Soil Data Explorer - BOSVILLE

Official Series Description

Lab Data Summary

Aggregate lab data for the BOSVILLE soil series. This aggregation is based on all pedons with a current taxon name of BOSVILLE, 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 BOSVILLE were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Water Balance

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

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the BOSVILLE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

Select annual climate data summaries for the BOSVILLE series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the BOSVILLE 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 (updated 2024-10-23).

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

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

Competing Series

Soil series competing with BOSVILLE share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

Select annual climate data summaries for the BOSVILLE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the BOSVILLE 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 (updated 2024-10-23).

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 BOSVILLE, 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 (updated 2024-10-23).

Block Diagrams

No block diagrams are available.

Map Units

Map units containing BOSVILLE 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
Bosville fine sandy loam, 5 to 12 percent slopes	17	16608	571329	m5hz	ok005	1977	1:24000
Bosville fine sandy loam, 3 to 5 percent slopes	16	5207	571328	m5hy	ok005	1977	1:24000
Bosville fine sandy loam, 1 to 3 percent slopes	15	3208	571327	m5hx	ok005	1977	1:24000
Bernow-Bosville complex, 3 to 5 percent slopes, eroded	7	10633	381854	dtbw	ok013	1974	1:24000
Bosville fine sandy loam, 3 to 5 percent slopes	11	5126	381790	dt8t	ok013	1974	1:24000
Bosville fine sandy loam, 5 to 8 percent slopes	12	3055	381791	dt8v	ok013	1974	1:24000
Bosville fine sandy loam, 8 to 15 percent slopes	11	30847	571200	m5ct	ok023	1977	1:24000
Bosville fine sandy loam, 1 to 3 percent slopes	8	21836	571256	m5fm	ok023	1977	1:24000
Bosville fine sandy loam, 5 to 8 percent slopes	9	13737	571257	m5fn	ok023	1977	1:24000
Bernow, Bosville, and Romia soils, 3 to 8 percent slopes, gullied	6	8170	571253	m5fj	ok023	1977	1:24000
Bosville fine sandy loam, 5 to 8 percent slopes, eroded	10	2644	571199	m5cs	ok023	1977	1:24000
Bosville loam, 3 to 5 percent slopes	CeC	7132	571589	m5sc	ok029	1969	1:24000
Bosville fine sandy loam, 3 to 5 percent slopes	BvlC	116	1714833	1vkf6	ok069	1976	1:24000
Bernow, Romia, and Bosville soils, 2 to 12 percent slopes, gullied	6	7311	571314	m5hh	ok127	1977	1:24000
Bosville fine sandy loam, 5 to 12 percent slopes	10	2217	571260	m5fr	ok127	1977	1:24000
Bosville fine sandy loam, 3 to 5 percent slopes	9	872	571320	m5hp	ok127	1977	1:24000

Map of Series Extent

Approximate geographic distribution of the BOSVILLE 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 (updated 2024-10-30).