Soil Data Explorer - BONFRI

Official Series Description

Lab Data Summary

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

Competing Series

Soil series competing with BONFRI 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 BONFRI 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 BONFRI 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 flats position figure.

Soil series sharing subgroup-level classification with BONFRI, 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 BONFRI 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
Twilight-Bonfri complex, 8 to 15 percent slopes	269D	13608	343060	2yk10	mt011	1992	1:24000
Bonfri-Parchin complex, 2 to 8 percent slopes	391C	11512	343102	2yk0y	mt011	1992	1:24000
Bonfri-Cabbart loams, 8 to 15 percent slopes	291D	8929	343073	2yvmt	mt011	1992	1:24000
Bonfri loam, 2 to 8 percent slopes	91C	8840	343277	2yk0v	mt011	1992	1:24000
Bonfri-Cambeth complex, 2 to 8 percent slopes	191C	7465	343001	2yk0x	mt011	1992	1:24000
Twilight-Bonfri complex, 2 to 8 percent slopes	269C	6920	343059	2yk0z	mt011	1992	1:24000
Bonfri loam, 8 to 15 percent slopes	91D	1291	343278	2yk0w	mt011	1992	1:24000
Bonfri loam, 2 to 8 percent slopes	602C	15	343560	2yk0v	mt017	1995	1:24000
Bonfri-Cabbart loams, 8 to 15 percent slopes	291D	13273	342193	2yvmt	mt025	1991	1:24000
Bonfri-Cambeth complex, 2 to 8 percent slopes	191C	9467	342144	2yk0x	mt025	1991	1:24000
Bonfri loam, 2 to 8 percent slopes	91C	6214	342312	2yk0v	mt025	1991	1:24000
Bonfri-Parchin complex, 2 to 8 percent slopes	391C	4637	342220	2yk0y	mt025	1991	1:24000
Twilight-Bonfri complex, 8 to 15 percent slopes	269D	2663	342180	2yk10	mt025	1991	1:24000
Twilight-Bonfri complex, 2 to 8 percent slopes	269C	2573	342179	2yk0z	mt025	1991	1:24000
Bonfri loam, 8 to 15 percent slopes	91D	1386	342313	2yk0w	mt025	1991	1:24000
Bonfri-Bullock, eroded-Cabbart complex, 4 to 25 percent slopes	13E	2028	342802	2yk11	mt033	2002	1:24000
Bonfri-Cabbart loams, 2 to 8 percent slopes	354C	2922	1715945	2yk18	mt065	1996	1:24000
Cabbart-Bonfri loams, 4 to 15 percent slopes	354D	1431	1715946	2yt5n	mt065	1996	1:24000
Bonfri-Cabbart loams, 0 to 4 percent slopes	354B	356	1887082	2yk17	mt065	1996	1:24000
Bonfri-Beenom-Cabbart loams, 2 to 8 percent	Cx	4670	345412	2zg52	mt103	1961	1:20000
Cabbart-Bonfri loams, 2 to 8 percent slopes	453C	1131	1946669	2yk0j	mt103	1961	1:20000
Bonfri-Cabbart loams, 0 to 4 percent slopes	354B	142	1946668	2yk17	mt103	1961	1:20000
Cabbart-Bonfri loams, 2 to 8 percent slopes	453C	29411	1883531	2yk0j	mt111	1966	1:20000
Bonfri-Cabbart loams, 0 to 4 percent slopes	354B	27714	1869336	2yk17	mt111	1966	1:20000
Bonfri-Cabbart loams, 2 to 8 percent slopes	354C	31	1913844	2yk18	mt111	1966	1:20000
Bonfri-Cabbart loams, 2 to 8 percent slopes	354C	123	2514000	cgj0	mt624	2021	1:24000
Foreleft-Bonfri loams, 3 to 15 percent slopes	282	236	1387762	1hl2j	mt643	1967	1:20000
Bonfri, deep-Bonfri fine sandy loams, 0 to 6 percent slopes	257	80	1387751	1hl25	mt643	1967	1:20000
Bonfri-Twilight-Blacksheep fine sandy loams, wooded, 3 to 30 percent slopes	259	38	1387752	1hl26	mt643	1967	1:20000
Bonfri-Galbreth fine sandy loams, 1 to 8 percent slopes	34	11544	348064	2yk15	mt649	1985	1:24000
Bonfri-Marmarth-Bullock fine sandy loams, 1 to 4 percent slopes	35	9105	348065	2yk16	mt649	1985	1:24000
Bonfri-Bullock, eroded-Cabbart complex, 4 to 25 percent slopes	33	9019	348063	2yk11	mt649	1985	1:24000
Cabbart-Bonfri loams, 2 to 8 percent slopes	453C	1	1946671	2yk0j	mt649	1985	1:24000
Bonfri-Lambeth complex, 2 to 8 percent slopes	16	21253	348145	2yk13	mt655	1975	1:24000
Bonfri-Lambeth complex, 8 to 15 percent slopes	17	3563	348146	2yk14	mt655	1975	1:24000
Bonfri-Cabbart loams, 2 to 8 percent slopes	154C	1345	1712541	2yk18	mt655	1975	1:24000
Bonfri-Cabbart loams, 0 to 4 percent slopes	354B	771	1914301	2yk17	mt655	1975	1:24000
Cabbart-Bonfri loams, 2 to 8 percent slopes	453C	391	1914302	2yk0j	mt655	1975	1:24000
Cabbart-Bonfri loams, 4 to 15 percent slopes	154D	40	1712542	2yt5n	mt655	1975	1:24000
Bonfri-Cabbart loams, 2 to 8 percent slopes	354C	4031	341651	2yk18	mt666	2008	1:24000
Cabbart-Bonfri loams, 4 to 15 percent slopes	354D	2010	341652	2yt5n	mt666	2008	1:24000
Bonfri-Twilight-Blacksheep fine sandy loams, wooded, 3 to 30 percent slopes	219	366	780116	v5s1	wy011	1978	1:24000
Bonfri, deep-Bonfri fine sandy loams, 0 to 6 percent slopes	218	47	780096	v5rd	wy011	1978	1:24000
Bonfri loam, 0 to 3 percent slopes	21	296	1153300	17q37	wy041		1:24000
Cabbart-Bonfri-Badland complex, 6 to 60 percent slopes	5428		3170888	2y62x	wy603		1:24000
Tymosling-like-Bonfri-Foreleft-like association 8 to 30 percent slopes	5476		3170890	2ypqh	wy603		1:24000
Bonfri-Foreleft-Geohrock complex, 6 to 35 percent slopes	S401		3170927	2z1yw	wy603		1:24000
Rangecreek-like-Bonfri-Foreleft complex, 2 to 15 percent slopes	722		2483590	2pcct	wy629		1:24000
Cabbart-Bonfri-Badland complex, 6 to 60 percent slopes	5428		2969116	2y62x	wy629		1:24000
Bonfri-Hawksell-like-Galbreth complex, 8 to 50 percent slopes	5443		2911918	2w7js	wy629		1:24000
Blacksheep-Dunlap, very stony-Bonfri, very stony complex, 20 to 50 percent slopes	5451		2911929	2w7k4	wy629		1:24000
Tymosling-like-Bonfri-Foreleft-like association 8 to 30 percent slopes	5476		3136911	2ypqh	wy629		1:24000
Broback-Bonfri-Bronec complex, 15 to 60 percent slopes	5571		3253231	2zthn	wy629		1:24000
Dunlap-Bonfri, very bouldery-Rock outcrop complex, 15 to 50 percent slopes	5835		3203110	2zbtc	wy629		1:24000
Bonfri-Archuleta-Badland complex, 8 to 35 percent slopes	9414		2911915	2w7jp	wy629		1:24000
Badland-Bonfri-Cabbart complex, 15 to 50 percent slopes	9506		3253274	2ztjm	wy629		1:24000
Bonfri-Raghigh complex, 4 to 15 percent slopes	740		2959854	2wsxf	wy630		1:24000
Shooter-Bonfri complex, 4 to 15 percent slopes	741		2959853	2wsxd	wy630		1:24000
Seminoe-Bonfri complex, 4 to 15 percent slopes	733		2959851	2wsxb	wy630		1:24000
Foreleft-Bonfri loams, 3 to 15 percent slopes	282	7065	817524	wfpr	wy705	2003	1:24000
Bonfri, deep-Bonfri fine sandy loams, 0 to 6 percent slopes	257	1473	817506	wfp5	wy705	2003	1:24000
Bonfri-Twilight-Blacksheep fine sandy loams, wooded, 3 to 30 percent slopes	259	1329	817647	wftq	wy705	2003	1:24000
Bonfri-Kirby complex, 0 to 10 percent slopes	258	732	817555	wfqr	wy705	2003	1:24000

Map of Series Extent

Approximate geographic distribution of the BONFRI 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).