Soil Data Explorer - BONILLA

Official Series Description

Lab Data Summary

Aggregate lab data for the BONILLA soil series. This aggregation is based on all pedons with a current taxon name of BONILLA, 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 BONILLA 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 BONILLA 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 BONILLA series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-02) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the BONILLA 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 2023-10-09).

Geomorphic description summaries for the BONILLA 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 2023-10-04).

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

Competing Series

Soil series competing with BONILLA share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-02) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the BONILLA 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 2023-10-09).

Geomorphic description summaries for the BONILLA 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 2023-10-04).

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

Soil series sharing subgroup-level classification with BONILLA, 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 2023-10-02).

Block Diagrams

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

1. SD-2010-11-01-17 | Spink County - 2009

   Pattern of soils and underlying materials in the Hand-Ethan-Bonilla and Northville-Farmsworth-Durrstein associations (Soil Survey of Spink County, South Dakota; 2009).

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

   Pattern of soils and underlying material in the Clarno-Crossplain-Davison association (Soil Survey of Bon Homme County, SD; 1983).

3. SD-2012-03-14-04 | Bon Homme County - January 1983

   Pattern of soils and underlying material in the Clarno-Ethan-Bonilla association (Soil Survey of Bon Homme County, SD; 1983).

4. SD-2012-03-14-15 | Clark County - 1999

   Typical pattern of soils and underlying material in the Clarno-Bonilla-Ethan association (Soil Survey of Clark County, SD; 1999).

5. SD-2012-03-15-43 | Hand County - April 1963

   A typical cross section of the northeastern part of Hand County (Soil Survey of Hand County, SD; 1963).

6. SD-2012-03-15-44 | Hand County - April 1963

   A cross section typical in both the south-central and northwestern parts of Hand County (Soil Survey of Hand County, SD; 1963).

7. SD-2012-03-15-65 | Kingsbury County - November 1997

   Typical pattern of soils and underlying material in the Clarno-Bonilla-Ethan association (Soil Survey of Kingsbury County, SD; 1997).

8. SD-2012-03-15-77 | Miner County - December 1984

   Pattern of soils and parent material in the Clarno-Bonilla-Crossplain association (Soil Survey of Miner County, SD; 1984).

9. SD-2012-03-15-79 | Miner County - December 1984

   Pattern of soils and parent material in the Clarno-Stickney association (Soil Survey of Miner County, SD; 1984).

10. SD-2012-03-16-01 | Turner County - November 1982

    Pattern of soils and parent material in the Clarno-Crossplain-Davison association (Soil Survey of Turner County, SD; 1982).

Map Units

Map units containing BONILLA 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
Clarno-Bonilla loams, 0 to 2 percent slopes	CpA	17641	354837	2wbq1	sd003	1979	1:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopes	CeC	2981	354836	2wknz	sd003	1979	1:20000
Hand-Bonilla loams, 3 to 6 percent slopes	HaB	85925	354580	2yygw	sd005	1976	1:20000
Hand-Bonilla loams, 0 to 3 percent slopes	HaA	13951	354579	2yyhk	sd005	1976	1:20000
Clarno-Bonilla loams, 0 to 2 percent slopes	CmA	32695	418252	2wbq1	sd009	1981	1:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopes	CsB	28953	418255	2wkny	sd009	1981	1:20000
Clarno-Bonilla loams, 1 to 6 percent slopes	CmB	8715	418253	2wknw	sd009	1981	1:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopes	EnC	7991	418269	2wknz	sd009	1981	1:20000
Bonilla-Crossplain complex	Br	2333	418250	g16y	sd009	1981	1:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopes	CeB	3658	355010	2wkny	sd023	1980	1:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopes	CeC	1762	355011	2wknz	sd023	1980	1:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopes	CeB	2856	417705	2wkny	sd025	1992	1:20000
Clarno-Bonilla loams, 0 to 2 percent slopes	CbA	2690	417703	2wbq1	sd025	1992	1:20000
Clarno-Bonilla loams, 1 to 6 percent slopes	CbB	969	417704	2wknw	sd025	1992	1:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopes	CeC	159	417706	2wknz	sd025	1992	1:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopes	ChB	38678	352911	2wkny	sd035	1966	1:20000
Clarno-Bonilla loams, 0 to 2 percent slopes	ChA	35650	352910	2wbq1	sd035	1966	1:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopes	CeC	6667	352909	2wknz	sd035	1966	1:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopes	CnB	32427	354883	2wkny	sd043	1979	1:20000
Clarno-Bonilla loams, 0 to 2 percent slopes	CpA	16571	354884	2wbq1	sd043	1979	1:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopes	CeC	4107	354881	2wknz	sd043	1979	1:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopes	CpB	25797	356413	2wkny	sd073	1987	1:20000
Clarno-Bonilla loams, 0 to 2 percent slopes	CrA	21476	356415	2wbq1	sd073	1987	1:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopes	CpC	4200	356414	2wknz	sd073	1987	1:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopes	CeB	45024	417465	2wkny	sd077	1992	1:20000
Clarno-Bonilla loams, 0 to 2 percent slopes	CbA	24258	417463	2wbq1	sd077	1992	1:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopes	CeC	3449	417466	2wknz	sd077	1992	1:20000
Clarno-Bonilla loams, 1 to 6 percent slopes	CbB	1743	417464	2wknw	sd077	1992	1:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopes	CeC	3107	416478	2wknz	sd079	1967	1:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopes	CeB	1121	416477	2wkny	sd079	1967	1:20000
Clarno-Bonilla loams, 0 to 2 percent slopes	CaA	1069	416474	2wbq1	sd079	1967	1:20000
Clarno-Bonilla loams, 0 to 2 percent slopes	CdA	42424	418013	2wbq1	sd087	1976	1:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopes	EbC	16468	418025	2wknz	sd087	1976	1:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopes	ChB	11478	418016	2wkny	sd087	1976	1:20000
Hand-Bonilla loams, 0 to 3 percent slopes	HbA	6995	418028	2yyhk	sd087	1976	1:20000
Clarno-Bonilla loams, 0 to 2 percent slopes	CfA	39775	355386	2wbq1	sd097	1983	1:20000
Clarno-Bonilla loams, 1 to 6 percent slopes	CfB	39275	355387	2wknw	sd097	1983	1:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopes	CkB	23474	355389	2wkny	sd097	1983	1:20000
Grovena-Bonilla loams, 0 to 2 percent slopes	GvA	2659	446048	gz4n	sd099	1995	1:24000
Dobalt-Bonilla loams, 0 to 2 percent slopes	DyA	462	446030	gz42	sd099	1995	1:24000
Grovena-Bonilla loams, 0 to 2 percent slopes	GvA	5756	418333	g19m	sd101	1985	1:20000
Doland-Bonilla loams, 0 to 2 percent slopes	DvA	4117	418320	g196	sd101	1985	1:20000
Clarno-Bonilla loams, 0 to 2 percent slopes	CoA	36498	354771	2wbq1	sd111	1978	1:20000
Clarno-Bonilla loams, 1 to 6 percent slopes	ChB	26203	354768	2wknw	sd111	1978	1:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopes	CmB	26179	354770	2wkny	sd111	1978	1:20000
Hand-Bonilla loams, 0 to 2 percent slopes	HaA	2136	354790	2xhcv	sd111	1978	1:20000
Hand-Ethan-Bonilla loams, 1 to 6 percent slopes	HgB	26657	356642	2yygx	sd115	1997	1:24000
Hand-Ethan-Bonilla loams, 2 to 9 percent slopes	HgC	5291	356643	2yygy	sd115	1997	1:24000
Hand-Bonilla loams, 0 to 3 percent slopes	HcA	4815	356637	2yyhk	sd115	1997	1:24000
Hand-Bonilla loams, 1 to 6 percent slopes	HcB	247	356638	2xhd0	sd115	1997	1:24000
Clarno-Bonilla loams, 0 to 2 percent slopes	ChA	21991	418213	2wbq1	sd125	1980	1:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopes	CoB	21180	418217	2wkny	sd125	1980	1:20000
Clarno-Bonilla loams, 1 to 6 percent slopes	ChB	19713	418214	2wknw	sd125	1980	1:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopes	CoC	7006	418218	2wknz	sd125	1980	1:20000
Clarno-Bonilla loams, 1 to 6 percent slopes	CeB	48499	418065	2wknw	sd135	1977	1:20000
Clarno-Bonilla loams, 0 to 2 percent slopes	CdA	13292	418064	2wbq1	sd135	1977	1:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopes	EnC	12574	418082	2wknz	sd135	1977	1:20000
Bonilla-Crossplain complex, 0 to 2 percent slopes	BnA	1077	418059	g10s	sd135	1977	1:20000
Clarno-Bonilla loams, 0 to 2 percent slopes	CdA	240736	417943	2wbq1	sd602	1975	1:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopes	CnC	18574	417947	2wknz	sd602	1975	1:20000
Hand-Bonilla loams, 0 to 3 percent slopes	HcA	1299	417977	2yyhk	sd602	1975	1:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopes	EuB	618	417968	2wkny	sd602	1975	1:20000

Map of Series Extent

Approximate geographic distribution of the BONILLA 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 2023-10-04).