Soil Data Explorer - BOOMER

Official Series Description

Lab Data Summary

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

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
14	UCD6449018	64-CA-49-018x	BOOMER	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.5110741,-122.8866043
15	UCD6445151	64-CA-45-151x	BOOMER	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.5992928,-122.5330505
18	UCD6758115	67-CA-58-115x	BOOMER	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.3912239,-121.2478485
18	40A2904	S1961CA017003	BOOMER	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.8477783,-120.9702759
18	40A2905	S1961CA017004	Boomer	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.8297234,-120.980278
20	40A2889	S1960CA073009	Boomer	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	33.0077782,-116.6033325
5	UCD6545159	65-CA-45-159x	BOOMER	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.1614876,-122.2871475
5	UCD6545160	65-CA-45-160x	BOOMER	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.1548767,-122.3112717
5	UCD7447106	74-CA-47-106x	BOOMER	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.2383347,-122.2616272
5	UCD7447112	74-CA-47-112x	BOOMER	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.2157021,-122.3160095
5	98P0318	97CA093001	BOOMER	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.0665169,-121.9666443
5	98P0319	97CA093002	BOOMER	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.0476303,-122.001091

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BOOMER 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 BOOMER 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 BOOMER 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 BOOMER 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 flats position figure.

Competing Series

Soil series competing with BOOMER 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 BOOMER 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 BOOMER 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 flats position figure.

Soil series sharing subgroup-level classification with BOOMER, 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 BOOMER 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
Boomer gravelly loam, 9 to 39 percent slopes, cool, MLRA 5	114mnf	14	2504868	2w8d6	ca033	1985	1:24000
Boomer-Forward-Felta complex, 30 to 50 percent slopes	110	8910	458934	hdkb	ca055	1974	1:24000
Boomer gravelly loam, volcanic bedrock, 14 to 60 percent slopes, MLRA 15	109	8745	458933	2w8d3	ca055	1974	1:24000
Boomer-Forward-Felta complex, 5 to 30 percent slopes	111	4505	458935	hdkc	ca055	1974	1:24000
Boomer loam, volcanic bedrock, 2 to 35 percent slopes, MLRA 15	107	1320	458931	2w8d7	ca055	1974	1:24000
Boomer gravelly loam, volcanic bedrock, 11 to 43 percent slopes, MLRA 15	108	1290	458932	2w8cz	ca055	1974	1:24000
Boomer loam, 2 to 15 percent slopes	107n		1607429	1qynk	ca097	1968	1:20000
Boomer loam, 50 to 75 percent slopes	BoG	8583	459679	hfbc	ca097	1968	1:20000
Boomer loam, 30 to 50 percent slopes	BoF	7317	459678	hfbb	ca097	1968	1:20000
Boomer loam, 7 to 50 percent slopes, moist, MLRA 15	BoE	2036	459677	2w8db	ca097	1968	1:20000
Hugo-Boomer complex, 50 to 75 percent slopes	HmG	1831	459770	hff9	ca097	1968	1:20000
Hugo-Boomer complex, 30 to 50 percent slopes	HmF	901	459769	hff8	ca097	1968	1:20000
Stonyford-Boomer complex, 30 to 75 percent slopes	SrG	692	459889	hfk4	ca097	1968	1:20000
Marpa-Kinkel-Boomer, cool complex, 15 to 50 percent slopes	184	80230	459093	hdqg	ca602	1978	1:24000
Marpa-Kinkel-Boomer, cool complex, 5 to 15 percent slopes	183	5800	459092	hdqf	ca602	1978	1:24000
Boomer loam, cool, 5 to 30 percent slopes	115	2190	459024	hdn7	ca602	1978	1:24000
Boomer variant sandy loam, 30 to 50 percent slopes	117	2050	459026	hdn9	ca602	1978	1:24000
Boomer variant stony sandy loam, 5 to 30 percent slopes	118	575	459027	hdnb	ca602	1978	1:24000
Boomer, cool-Neuns complex, 30 to 70 percent slopes	116	560	459025	hdn8	ca602	1978	1:24000
Boomer gravelly loam, 13 to 52 percent slopes, MLRA 15	BkE	4746	459946	2w8d4	ca607	1967	1:20000
Boomer very stony loam, 50 to 70 percent slopes	BlF	3239	459947	hfm0	ca607	1967	1:20000
Boomer gravelly loam, 15 to 30 percent slopes	BkD	2547	459945	hfly	ca607	1967	1:20000
Boomer very stony clay loam, 30 to 50 percent slopes, severely eroded	BoE3	1374	459948	hfm1	ca607	1967	1:20000
Boomer gravelly loam, 0 to 15 percent slopes	BkC	1027	459944	hflx	ca607	1967	1:20000
Boomer very stony clay loam, 50 to 70 percent slopes, severely eroded	BoF3	600	459949	hfm2	ca607	1967	1:20000
Boomer-Pendola-Sites complex, 2 to 30 percent slopes	127	3095	460418	hg36	ca618	1991	1:24000
Boomer-Pendola-Sites complex, 30 to 50 percent slopes	128	2415	460420	hg38	ca618	1991	1:24000
Boomer gravelly loam, 8 to 35 percent slopes, dry	124	1680	460412	2w8d2	ca618	1991	1:24000
Boomer gravelly loam, 13 to 41 percent slopes, dry	125	775	460414	2w8d5	ca618	1991	1:24000
Boomer gravelly loam, 8 to 15 percent slopes	123	415	460410	hg2y	ca618	1991	1:24000
Boomer-Pendola complex, 50 to 75 percent slopes	126	170	460416	hg34	ca618	1991	1:24000
Boomer, hard bedrock - Rock outcrop complex, 5 to 30 percent slopes	BrD	18561	460191	2w8df	ca619	1970	1:24000
Boomer, hard bedrock - Rock outcrop complex, 15 to 60 percent slopes	BrE	15459	460192	2w8dh	ca619	1970	1:24000
Boomer loam, 5 to 15 percent slopes	BoC	4310	460189	hfvt	ca619	1970	1:24000
Boomer loam, hard bedrock, 7 to 28 percent slopes	BoD	2932	460190	2w8dc	ca619	1970	1:24000
Boomer variant very stony sandy loam, 15 to 50 percent slopes	128	2615	460292	hfz4	ca620	1975	1:24000
Boomer - Rock outcrop complex, 15 to 50 percent slopes	125	2600	460289	2w8dj	ca620	1975	1:24000
Boomer - Rock outcrop complex, 5 to 30 percent slopes	124	1900	460288	2w8dg	ca620	1975	1:24000
Boomer-Rock outcrop complex, 50 to 70 percent slopes	126	900	460290	hfz2	ca620	1975	1:24000
Boomer loam, 3 to 22 percent slopes	122	820	460286	2w8d8	ca620	1975	1:24000
Boomer variant stony sandy loam, 2 to 15 percent slopes	127	650	460291	hfz3	ca620	1975	1:24000
Boomer loam, backslopes, 7 to 34 percent slopes	123	600	460287	2w8dd	ca620	1975	1:24000
Boomer very rocky loam, 30 to 50 percent slopes	BkE	10361	462209	hhyz	ca624	1968	1:20000
Boomer very rocky loam, 3 to 30 percent slopes	BkD	4204	462208	hhyy	ca624	1968	1:20000
Boomer-Sites very rocky loams, 9 to 50 percent slopes	BrE	3559	462213	hhz3	ca624	1968	1:20000
Boomer very rocky loam, 50 to 70 percent slopes	BkF	1925	462210	hhz0	ca624	1968	1:20000
Boomer gravelly loam, 8 to 35 percent slopes, dry	BhD	1773	462207	2w8d2	ca624	1968	1:20000
Boomer-Sites loams, 15 to 30 percent slopes	BpD	1703	462212	hhz2	ca624	1968	1:20000
Boomer gravelly loam, 3 to 15 percent slopes	BhC	1466	462206	hhyw	ca624	1968	1:20000
Rescue very stony sandy loam, 30 to 50 percent slopes	RfE	1155	462274	hj12	ca624	1968	1:20000
Boomer-Sites loams, 9 to 15 percent slopes	BpC	593	462211	hhz1	ca624	1968	1:20000
Boomer stony loam, 30 to 65 percent slopes	BrG	8736	3295900	2zwr7	ca638	1967	1:24000
Boomer stony loam, 9 to 30 percent slopes	BrE	7232	3295906	2zwrq	ca638	1967	1:24000
Boomer sandy loam, 9 to 35 percent slopes	1303	2083	3295913	2zwrz	ca638	1967	1:24000
Boomer loam, 9 to 30 percent slopes	BoE	1216	3295905	2zwrp	ca638	1967	1:24000
Boomer loam, 2 to 9 percent slopes	BoC	413	456746	hb8r	ca638	1967	1:24000
Boomer loam, 4 to 23 percent slopes, cool	BoD	854	463256	2w8d9	ca649	1967	1:24000
Marpa-Kinkel-Boomer, cool complex, 15 to 50 percent slopes	184sc	5116	1905934	21z8r	ca702	1984	1:24000
Marpa-Kinkel-Boomer, cool complex, 5 to 15 percent slopes	183sc	221	1905932	21z8p	ca702	1984	1:24000
Boomer, cool-Neuns complex, 30 to 70 percent slopes	116sc	18	1905881	21z71	ca702	1984	1:24000
Boomer, cool-Neuns complex, 30 to 70 percent slopes	116sc	409	1867647	20pfp	ca707	1983	1:24000
Boomer gravelly loam, 30 to 50 percent slopes	BkEsh	243	1868326	20q4l	ca707	1983	1:24000
Boomer very stony clay loam, 50 to 70 percent slopes, severely eroded	BoF3sh	185	1868330	20q4q	ca707	1983	1:24000
Marpa-Kinkel-Boomer, cool complex, 15 to 50 percent slopes	184sc	107	1867674	20pgk	ca707	1983	1:24000
Boomer very stony loam, 50 to 70 percent slopes	BlFsh	88	1868328	20q4n	ca707	1983	1:24000
Boomer gravelly loam, 2 to 30 percent slopes, MLRA 15	BkDsh	80	1868324	2w8d1	ca707	1983	1:24000
Boomer loam, cool, 5 to 30 percent slopes	115sc	12	1867646	20pfn	ca707	1983	1:24000
Marpa-Kinkel-Boomer, cool complex, 5 to 15 percent slopes	183sc	10	1867672	20pgh	ca707	1983	1:24000
Boomer gravelly loam, 30 to 50 percent slopes	114	1518	2747795	2q1ym	ca709	2010	1:24000
Boomer-Boomer variant-Sites complex, 2 to 30 percent slopes	BSE	130	464614	hlgk	ca719	1982	1:24000
Boomer-Boomer variant-Sites complex, 30 to 50 percent slopes	BSF	33	464615	hlgl	ca719	1982	1:24000
Boomer loam, 2 to 15 percent slopes	BoDma	52	1674970	1t6y9	ca750	1983	1:24000
Boomer-Crozier-Rock outcrop complex, 5 to 40 percent slopes	681	7182	465260	hm4d	ca760	1981	1:24000

Map of Series Extent

Approximate geographic distribution of the BOOMER 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).