Soil Data Explorer - WINDTHORST

Official Series Description

Lab Data Summary

Aggregate lab data for the WINDTHORST soil series. This aggregation is based on all pedons with a current taxon name of WINDTHORST, 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 WINDTHORST 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
84A	70-OK-57-20	70-OK113-57-20	Windthorst	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.3868,-96.2278139
84A	70-OK-57-22	70-OK113-57-22	Windthorst	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.7555833,-96.1399583
84A	70-OK-62-2	70-OK123-62-2	Windthorst	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.78275,-96.5740306
84B	68-OK-10-8	68-OK019-10-8	Windthorst	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.0928,-97.160025
84B	70-OK-10-1	70-OK019-10-1	Windthorst	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.2495167,-97.2449528
84B	78P0389	77TX143001	Windthorst	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.2586098,-98.1927795
84B	96P0306	96TX143007	Windthorst	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.2525826,-98.2016907
84B	96P0307	96TX143008	Windthorst	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.245472,-98.1815033
84B	96P0308	96TX143009	Windthorst	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.2982483,-98.3027191
85	68-OK-62-1	68-OK123-62-1	Windthorst	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.78235,-96.8659667
85	40A4630	S1974TX367001	Windthorst	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.7288895,-97.8766632

Water Balance

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

Soil series sharing subgroup-level classification with WINDTHORST, 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-2012-02-16-16 | Comanche County - August 1967

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

2. OK-2012-02-17-07 | Love County - September 1966

   Diagram showing typical relief and relative positions of the soils in associations 2 and 5 in the north-central part of Love County (Soil Survey of Love County, Oklahoma; September 1966).

3. 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).

4. OK-2012-02-17-09 | Love County - September 1966

   Diagram showing relief typical of the central part of the county and the relative positions of the soils in association 7 (Soil Survey of Love County, Oklahoma; September 1966).

5. OK-2012-02-17-37 | Pontotoc County - April 1973

   Pattern of soils in the Stephenville-Darnell-Windthorst association (Soil Survey of Pontotoc County, Oklahoma; April 1973).

6. OK-2012-02-17-38 | Pontotoc County - April 1973

   Pattern of soils in the Chigley-Windthorst association (Soil Survey of Pontotoc County, Oklahoma; April 1973).

7. OK-2012-02-17-48 | Stephens County - 1964

   Typical pattern of soils in associations 1 and 5 (Soil Survey of Stephens County, Oklahoma; 1964).

8. TX-2010-11-03-44 | Jack County - 2005

   Typical pattern of soils and underlying material in the Duffau-Windthorst-Keeter general soil map unit (Soil Survey of Jack County, Texas; 2005).

9. TX-2012-03-22-19 | Wise County - May 1989

   Typical pattern of the Windthorst-Chaney-Selden general soil map unit (Soil Survey of Wise County, TX; 1989).

Map Units

Map units containing WINDTHORST 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
Windthorst-Weatherford complex, 5 to 12 percent slopes	55	77136	382041	2sz2w	ok019	1977	1:24000
Windthorst fine sandy loam, 3 to 8 percent slopes, eroded	53	24100	382039	2tc3w	ok019	1977	1:24000
Windthorst fine sandy loam, 3 to 5 percent slopes	52	14261	382038	2tc3t	ok019	1977	1:24000
Windthorst very fine sandy loam, 1 to 3 percent slopes	51	9677	382037	2tc3q	ok019	1977	1:24000
Windthorst-Darnell-Rock outcrop complex, 5 to 25 percent slopes	54	9460	382040	2tc3z	ok019	1977	1:24000
Windthorst sandy loam, 3 to 5 percent slopes	WhC	4518	382214	30kzr	ok031	1965	1:24000
Windthorst sandy loam, 1 to 3 percent slopes	WhB	3025	382213	30kzq	ok031	1965	1:24000
Windthorst-Weatherford complex, 5 to 12 percent slopes	WsD	26917	383761	2sz2w	ok085	1963	1:24000
Weatherford-Windthorst-Konsil complex, 1 to 8 percent slopes, severely eroded	Sw3	22261	383744	dw9v	ok085	1963	1:24000
Windthorst-Darnell-Rock outcrop complex, 5 to 25 percent slopes	Wn	5934	383760	2tc3z	ok085	1963	1:24000
Windthorst fine sandy loam, 1 to 5 percent slopes	WdC	2780	383758	2tc3r	ok085	1963	1:24000
Windthorst fine sandy loam, 1 to 5 percent slopes, eroded	WdC2	1703	383759	2tc3s	ok085	1963	1:24000
Windthorst fine sandy loam, 1 to 5 percent slopes, moderately eroded	WoB2	5778	363031	2zht3	tx035	1977	1:24000
Hico and Windthorst sandy clay loams, 1 to 8 percent slopes, severely eroded	HwD3	4065	363032	2zhsz	tx035	1977	1:24000
Windthorst very fine sandy loam, 1 to 5 percent slopes	WoB	2906	363029	2zht2	tx035	1977	1:24000
Windthorst very fine sandy loam, 1 to 5 percent slopes	WoB	2599	3221186	2zht2	tx093	1974	1:20000
Hico and Windthorst sandy clay loams, 1 to 8 percent slopes, severely eroded	HwD3	1987	3221185	2zhsz	tx093	1974	1:20000
Windthorst fine sandy loam, 1 to 5 percent slopes, moderately eroded	WoB2	29	3221187	2zht3	tx093	1974	1:20000
Windthorst and Duffau soils, 2 to 8 percent slopes, severely eroded	21	4346	364469	2tc22	tx097	1973	1:24000
Duffau-Windthorst complex, 1 to 5 percent slopes, moderately eroded	19	3989	364466	2xmd9	tx097	1973	1:24000
Windthorst fine sandy loam, 5 to 8 percent slopes	83	3366	364537	2tc3v	tx097	1973	1:24000
Windthorst fine sandy loam, 1 to 5 percent slopes	82	2661	364536	2tc3r	tx097	1973	1:24000
Windthorst loamy fine sand, 5 to 8 percent slopes	81	957	364535	d7b6	tx097	1973	1:24000
Windthorst loamy fine sand, 1 to 5 percent slopes	80	676	364534	2tc3x	tx097	1973	1:24000
Windthorst very fine sandy loam, 1 to 5 percent slopes	WoB	987	3221198	2zht2	tx133	1972	1:20000
Hico and Windthorst sandy clay loams, 1 to 8 percent slopes, severely eroded	HwD3	784	3221196	2zhsz	tx133	1972	1:20000
Windthorst fine sandy loam, 1 to 5 percent slopes	WnBC	332	3221197	2zht1	tx133	1972	1:20000
Windthorst fine sandy loam, 1 to 5 percent slopes, moderately eroded	WoB2	31643	365418	2zht3	tx143	1966	1:20000
Hico and Windthorst sandy clay loams, 1 to 8 percent slopes, severely eroded	HwD3	24750	365371	2zhsz	tx143	1966	1:20000
Windthorst loamy fine sand, 1 to 5 percent slopes	WnC	16664	365416	2tc3x	tx143	1966	1:20000
Windthorst very fine sandy loam, 1 to 5 percent slopes	WoB	15882	365417	2zht2	tx143	1966	1:20000
Windthorst and Duffau sandy clay loams, 1 to 8 percent slopes, severely eroded	WnD3	11270	365422	2zht0	tx143	1966	1:20000
Windthorst fine sandy loam, 1 to 5 percent slopes	WnBC	1469	365419	2zht1	tx143	1966	1:20000
Windthorst fine sandy loam, 1 to 5 percent slopes, eroded	WdC3	20042	366884	d9rz	tx187	1973	1:20000
Windthorst fine sandy loam, 1 to 3 percent slopes	WdB	2551	366883	d9ry	tx187	1973	1:20000
Windthorst fine sandy loam, 1 to 5 percent slopes, moderately eroded	WoB2	3580	376672	2zht3	tx193	1994	1:24000
Windthorst very fine sandy loam, 1 to 5 percent slopes	WoB	3513	376671	2zht2	tx193	1994	1:24000
Hico and Windthorst sandy clay loams, 1 to 8 percent slopes, severely eroded	HwD3	453	3221223	2zhsz	tx193	1994	1:24000
Windthorst fine sandy loam, 1 to 5 percent slopes	WnBC	9169	368068	2zht1	tx237	1992	1:24000
Windthorst and Duffau soils, 2 to 8 percent slopes, severely eroded	45	45775	370792	2tc22	tx337	1975	1:24000
Windthorst fine sandy loam, 1 to 5 percent slopes	43	39863	370790	2tc3r	tx337	1975	1:24000
Windthorst fine sandy loam, 5 to 8 percent slopes	44	33162	370791	2tc3v	tx337	1975	1:24000
Duffau-Windthorst complex, 1 to 5 percent slopes, moderately eroded	15	19153	370759	2xmd9	tx337	1975	1:24000
Windthorst loamy fine sand, 1 to 5 percent slopes	42	8060	370789	2tc3x	tx337	1975	1:24000
Windthorst fine sandy loam, 1 to 5 percent slopes	WnBC	3764	390979	2zht1	tx363	1979	1:24000
Windthorst fine sandy loam, 1 to 5 percent slopes, moderately eroded	WoB2	7	3221231	2zht3	tx363	1979	1:24000
Windthorst fine sandy loam, 1 to 5 percent slopes, moderately eroded	WoB2	40374	390921	2zht3	tx367	1973	1:20000
Duffau-Windthorst complex, 1 to 5 percent slopes, moderately eroded	DwC2	24416	390876	2xmd9	tx367	1973	1:20000
Windthorst and Duffau sandy clay loams, 1 to 8 percent slopes, severely eroded	WnD3	11866	390924	2zht0	tx367	1973	1:20000
Windthorst loamy fine sand, 1 to 5 percent slopes	WnC	7724	390918	2tc3x	tx367	1973	1:20000
Windthorst fine sandy loam, 1 to 5 percent slopes	WnBC	5498	390920	2zht1	tx367	1973	1:20000
Windthorst very fine sandy loam, 1 to 5 percent slopes	WoB	4264	390919	2zht2	tx367	1973	1:20000
Windthorst-Urban land complex, 2 to 8 percent slopes	WuD	515	390923	2xmf9	tx367	1973	1:20000
Hico and Windthorst sandy clay loams, 1 to 8 percent slopes, severely eroded	HwD3	208	3221245	2zhsz	tx367	1973	1:20000
Windthorst very fine sandy loam, 1 to 5 percent slopes	WoB	1136	372437	2zht2	tx439	1979	1:20000
Duffau-Windthorst complex, 1 to 5 percent slopes, moderately eroded	DwC2	497	3054445	2xmd9	tx439	1979	1:20000
Windthorst fine sandy loam, 1 to 5 percent slopes, moderately eroded	WoB2	124	372439	2zht3	tx439	1979	1:20000
Windthorst fine sandy loam, 1 to 5 percent slopes	WtC	21779	373704	2tc3r	tx497	1984	1:20000
Duffau-Windthorst complex, 1 to 5 percent slopes, moderately eroded	WeC	12821	373701	2xmd9	tx497	1984	1:20000
Windthorst fine sandy loam, 3 to 8 percent slopes, eroded	WtC3	10879	373705	2tc3w	tx497	1984	1:20000
Windthorst and Duffau sandy clay loams, 1 to 8 percent slopes, severely eroded	WnD3	577	3221255	2zht0	tx497	1984	1:20000
Windthorst fine sandy loam, 1 to 5 percent slopes, moderately eroded	WoB2	21333	374371	2zht3	tx609	1975	1:20000
Windthorst and Duffau sandy clay loams, 1 to 8 percent slopes, severely eroded	WnD3	8346	374373	2zht0	tx609	1975	1:20000
Windthorst very fine sandy loam, 1 to 5 percent slopes	WoB	7236	374369	2zht2	tx609	1975	1:20000
Windthorst loamy fine sand, 1 to 5 percent slopes	WnC	4689	374368	2tc3x	tx609	1975	1:20000
Windthorst fine sandy loam, 1 to 5 percent slopes	WnBC	952	374370	2zht1	tx609	1975	1:20000
Duffau-Windthorst complex, 1 to 5 percent slopes, moderately eroded	DwC2	943	374334	2xmd9	tx609	1975	1:20000
Hico and Windthorst sandy clay loams, 1 to 8 percent slopes, severely eroded	HwD3	240	374372	2zhsz	tx609	1975	1:20000

Map of Series Extent

Approximate geographic distribution of the WINDTHORST 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).