Soil Data Explorer - BON

Official Series Description

Lab Data Summary

Aggregate lab data for the BON soil series. This aggregation is based on all pedons with a current taxon name of BON, 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 BON 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 BON 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 BON 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 BON 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 BON 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.

Competing Series

Soil series competing with BON 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 BON 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 BON 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.

Soil series sharing subgroup-level classification with BON, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. SD-2010-11-01-12 | Minnehaha County - 2004

   Typical pattern of soils and parent material in the Clamo-Chaska association (Soil Survey of Minnehaha County, South Dakota; 2004).

2. SD-2012-03-14-06 | Bon Homme County - January 1983

   Pattern of soils and underlying material in the Eltree-Yankton-Alcester association (Soil Survey of Bon Homme County, SD; 1983).

3. SD-2012-03-15-16 | Davison County - January 1974

   Typical pattern of soils in associations 5 and 7 near the James River and Firesteel Creek (Soil Survey of Davison County, SD; 1974).

4. SD-2012-03-15-56 | Jerauld County - September 1994

   Pattern of soils and parent material in the Delmont-Ree-Canning association (Soil Survey of Jerauld County, SD; 1994).

5. SD-2012-03-15-57 | Jerauld County - September 1994

   Pattern of soils and parent material in the Homme-Peno association (Soil Survey of Jerauld County, SD; 1994).

6. SD-2012-03-15-86 | Moody County - April 1989

   Pattern of soils and parent material in the Dempster-Flandreau-Lamo association (Soil Survey of Moody County, SD; 1989).

Map Units

Map units containing BON 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
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Bx	5659	354833	2wkpn	sd003	1979	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	Bo	1395	354832	2wkpm	sd003	1979	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Bx	10136	354554	2wkpn	sd005	1976	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	La	4731	354589	2wkpm	sd005	1976	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Bo	7155	418249	2wkpn	sd009	1981	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	Bn	4248	418248	2wkpm	sd009	1981	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Bo	7753	355008	2wkpn	sd023	1980	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	Bn	4335	355007	2wkpm	sd023	1980	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	Bn	495	417695	2wkpm	sd025	1992	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Bo	384	417696	2wkpn	sd025	1992	1:20000
Ethan-Bon, channeled, loams, 0 to 20 percent slopes	EoD	101	417723	g0ny	sd025	1992	1:20000
Ethan-Bon, channeled, loams, 0 to 20 percent slopes	EpD	2876	445563	gyn0	sd027	1995	1:24000
Ethan-Clarno-Bon, channeled, loams, 0 to 9 percent slopes	EtC	2160	445568	gyn5	sd027	1995	1:24000
Bon loam, 0 to 2 percent slopes, occasionally flooded	Bm	1792	445534	2vwbn	sd027	1995	1:24000
Ethan-Clarno-Bon loams 0 to 6 percent slopes	EsB	1500	445567	gyn4	sd027	1995	1:24000
Ethan-Bon, channeled, loams, 0 to 40 percent slopes	EpE	1495	445564	gyn1	sd027	1995	1:24000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Bn	939	445535	2wkpn	sd027	1995	1:24000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Aa	6026	352898	2wkpn	sd035	1966	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	BoA	1426	352905	2wkpm	sd035	1966	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Bo	3779	354880	2wkpn	sd043	1979	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	Bn	1186	354879	2wkpm	sd043	1979	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	La	749	355173	2wkpm	sd049	1981	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Lb	620	355174	2wkpn	sd049	1981	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Bc	12035	355227	2wkpn	sd053	1982	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	Bb	2921	355226	2wkpm	sd053	1982	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	LbA	18825	352632	2wkpm	sd059	1959	1:20000
Bon-Northville complex, nearly level	LeA	9930	352635	ctyb	sd059	1959	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	LlA	7742	352636	2wkpn	sd059	1959	1:20000
Durrstein-Bon complex, nearly level	HdA	1993	352611	ctxk	sd059	1959	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	Bo	3549	353267	2wkpm	sd065	1970	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Bn	783	353783	2wkpn	sd069	1992	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Bv	5397	356410	2wkpn	sd073	1987	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	Br	3598	356409	2wkpm	sd073	1987	1:20000
Ethan-Bon, channeled, loams, 0 to 20 percent slopes	EoD	4554	417481	g0f4	sd077	1992	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Bo	4242	417458	2wkpn	sd077	1992	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	Bn	1442	417457	2wkpm	sd077	1992	1:20000
Bon soils, frequently flooded	Bo	2074	416624	fzjh	sd083	1971	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Ca	5422	418009	2wkpn	sd087	1976	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	Bo	2685	418008	2wkpm	sd087	1976	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Bo	5826	355383	2wkpn	sd097	1983	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	Bn	4281	355382	2wkpm	sd097	1983	1:20000
Bon loam, 0 to 2 percent slopes, occasionally flooded	Bo	4099	446005	2vwbn	sd099	1995	1:24000
Bon loam, 0 to 2 percent slopes, occasionally flooded	Bo	3076	418306	2vwbn	sd101	1985	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Bv	1411	355316	2wkpn	sd107	1983	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	Bo	791	355315	2wkpm	sd107	1983	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Bd	1642	354759	2wkpn	sd111	1978	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	Bu	2585	356572	2wkpm	sd115	1997	1:24000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Bw	2150	356573	2wkpn	sd115	1997	1:24000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Cc	6613	418210	2wkpn	sd125	1980	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	Ro	6529	418238	2wkpm	sd125	1980	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	Bn	200	354475	2wkpm	sd129	1975	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Rb	3059	418100	2wkpn	sd135	1977	1:20000
Bon loam, 0 to 2 percent slopes, occasionally flooded	Bm	2518	418058	2vwbn	sd135	1977	1:20000
Ethan-Bon, channeled, loams, 0 to 20 percent slopes	EsD	14	418124	g12w	sd135	1977	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Cb	16751	417941	2wkpn	sd602	1975	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	Bo	1254	417939	2wkpm	sd602	1975	1:20000
Bon loam, 0 to 2 percent slopes, rarely flooded	Bn	3442	355486	2wkpm	sd603	1983	1:20000
Bon loam, channeled, 0 to 2 percent slopes, frequently flooded	Bo	3233	355487	2wkpn	sd603	1983	1:20000

Map of Series Extent

Approximate geographic distribution of the BON 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).