Soil Data Explorer - CLEAR LAKE

Official Series Description

Lab Data Summary

Aggregate lab data for the CLEAR LAKE soil series. This aggregation is based on all pedons with a current taxon name of CLEAR LAKE, 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 CLEAR LAKE were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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	40A3087	S1961CA097009	Clear Lake	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.248333,-122.6086121
14	40A3088	S1961CA097010	Clear Lake	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.2705574,-122.6438904
17	79P0090	79CA095000	Clear Lake	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.3485069,-121.6993713
17	83P0299	82CA077004	Clear Lake	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.9427795,-121.1891632
17	89P0066	89CA011005	Clear Lake	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9958344,-121.9208298
17	91P0346	91CA099005	Clear Lake	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.601944,-121.2077789

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CLEAR LAKE 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 CLEAR LAKE 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 CLEAR LAKE 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 CLEAR LAKE 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 CLEAR LAKE 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 CLEAR LAKE 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 CLEAR LAKE 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 CLEAR LAKE, 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. CA-2012-05-08-17 | Alameda Area - March 1966

   The relationship of geologic formations, landforms, and soil series in the Alameda Area (Soil Survey of Alameda Area, California; March, 1966).

Map Units

Map units containing CLEAR LAKE 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
Clear Lake clay, 0 to 1 percent slopes, occasionally flooded, MLRA 17	115	17501	461556	2vbsr	ca011	1999	1:24000
Clear Lake clay, drained, 0 to 1 percent slopes, frequently flooded, MLRA 17	118	1727	461559	2vbtd	ca011	1999	1:24000
Clear Lake clay, calcareous, 0 to 2 percent slopes, occasionally flooded	116	1446	461557	hh8y	ca011	1999	1:24000
Clear Lake clay, drained, 0 to 8 percent slopes, MLRA 15	200	998	461590	2vbss	ca011	1999	1:24000
Clear Lake clay, calcareous, 0 to 1 percent slopes, frequently flooded	117	450	461558	hh8z	ca011	1999	1:24000
Clear Lake clay, 0 to 15 percent slopes, MLRA 15	Cc	19997	455777	2vbsq	ca013	1973	1:24000
Clear Lake clay, drained, 0 to 2 percent slopes, MLRA 14	CdAaa	3	843722	2vbt2	ca013	1973	1:24000
Clear Lake clay, drained, 3 to 7 percent slopes	CdBaa	1	843723	x9yw	ca013	1973	1:24000
Clear Lake clay, 0 to 4 percent slopes, MLRA 17	Cc	4019	458598	2vbsy	ca021	1961	1:20000
Clear Lake variant clay, drained	122	1809	459525	hf5d	ca033	1985	1:24000
Clear Lake clay, drained, 0 to 2 percent slopes, MLRA 15	121	1475	459524	2vbt4	ca033	1985	1:24000
Clear Lake clay, 0 to 2 percent slopes, MLRA 15	113	990	459405	2vbsx	ca041	1979	1:24000
Clear Lake clay, sandy substratum, drained, 0 to 1 percent slopes, MLRA 14	Cg	8170	455574	2vbt9	ca053	1972	1:24000
Clear Lake clay, 0 to 1 percent slopes, frequently flooded, MLRA 14	Cf	1810	455573	2vbtc	ca053	1972	1:24000
Clear Lake clay, drained, 0 to 2 percent slopes, MLRA 14	116	6645	458940	2vbt2	ca055	1974	1:24000
Clear Lake clay, overwashed	117	545	458941	hdkk	ca055	1974	1:24000
Clear Lake clay, hardpan substratum, drained, 0 to 1 percent slopes	115	16330	461859	hhlp	ca067	1989	1:24000
Clear Lake clay, partially drained, 0 to 2 percent slopes, frequently flooded	114	2770	461858	hhln	ca067	1989	1:24000
Clear Lake clay, saline, drained, 0 to 1 percent slopes, MLRA 14	Ck	5025	456170	2vbtf	ca069	1965	1:20000
Clear Lake clay, drained, low precip, 0 to 2 percent slopes, MLRA 14	Ch	4972	456169	2vbsm	ca069	1965	1:20000
Clear Lake silty clay loam, drained, 0 to 2 percent slopes, MLRA 15	Cl	293	456171	2vbsv	ca069	1965	1:20000
Clear Lake clay, drained, 0 to 1 percent slopes, MLRA 14	119	2500	455895	2vbtb	ca087	1976	1:24000
Clear Lake clay, 0 to 2 percent slopes, MLRA 17	CeA	15513	456066	2vbt0	ca095	1969	1:24000
Clear Lake clay, drained, 2 to 5 percent slopes, MLRA 15	CeB	1033	456067	2vbt7	ca095	1969	1:24000
Clear Lake clay, saline, drained, 0 to 2 percent slopes, MLRA 14	ClA	394	456068	2vbtg	ca095	1969	1:24000
Clear Lake clay, sandy substratum, 0 to 2 percent slopes	CeA	18523	459685	2vbsl	ca097	1968	1:20000
Clear Lake clay, ponded, 0 to 2 percent slopes	CfA	4621	3251973	2y8vg	ca097	1968	1:20000
Clear Lake clay loam, 0 to 2 percent slopes	CcA	4461	3251971	2y8vc	ca097	1968	1:20000
Clear Lake clay, sandy substratum, 2 to 5 percent slopes	CeB	2035	459686	2vbt8	ca097	1968	1:20000
Clear Lake clay loam, 2 to 5 percent slopes	CcB	1621	3251972	2y8vd	ca097	1968	1:20000
Clear Lake clay, 0 to 1 percent slopes, MLRA 17	112	30283	459322	2vbsz	ca101	1984	1:24000
Clear Lake clay, siltstone substratum, 0 to 2 percent slopes	115	4172	459325	hdyy	ca101	1984	1:24000
Clear Lake silt loam, 0 to 2 percent slopes	110	2436	459320	hdys	ca101	1984	1:24000
Clear Lake clay, drained, 0 to 1 percent slopes, frequently flooded, MLRA 17	113	2335	459323	2vbtd	ca101	1984	1:24000
Clear Lake silt loam, frequently flooded, 0 to 2 percent slopes	111	2253	459321	hdyt	ca101	1984	1:24000
Clear Lake clay, hardpan substratum, 0 to 2 percent slopes	114	2075	459324	hdyx	ca101	1984	1:24000
Clear Lake clay, siltstone substratum, frequently flooded, 0 to 2 percent slopes	116	766	459326	hdyz	ca101	1984	1:24000
Clear Lake soils, flooded	Cn	11671	459219	hdvj	ca113	1968	1:20000
Clear Lake clay, 0 to 1 percent slopes, MLRA 17	Ck	6949	459218	2vbsz	ca113	1968	1:20000
Clear Lake silty clay loam, drained, 0 to 1 percent slopes, MLRA17	Ch	402	459217	2vbt6	ca113	1968	1:20000
Clear Lake clay, 0 to 1 percent slopes, occasionally flooded, MLRA 17	115c	160	757751	2vbsr	ca113	1968	1:20000
Clear Lake clay, drained, 0 to 2 percent slopes, MLRA 14	CdA	5318	456568	2vbt2	ca609	1963	1:20000
Clear Lake clay, 0 to 3 percent slopes, MLRA 14	Cc	1716	456567	2vbt5	ca609	1963	1:20000
Clear Lake clay, drained, 3 to 7 percent slopes	CdB	1316	456569	hb31	ca609	1963	1:20000
Clear Lake clay, drained, 0 to 2 percent slopes, MLRA 14	107	8746	456660	2vbt2	ca610	1975	1:24000
Urban land-Clear Lake complex	148	4156	456701	hb79	ca610	1975	1:24000
Clear Lake clay, 2 to 9 percent slopes, drained	108	1518	456661	hb60	ca610	1975	1:24000
Clear Lake clay, 0 to 15 percent slopes, MLRA 15	Cccc	100	825140	2vbsq	ca610	1975	1:24000
Esquon-Clearlake , 0 to 1 percent slopes, frequently flooded	220	904	461163	hgw7	ca612	2005	1:24000
Clear Lake clay, drained, 0 to 1 percent slopes, frequently flooded, MLRA 17	118co	772	886404	2vbtd	ca612	2005	1:24000
Clearlake silty clay loam, 0 to 1 percent slopes, overwash, frequently flooded	522	696	461193	hgx6	ca612	2005	1:24000
Clear Lake clay, partially drained, 0 to 2 percent slopes	195	402	1403424	1j3cr	ca632	2006	1:24000
Urbanland-Clear Lake complex, 0 to 2 percent slopes	160	5172	1543359	1nszs	ca641	2009	1:24000
Clear Lake silty clay, 0 to 2 percent slopes, drained	161	444	1882926	216bk	ca641	2009	1:24000
Clear Lake silty clay, drained, 0 to 2 percent slopes, MLRA 17	195	825	466938	2vbsw	ca642	1998	1:24000
Clear Lake clay, drained, 0 to 2 percent slopes, occasionally flooded, MLRA 17	190	369	466937	2vbst	ca642	1998	1:24000
Clear Lake clay, 0 to 4 percent slopes, MLRA 17	Cc	1632	460698	2vbsy	ca645	1961	1:20000
Clear Lake clay, 0 to 2 percent slopes, occasionally flooded, MLRA 14	Cg	1856	456975	2vbsp	ca646	1967	1:24000
Clear Lake clay, drained, 0 to 2 percent slopes, MLRA 14	Ch	1396	456976	2vbt2	ca646	1967	1:24000
Clear Lake clay, saline, drained, 0 to 1 percent slopes, MLRA 14	Ck	558	456977	2vbtf	ca646	1967	1:24000
Clear Lake clay, drained, 0 to 2 percent slopes, MLRA 17	117	1679	463582	2vbt1	ca660	1977	1:24000
Clear Lake clay, drained, 0 to 1 percent slopes, MLRA 15	130	885	457233	2vbt3	ca665	1977	1:24000
Clear Lake clay	129	605	457232	hbsf	ca665	1977	1:24000
Clear Lake clay, high precip, 0 to 2 percent slopes, MLRA 14	112	1628	460997	2vbsn	ca687	1985	1:24000

Map of Series Extent

Approximate geographic distribution of the CLEAR LAKE 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).