes, rarely flooded8201824726898622pqqxmo13319781:24000
Bosket fine sandy loam, 0 to 1 percent slopes, frequently flooded860838125010312q0j0mo13319781:24000
Bosket fine sandy loam, 0 to 1 percent slopes, rarely flooded820181863324978362pqqxmo14319741:24000
Bosket fine sandy loam, 0 to 1 percent slopes82017915824978342pqqwmo14319741:24000
Bosket fine sandy loam, 1 to 5 percent slopes, rarely flooded82020755894224z0hymo14319741:24000
Bosket fine sandy loam, 0 to 1 percent slopes, frequently flooded8608324125010302q0j0mo14319741:24000
Bosket fine sandy loam, 1 to 5 percent slopes820061726898792pqqnmo14319741:24000
Bosket loam, 0 to 3 percent slopes, occasionally flooded82007122689880rwxhmo14319741:24000
Bosket fine sandy loam, 0 to 1 percent slopes82017554824978312pqqwmo20119781:24000
Bosket fine sandy loam, 0 to 5 percent slopes9030315326899162r03gmo20119781:24000
Bosket fine sandy loam, 0 to 1 percent slopes, rarely flooded820186126898992pqqxmo20119781:24000
Bosket loam, 0 to 3 percent slopes, occasionally flooded8200762689898rwxhmo20119781:24000
Bosket fine sandy loam, 1 to 5 percent slopes, eroded820193055894103z0d1mo20719831:24000
Bosket fine sandy loam, 1 to 5 percent slopes82006135124977832pqqnmo20719831:24000
Bosket fine sandy loam, 1 to 5 percent slopes, rarely flooded820201512689924z0hymo20719831:24000
Bosket fine sandy loam, 3 to 8 percent slopes, severely eroded82023151894101z0czmo20719831:24000
Bosket fine sandy loam, 0 to 1 percent slopes820171326899232pqqwmo20719831:24000
Bosket loam, 0 to 3 percent slopes, occasionally flooded82007122689922rwxhmo20719831:24000
Bosket fine sandy loam, 0 to 5 percent slopes903031126899472r03gmo20719831:24000
Bosket sandy loamBo479566768m0rvtn04519631:15840

Map of Series Extent

Approximate geographic distribution of the BOSKET 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 .