Soil Data Explorer - LINNE

Official Series Description

Lab Data Summary

Aggregate lab data for the LINNE soil series. This aggregation is based on all pedons with a current taxon name of LINNE, 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 LINNE 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
15	40A3060	S1962CA083011	Linne	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.8172226,-120.3516693
15	40A0224	S1965CA053004	Linne	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.2833328,-121.0999985

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LINNE 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 LINNE 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 LINNE 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 LINNE 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 LINNE 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 LINNE 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 LINNE 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 LINNE, 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 LINNE 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
Linne clay loam, 5 to 15 percent slopes	LbD	1330	455809	h99j	ca013	1973	1:24000
Linne clay loam, 15 to 30 percent slopes, MLRA 15	LbE	1000	455810	2w63l	ca013	1973	1:24000
Linne clay loam, 3 to 15 percent slopes	LaCaa	1	843729	x9z2	ca013	1973	1:24000
Linne clay loam, 30 to 45 percent slopes, eroded	LaE2aa	1	843731	x9z4	ca013	1973	1:24000
Linne-Shedd silty clay loams, 50 to 75 percent slopes, eroded	LcG2	15700	455638	h940	ca053	1972	1:24000
Linne-Shedd silty clay loams, 15 to 50 percent slopes, eroded	LcF2	15110	455637	h93z	ca053	1972	1:24000
Linne-Shedd silty clay loams, 15 to 30 percent slopes	LcE	13030	455635	h93x	ca053	1972	1:24000
Linne-Shedd silty clay loams, 30 to 50 percent slopes	LcF	9055	455636	h93y	ca053	1972	1:24000
Linne silty clay loam, 15 to 30 percent slopes	LaE	7800	455631	h93s	ca053	1972	1:24000
Linne-Diablo complex, 15 to 30 percent slopes	LbE	6025	455634	h93w	ca053	1972	1:24000
Linne silty clay loam, 30 to 50 percent slopes	LaF	5675	455632	h93t	ca053	1972	1:24000
Linne silty clay loam 5 to 15 percent slopes	LaD	3300	455630	h93r	ca053	1972	1:24000
Linne-Diablo complex, 9 to 15 percent slopes	LbD	2875	455633	2x52r	ca053	1972	1:24000
Linne clay loam, 30 to 50 percent slopes, eroded, MLRA 15	LnF2	8750	456219	2w63n	ca069	1965	1:20000
Linne clay loam, 15 to 30 percent slopes, eroded	LnE2	6217	456218	h9qq	ca069	1965	1:20000
Linne-Shedd complex, 30 to 50 percent slopes, eroded	LsF2	5089	456222	h9qv	ca069	1965	1:20000
Diablo-Linne complex, 15 to 30 percent slopes, eroded	DlE2	1544	456189	h9ps	ca069	1965	1:20000
Linne clay loam, 30 to 50 percent slopes, severely erod ed	LnF3	1346	456220	h9qs	ca069	1965	1:20000
Diablo-Linne complex, 9 to 15 percent slopes	DlD	1227	456188	h9pr	ca069	1965	1:20000
Linne clay loam, 9 to 15 percent slopes, MLRA 15	LnD	967	456217	2w63p	ca069	1965	1:20000
Diablo-Linne complex, 30 to 50 percent slopes, eroded	DlF2	613	456190	h9pt	ca069	1965	1:20000
Linne-Shedd complex, 15 to 30 percent slopes, eroded	LsE2	353	456221	h9qt	ca069	1965	1:20000
Linne clay loam, 5 to 15 percent slopes	LbDcc		801715	vx7s	ca609	1963	1:20000
Linne clay loam, 15 to 30 percent slopes, MLRA 15	LaD	7201	456587	2w63l	ca609	1963	1:20000
Linne clay loam, 3 to 15 percent slopes	LaC	7083	456586	hb3l	ca609	1963	1:20000
Linne clay loam, 30 to 45 percent slopes, eroded	LaE2	6761	456588	hb3n	ca609	1963	1:20000
Linne clay loam, shallow, 45 to 75 percent slopes, eroded	LcF2	1797	456589	hb3p	ca609	1963	1:20000
Linne clay loam, 30 to 50 percent slopes	LsF	4816	456873	hbdv	ca638	1967	1:24000
Linne clay loam, 9 to 30 percent slopes	LsE	3870	456872	hbdt	ca638	1967	1:24000
Linne-Calodo complex, 9 to 30 percent slopes	152	20130	457255	hbt5	ca665	1977	1:24000
Linne-Calodo complex, 50 to 75 percent lsopes	154	13675	457257	hbt7	ca665	1977	1:24000
Linne-Calodo complex, 30 to 50 percent slopes	153	12680	457256	hbt6	ca665	1977	1:24000
Linne-Zakme complex, 30 to 50 percent slopes	156	3345	457259	hbt9	ca665	1977	1:24000
Linne-Diablo complex, 9 to 15 percent slopes	155	790	457258	2x52r	ca665	1977	1:24000
Linne clay loam, 30 to 45 percent slopes	LcF	9119	457419	hbzg	ca672	1966	1:20000
Linne clay loam, 45 to 75 percent slopes	LcG	2890	457420	hbzh	ca672	1966	1:20000
Linne clay loam, 15 to 30 percent slopes	LaE	2873	3356378	2zwtq	ca672	1966	1:20000
Linne clay loam, 9 to 15 percent slopes, MLRA 15	LcD	664	457417	2w63p	ca672	1966	1:20000
Linne clay loam, 30 to 50 percent slopes, eroded	LaF2	2404	3356350	2zwtr	ca673	1974	1:24000
Linne clay loam, 15 to 30 percent slopes	LaE	1020	3356349	2zwtq	ca673	1974	1:24000
Linne clay loam, 50 to 75 percent slopes	LaG	313	457607	hc5j	ca673	1974	1:24000
Linne silty clay loam, 30 to 50 percent slopes, eroded	LeF2	7358	457721	hc96	ca674	1968	1:24000
Linne silty clay loam, 15 to 30 percent slopes, eroded	LeE2	2948	457720	hc95	ca674	1968	1:24000
Linne silty clay loam, 9 to 15 percent slopes, eroded	LeD2	1300	457719	hc94	ca674	1968	1:24000
Linne-Los Osos-Haploxerepts association, 30 to 75 percent slopes	330	2	735081	snx9	ca676	1975	1:24000
Linne-Los Osos, warm-Calcic Haploxerepts association, 15 to 65 percent slopes	330	7005	469936	2y8sx	ca692	2001	1:24000
Linne silty clay loam, 15 to 50 percent slopes	331	1345	469937	hs08	ca692	2001	1:24000
Urban land-Linne-Los Osos, warm complex, 0 to 30 percent slopes	334	912	2403875	2y8ss	ca692	2001	1:24000
Linne silty clay loam, 9 to 15 percent slopes	332	500	469938	hs09	ca692	2001	1:24000
Linne-Calcic Haploxeralfs-Calcic Haploxerepts complex, 30 to 75 percent slopes	335	335	2403874	2lpfb	ca692	2001	1:24000
Calcic Haploxerepts-Linne-Haploxererts complex, 15 to 75 percent slopes	541	137	2403970	2lpjf	ca692	2001	1:24000

Map of Series Extent

Approximate geographic distribution of the LINNE 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).