Official Series Description


Lab Data Summary

Aggregate lab data for the BOHICKET soil series. This aggregation is based on all pedons with a current taxon name of BOHICKET, 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 BOHICKET 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
153A83P028582SC013001Bohicket7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.566555,-80.7359238
153B83P028682SC013002Bohicket7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.5668335,-80.7498093
n/aS57_0451976-FL113-S57_045Bohicket3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.5684147,-87.1866074

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BOHICKET 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 BOHICKET 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 BOHICKET 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 BOHICKET 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 BOHICKET 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 BOHICKET 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 BOHICKET 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 BOHICKET, 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 BOHICKET 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
Bohicket and Tisonia soils, tidal71450914771051ll1kfl03719901:20000
Duckston-Bohicket-Corolla complex47108014771011ll1ffl03719901:20000
Bohicket and Handsboro soils47340823751wn5mfl11319781:20000
Bohicket-Capers associationBO15252012540346h8ga61619771:20000
Bohicket-Capers associationBO4365412579146wsga64419801:20000
Bohicket silty clayBo818332387c4w5ms04519791:20000
Bohicket silty clay loamBO129821155283w6qnc01919831:24000
Tidal marshTM96131160593wrvnc12919741:15840
Bohicket silty clay loamBo92361160703ws6nc13319841:24000
Bohicket silty clay loam, frequently floodedBo10491161593ww2nc14119861:24000
Bohicket associationBK1000371324094fs8sc01319751:20000
Bohicket associationBH135001319384f92sc01519741:20000
Bohicket association15176011322574fmcsc02919801:20000
Bohicket silty clay loam1544090639575pgjgsc04319801:20000
Bohicket silty clay loamBo17341301374cdzsc05119831:20000
Bohicket associationBK163541325274fx2sc05319751:20000
Tidal marsh, softTs1199901383074mxjsc69019671:24000
Bohicket silty clay loam235501193204051va09319821:15840
Bohicket silty clay loam, 0 to 1 percent slopes, very frequently flooded4A3446694780r9z8va10119951:15840
Bohicket muck, 0 to 1 percent slopes, frequently flooded4A400511970040k9va12719851:15840
Bohicket mucky silty clay loam, 0 to 1 percent slopes, very frequently flooded3A55612247243fqva18119971:24000
Bohicket silty clay loam3178912061441hsva19319801:20000
Bohicket muck6264912083541qxva69519811:15840
Bohicket muck, 0 to 1 percent slopes, very frequently flooded6331212245943f9va71519951:12000
Bohicket silty clay loam3510012087041s1va80019791:15840

Map of Series Extent

Approximate geographic distribution of the BOHICKET 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 .