Soil Data Explorer - ZANEIS

Official Series Description

Lab Data Summary

Aggregate lab data for the ZANEIS soil series. This aggregation is based on all pedons with a current taxon name of ZANEIS, 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 ZANEIS 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
80A	72-OK-60-4	72-OK119-60-4	Zaneis	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.151775,-97.3159778
80A	90P0709	90OK083002	Zaneis	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.1005554,-97.4588852
80A	91P0874	91OK083003	Zaneis	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.0066681,-97.4597244
80A	90P0708	S1990OK083001	Zaneis	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.086113,-97.3888855
84A	91P0904	S1991OK109003	Zaneis	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.7247238,-97.4563904

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ZANEIS 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 ZANEIS 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 ZANEIS 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 ZANEIS 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.

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

Competing Series

Soil series competing with ZANEIS 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 ZANEIS 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 ZANEIS 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 terrace figure.

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

Soil series sharing subgroup-level classification with ZANEIS, 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. OK-2010-09-29-06 | Logan County - 2006

   Typical pattern of soils and underlying material in the Coyle-Ironmound-Zaneis general soil map unit (Soil Survey of Logan County, Oklahoma; 2006).

2. OK-2012-02-16-15 | Comanche County - August 1967

   Topography and underlying material of major soils in northeastern part of county (Soil Survey of Comanche County, Oklahoma; August 1967).

3. OK-2012-02-16-17 | Comanche County - August 1967

   Topography and underlying material of Waurika soils and other extensive soils in southeastern part of county (Soil Survey of Comanche County, Oklahoma; August 1967).

4. OK-2012-02-16-20 | Cotton County - December 1963

   Typical pattern of Zaneis, Lucien, and associated soils in the northeastern part of Cotton County (Soil Survey of Cotton County, Oklahoma; December 1963).

5. OK-2012-02-16-23 | Cotton County - December 1963

   Schematic diagram showing the location of the Chickasha and other extensive soils in the east-central part of Cotton County (Soil Survey of Cotton County, Oklahoma; December 1963).

6. OK-2012-02-16-33 | Garfield County - October 1967

   Typical pattern of soils in the Renfrow-Vernon-Kirkland association (Soil Survey of Garfield County, Oklahoma; October 1967).

7. OK-2012-02-17-03 | Logan County - June 1960

   Soils of the Zaneis-Lucien-Chickasha and the Renfrow-Vernon-Kirkland associations on red clays, sandstone, siltstone, and alluvium. They have developed largely on the Wellington, Garber, and Hennessey formations that dip successively toward the west (Soil Survey of Logan County, Oklahoma; June 1960).

8. OK-2012-02-17-08 | Love County - September 1966

   Diagram showing typical relief in the northwestern corner of the county and the relative positions of the soils in association 4 (Soil Survey of Love County, Oklahoma; September 1966).

9. OK-2012-02-17-15 | Oklahoma County - February 1969

   Typical pattern of soils in soil association 2 (Soil Survey of Oklahoma County, Oklahoma; February 1969).

10. OK-2012-02-17-22 | Pawnee County - March 1959

    Prairie soils of western Pawnee County formed in clay and sandy strata of the Permian "redbeds" area, and in accompanying alluvium (Soil Survey of Pawnee County, Oklahoma; March 1959).

11. OK-2012-02-17-27 | Payne County - April 1987

    Typical pattern of soils and underlying material in the Renfrow-Coyle-Grainola map unit (Soil Survey of Payne County, Oklahoma; April 1987).

12. OK-2012-02-17-51 | Stephens County - 1964

    Typical pattern of soils in associations 6, 7, and 8 (Soil Survey of Stephens County, Oklahoma; 1964).

Map Units

Map units containing ZANEIS 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
Zaneis loam, 3 to 5 percent slopes	58	1437	382044	dtk0	ok019	1977	1:24000
Zaneis-Huska complex, 1 to 3 percent slopes	ZsB	43942	382218	2tq65	ok031	1965	1:24000
Lucien-Grainola-Zaneis complex, 5 to 12 percent slopes	LzD	36012	382191	30c0k	ok031	1965	1:24000
Zaneis and Stephenville soils, 2 to 8 percent slopes, severely eroded	Et	17371	382172	30c0t	ok031	1965	1:24000
Zaneis loam, 3 to 5 percent slopes, moderately eroded	ZaC2	14595	382217	2tq6y	ok031	1965	1:24000
Zaneis loam, 1 to 3 percent slopes	ZaB	10201	382215	2tp4j	ok031	1965	1:24000
Zaneis loam, 3 to 5 percent slopes	ZaC	8961	382216	2tp4l	ok031	1965	1:24000
Zaneis-Huska complex, 1 to 3 percent slopes	ZsB	28535	382263	2tq65	ok033	1961	1:24000
Zaneis-Grainola-Lucien complex, 5 to 20 percent slopes	Lz	16242	382237	dtr7	ok033	1961	1:24000
Zaneis loam, 1 to 3 percent slopes	ZaB	10780	382259	2tp4j	ok033	1961	1:24000
Zaneis loam, 3 to 5 percent slopes, moderately eroded	ZaC2	3309	382261	2tq6y	ok033	1961	1:24000
Zaneis loam, 3 to 5 percent slopes	ZaC	1219	382260	2tp4l	ok033	1961	1:24000
Zaneis loam, 3 to 8 percent slopes, severely eroded	Zn3	355	382262	2tq6x	ok033	1961	1:24000
Zaneis-Huska complex, 1 to 5 percent slopes	ZaHC	10	2516359	2tq6v	ok037	1952	1:24000
Zaneis loam, 1 to 3 percent slopes	ZaB	1120	382536	2tp4j	ok047	1965	1:24000
Zaneis loam, 3 to 5 percent slopes, moderately eroded	ZaC2	717	382538	2tq6y	ok047	1965	1:24000
Zaneis loam, 3 to 5 percent slopes	ZaC	555	382537	2tp4l	ok047	1965	1:24000
Zaneis loam, 3 to 5 percent slopes, moderately eroded	88	19049	382624	2tq6y	ok049	1982	1:24000
Zaneis loam, 3 to 5 percent slopes, gullied	89	6739	382625	dv4r	ok049	1982	1:24000
Zaneis loam, 1 to 3 percent slopes	86	6208	382622	2tp4j	ok049	1982	1:24000
Zaneis loam, 3 to 5 percent slopes	87	5006	382623	2tp4l	ok049	1982	1:24000
Zaneis loam, 3 to 5 percent slopes, moderately eroded	65	28954	382688	2tq6y	ok051	1975	1:24000
Zaneis loam, 3 to 8 percent slopes, severely eroded	66	20860	382689	2tq6x	ok051	1975	1:24000
Zaneis loam, 1 to 3 percent slopes	63	5947	382686	2tp4j	ok051	1975	1:24000
Zaneis loam, 3 to 5 percent slopes	64	3114	382687	2tp4l	ok051	1975	1:24000
Zaneis-Pawhuska complex, 0 to 3 percent slopes	ZwB	140555	383270	2wrk7	ok067	1967	1:24000
Zaneis, Lucien, and Grainola soils, 5 to 12 percent slopes	ZvD	107302	383269	2xm2m	ok067	1967	1:24000
Zaneis loam, 1 to 3 percent slopes	ZaB	10239	383266	2tp4j	ok067	1967	1:24000
Zaneis loam, 3 to 5 percent slopes, moderately eroded	ZaC2	2202	383268	2tq6y	ok067	1967	1:24000
Zaneis loam, 3 to 5 percent slopes	ZaC	2036	383267	2tp4l	ok067	1967	1:24000
Zaneis loam, 3 to 5 percent slopes	ZaC	3864	383549	2tp4l	ok081	1966	1:24000
Zaneis loam, 3 to 5 percent slopes, eroded	ZaC2	2857	383550	dw3l	ok081	1966	1:24000
Zaneis loam, 3 to 5 percent slopes, moderately eroded	ZanC2	18461	383695	2tq6y	ok083	1994	1:12000
Zaneis loam, 1 to 3 percent slopes	ZanB	8407	383693	2tp4j	ok083	1994	1:12000
Zaneis-Huska complex, 3 to 5 percent slopes	ZaHC	5484	383692	dw85	ok083	1994	1:12000
Coyle and Zaneis soils, 3 to 5 percent slopes, severely eroded	CoZC3	4185	383601	2wrk5	ok083	1994	1:12000
Zaneis loam, 3 to 5 percent slopes	ZanC	701	383694	2tp4l	ok083	1994	1:12000
Zaneis and Durant soils, 1 to 5 percent slopes, severely eroded	Et	2219	383713	dw8v	ok085	1963	1:24000
Chickasha and Zaneis soils, 1 to 3 percent slopes	ChB	879	383700	dw8f	ok085	1963	1:24000
Zaneis loam, 3 to 5 percent slopes	ZaC	493	383763	dwbg	ok085	1963	1:24000
Zaneis-Huska complex, 1 to 5 percent slopes	ZaHC	6806	384127	2tq6v	ok103	1994	1:24000
Coyle and Zaneis soils, 3 to 5 percent slopes, severely eroded	CoZC3	2682	384041	2wrk5	ok103	1994	1:24000
Zaneis loam, 1 to 3 percent slopes	ZanB	277	384128	2tp4j	ok103	1994	1:24000
Zaneis loam, 1 to 3 percent slopes	ZanB	1127	384379	2tp4j	ok109	1996	1:12000
Zaneis-Urban land complex, 1 to 5 percent slopes	ZaUC	660	384378	dwz9	ok109	1996	1:12000
Zaneis loam, 3 to 5 percent slopes	ZanC	657	384380	2tp4l	ok109	1996	1:12000
Zaneis loam, 3 to 5 percent slopes, moderately eroded	ZanC2	536	384381	2tq6y	ok109	1996	1:12000
Zaneis-Huska complex, 1 to 5 percent slopes	ZaHC	5875	1423193	2tq6v	ok117	2007	1:24000
Zaneis-Huska complex, 1 to 5 percent slopes, eroded	ZaHC2	920	1883799	2177q	ok117	2007	1:24000
Zaneis loam, 1 to 3 percent slopes	ZanB	665	1423192	2tp4j	ok117	2007	1:24000
Coyle and Zaneis soils, 3 to 5 percent slopes, severely eroded	CoZC3	225	1677021	2wrk5	ok117	2007	1:24000
Zaneis-Huska complex, 1 to 5 percent slopes	ZaHC	10458	1907649	2tq6v	ok119	1983	1:24000
Coyle and Zaneis soils, 3 to 5 percent slopes, severely eroded	76	7323	384577	2wrk5	ok119	1983	1:24000
Zaneis loam, 3 to 5 percent slopes, moderately eroded	71	3109	384572	2tq6y	ok119	1983	1:24000
Zaneis loam, 1 to 3 percent slopes	ZanB	1316	1907648	2tp4j	ok119	1983	1:24000
Zaneis loam, 3 to 5 percent slopes	70	1239	384571	2tp4l	ok119	1983	1:24000
Chickasha and Zaneis soils and Gullied land, 1 to 8 percent slopes, severely eroded	8	16849	384723	2yhdy	ok125	1975	1:24000
Zaneis loam, 3 to 5 percent slopes	57	11371	384720	2tp4l	ok125	1975	1:24000
Zaneis loam, 1 to 3 percent slopes	56	2971	384719	2tp4j	ok125	1975	1:24000
Zaneis-Grainola-Lucien complex, 5 to 12 percent slopes	Lz	37710	384867	dxh2	ok137	1960	1:24000
Zaneis-Ashport frequently flooded complex, 0 to 12 percent slopes	Ba	24234	384846	dxgd	ok137	1960	1:24000
Zaneis loam, 5 to 8 percent slopes	ZaD	13425	384897	dxj1	ok137	1960	1:24000
Zaneis loam, 3 to 5 percent slopes	ZaC	10508	384895	2tp4l	ok137	1960	1:24000
Chickasha and Zaneis soils and Gullied land, 1 to 8 percent slopes, severely eroded	Et	8889	384861	2yhdy	ok137	1960	1:24000
Zaneis loam, 3 to 5 percent slopes, moderately eroded	ZaC2	4008	384896	2tq6y	ok137	1960	1:24000
Zaneis loam, 1 to 3 percent slopes	ZaB	3475	384894	2tp4j	ok137	1960	1:24000

Map of Series Extent

Approximate geographic distribution of the ZANEIS 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).