Soil Data Explorer - LINOYER

Official Series Description

Lab Data Summary

Aggregate lab data for the LINOYER soil series. This aggregation is based on all pedons with a current taxon name of LINOYER, 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 LINOYER 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
28A	78P0139	77NV033002	Linoyer	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9757767,-114.5469437
28A	67C0018	S1967UT039007	Linoyer	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.1402779,-111.839447
28A	67C0019	S1967UT039010	Linoyer	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.0463905,-111.8691635
28A	71C0035	S1971UT039006	Linoyer	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.1680565,-111.8024979
28B	86P0807	86NV023004	Linoyer	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.121666,-116.0536118
28B	89P0573	89NV007008	Linoyer	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.3452797,-114.2980576
28B	81P0660	S1981NV033028	Linoyer	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.0354958,-114.7580795
29	87P0281	87NV023009	Linoyer	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9902115,-115.6119843

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LINOYER 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 LINOYER series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the LINOYER 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 LINOYER 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).

Competing Series

Soil series competing with LINOYER share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the LINOYER 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 LINOYER 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.

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

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with LINOYER, 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

No block diagrams are available.

Map Units

Map units containing LINOYER 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
Linoyer-Heist association	1100	34	2480497	2p851	nv713	2014	1:24000
Blimo-Kunzler-Linoyer association	1210	17087	478605	j20w	nv766	1994	1:24000
Linoyer-Okan association	371	11649	478311	j1qd	nv766	1994	1:24000
Palinor-Shabliss-Linoyer association	857	10554	478503	j1xl	nv766	1994	1:24000
Wintermute-Linoyer association	119	9350	478221	j1mh	nv766	1994	1:24000
Timpie-Piltdown-Linoyer association	373	7140	478313	j1qg	nv766	1994	1:24000
Toano-Linoyer association	101	7104	478208	j1m2	nv766	1994	1:24000
Tulase-Linoyer association	1480	6343	478648	j228	nv766	1994	1:24000
Zerk-Automal-Linoyer association	900	6042	478518	j1y2	nv766	1994	1:24000
Shabliss-Tulase-Linoyer association	700	4502	478434	2wbj1	nv766	1994	1:24000
Sodhouse-Linoyer association	496	4232	478359	j1ry	nv766	1994	1:24000
Wintermute-Linoyer-Okan association	174	4044	478240	j1n3	nv766	1994	1:24000
Palinor-Automal-Linoyer association	858	3762	478504	j1xm	nv766	1994	1:24000
Threesee-Linoyer-Okan association	1411	1527	478635	j21v	nv766	1994	1:24000
Keefa-Lyx-Linoyer association	3747	2462	2634084	2rn3s	nv776	1983	1:63360
Linoyer-Clowfin association	3973	1022	2634090	2rn3z	nv776	1983	1:63360
Linoyer-Heist-Tulase association	232	417	2634045	2rn2h	nv776	1983	1:63360
Linoyer very fine sandy loam, 0 to 4 percent slopes	3972	381	2634089	2rn3y	nv776	1983	1:63360
Linoyer-Rebel association	3970	153	2634088	2rn3x	nv776	1983	1:63360
Shabliss-Tulase-Linoyer association	6455	8	2215797	2dcqb	nv778	2013	1:24000
Linoyer-Escalante association	3170	10033	480012	j3h8	nv779	2004	1:24000
Toano-Linoyer association	1030	2909	479923	j3dd	nv779	2004	1:24000
Rouette-Linoyer association	3218	2623	480033	j3hy	nv779	2004	1:24000
Linoyer-Tulase-Shabliss association	3177	1055	480014	j3hb	nv779	2004	1:24000
Jericho-Linoyer association	1298	968	479947	j3f5	nv779	2004	1:24000
Wintermute-Linoyer association	1040	580	479924	j3df	nv779	2004	1:24000
Pyrat-Linoyer association	1121	223	479935	j3ds	nv779	2004	1:24000
Shabliss-Tulase-Linoyer association	455	19179	480487	2wbj1	nv780	1990	1:24000
Linoyer-Heist-Tulase association	232	18772	480357	j3vd	nv780	1990	1:24000
Pyrat-Linoyer association	189	14210	480336	j3tq	nv780	1990	1:24000
Blimo-Linoyer-Tulase association	992	7375	480655	j450	nv780	1990	1:24000
Tosser-Pyrat-Linoyer association	166	5925	480306	j3sr	nv780	1990	1:24000
Kunzler-Linoyer association	642	4270	480561	j41z	nv780	1990	1:24000
Pyrat-Shabliss-Linoyer association	1492	3826	480278	j3rv	nv780	1990	1:24000
Linoyer very fine sandy loam, 0 to 4 percent slopes	231	2640	480356	2whnh	nv780	1990	1:24000
Linoyer-Katelana association	230	2135	480355	j3vb	nv780	1990	1:24000
Linoyer silt loam, 0 to 2 percent slopes	233	1120	480358	j3vf	nv780	1990	1:24000
Linoyer-Rebel association	1970	12046	480839	j4by	nv781	1994	1:24000
Linoyer-Rebel association	3970	26803	481083	j4lt	nv783	1991	1:24000
Linoyer-Kunzler association	3974	20979	481087	j4ly	nv783	1991	1:24000
Linoyer very fine sandy loam, 0 to 4 percent slopes	3972	10956	481085	2whnh	nv783	1991	1:24000
Linoyer-Easychair association	3971	1858	481084	j4lv	nv783	1991	1:24000
Keefa-Lyx-Linoyer association	3747	1436	481040	j4kf	nv783	1991	1:24000
Linoyer-Clowfin association	3973	1189	481086	j4lx	nv783	1991	1:24000
Chuffa-Linoyer-Playas complex	2071	23785	481190	j4q8	nv784	2006	1:24000
Linoyer-Heist association	1100	18178	481126	j4n6	nv784	2006	1:24000
Crestline-Linoyer association	2061	1410	481188	j4q6	nv784	2006	1:24000
Linoyer-Escalante association	3170	690	1395629	1hv89	nv784	2006	1:24000
Linoyer very fine sandy loam, 2 to 5 percent slopes	LaC	35082	482539	2smc4	ut608	1981	1:24000
Linoyer very fine sandy loam, 5 to 10 percent slopes, eroded	LaD2	4317	482540	j63t	ut608	1981	1:24000
Linoyer very fine sandy loam, 0 to 1 percent slopes	LaA	3402	482537	j63q	ut608	1981	1:24000
Linoyer very fine sandy loam, 1 to 2 percent slopes	LaB	2771	482538	j63r	ut608	1981	1:24000
Thiokol-Linoyer complex, 0 to 5 percent slopes	TcC	1773	482634	j66v	ut608	1981	1:24000
Linoyer loam, 0 to 2 percent slopes	82	2712	481881	j5fk	ut618	1995	1:24000
Kessler-Linoyer complex, 0 to 2 percent slopes	75	2211	481871	j5f7	ut618	1995	1:24000
Heist-Linoyer complex, 0 to 8 percent slopes	55	981	481849	j5dj	ut618	1995	1:24000
Linoyer very fine sandy loam, 2 to 5 percent slopes	83	915	481882	2smc4	ut618	1995	1:24000
Linoyer very fine sandy loam, 2 to 5 percent slopes, eroded	LdC2	5720	482278	j5vc	ut627	1971	1:24000
Linoyer very fine sandy loam, 1 to 2 percent slopes	LdB	2780	482277	j5vb	ut627	1971	1:24000
Linoyer very fine sandy loam, 2 to 5 percent slopes, eroded	163	23	483551	j75f	ut628		1:24000

Map of Series Extent

Approximate geographic distribution of the LINOYER 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).