Soil Data Explorer - COLLINSVILLE

Official Series Description

Lab Data Summary

Aggregate lab data for the COLLINSVILLE soil series. This aggregation is based on all pedons with a current taxon name of COLLINSVILLE, 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 COLLINSVILLE 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
112	M9309724	1993MO097024	Collinsville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.2532694,-94.5756889
112	M9509713	1995MO097013	Collinsville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.3120222,-94.4135194
112	M9609709	1996MO097009	Collinsville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.3050417,-94.4168528
112	M0501138	2005MO011038	Collinsville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.5268333,-94.5773889
112	79-OK-66-1	79-OK131-66-1	Collinsville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.1913083,-95.479775
115B	M9105763	1991MO057063	Collinsville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9672203,-92.3450012
115B	M9205746	1992MO057046	Collinsville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9672203,-92.3450012
115B	M9205752	1992MO057052	Collinsville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9672203,-92.3450012
115B	M9318508	1993MO185008	Collinsville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9672203,-92.3450012
116A	M9703912	1997MO039130	Collinsville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.879202,-93.8464675

Water Balance

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

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

Competing Series

Soil series competing with COLLINSVILLE 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 COLLINSVILLE 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the COLLINSVILLE 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 2D hillslope position figure.

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

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 COLLINSVILLE, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. KS-2012-01-20-33 | Coffey County - July 1982

   Typical pattern of soils in Kenoma-Eram-Dennis association (Soil Survey of Coffey County, Kansas; 1982).

2. KS-2012-01-26-35 | Wilson County - February 1989

   Typical pattern of soils and parent material in the Bates-Collinsville-Dennis association (Soil Survey of Wilson County, Kansas; 1989).

3. OK-2012-02-16-07 | Cherokee and Delaware Counties - December 1970

   Major soils in soil association 2 and their relation to the landscape (Soil Survey of Cherokee and Delaware Counties, Oklahoma; December 1970).

4. OK-2012-02-16-48 | Hughes County - December 1968

   Typical pattern of soils in associations 1 and 2 (Soil Survey of Hughes County, Oklahoma; December 1968).

5. OK-2012-02-17-16 | Okmulgee County - May 1968

   Relationship of the Dennis, Bates, and Parsons soils to the soils of the Collinsville-Talihina and Hector-Hartsells associations (Soil Survey of Okmulgee County, Oklahoma; May 1968).

6. OK-2012-02-17-17 | Okmulgee County - May 1968

   Relationship of the Taloka and Choteau soils (upper right) to the soils of the Dennis-Bates-Parsons, Collinsville-Talihina, Hector-Hartsells, Konawa-Stidham, and Verdigris-Lightning-Pulaski associations. (The Deep Fork River is also known as the Deep Fork Canadian River) (Soil Survey of Okmulgee County, Oklahoma; May 1968).

7. OK-2012-02-17-18 | Okmulgee County - May 1968

   Soils of the Okemah-Woodson association (Soil Survey of Okmulgee County, Oklahoma; May 1968).

8. OK-2012-02-17-19 | Ottawa County - November 1964

   Major soil series in soil associations 1 and 3, and their relation to the landscape. Typical slope range is shown for the soil series (Soil Survey of Ottawa County, Oklahoma; November 1964).

9. OK-2012-02-17-21 | Pawnee County - March 1959

   Prairie soils of central and eastern Pawnee County formed in sandstone, shale, and limestone, and in accompanying alluvium (Soil Survey of Pawnee County, Oklahoma; March 1959).

10. OK-2012-02-17-34 | Pittsburg County - May 1971

    Major soils and underlying material in soil associations 5 and 6 (Soil Survey of Pittsburg County, Oklahoma; May 1971).

11. OK-2012-02-17-35 | Pontotoc County - April 1973

    Pattern of soils in the Dennis-Bates-Steedman association (Soil Survey of Pontotoc County, Oklahoma; April 1973).

12. OK-2012-02-17-43 | Rogers County - August 1966

    General locations of soil associations 1, 2, and 4 in a landscape that is typical of the central and eastern parts of Rogers County (Soil Survey of Rogers County, Oklahoma; August 1966).

13. OK-2012-02-17-46 | Sequoyah County - June 1970

    Typical pattern of soils in association 3 (Soil Survey of Sequoyah County, Oklahoma; June 1970).

14. OK-2012-02-17-55 | Washington County - November 1968

    Major soil series in soil associations 1 and 2, and their relation to the landscape (Soil Survey of Washington County, Oklahoma; November 1968).

Map Units

Map units containing COLLINSVILLE 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
Collinsville-Bates complex, 3 to 15 percent slopes	8673	3603	2740893	2wwdd	ks001	1975	1:24000
Bates-Collinsville complex, 3 to 15 percent slopes	8627	94	1427114	2tgt8	ks001	1975	1:24000
Collinsville-Bates complex, 3 to 15 percent slopes	8673	3307	2740894	2wwdd	ks003	1974	1:24000
Eram-Collinsville complex, 5 to 15 percent slopes	8749	537	1427972	2q01z	ks003	1974	1:24000
Eram-Collinsville complex, 5 to 15 percent slopes	8749	4916	1427067	2q01z	ks011	1979	1:24000
Collinsville-Bates complex, 3 to 15 percent slopes	8673	81	1427063	2wwdd	ks011	1979	1:24000
Eram-Collinsville complex, 1 to 5 percent slopes	8747	10970	1453407	1ksd3	ks019	1972	1:24000
Bates-Collinsville complex, 3 to 15 percent slopes	8627	53	1453396	2tgt8	ks019	1972	1:24000
Bates-Collinsville complex, 3 to 15 percent slopes	8627	4466	1426889	2tgt8	ks021	1983	1:24000
Eram-Collinsville complex, 5 to 15 percent slopes	8749	10466	1454612	2q01z	ks031	1980	1:24000
Eram-Collinsville complex, 5 to 15 percent slopes	8749	32	1387004	2q01z	ks037	1969	1:24000
Bates-Collinsville complex, 3 to 7 percent slopes	8626	271	1468867	2tgtc	ks045	1974	1:24000
Bates-Collinsville complex, 3 to 15 percent slopes	8627	24	1468868	2tgt8	ks045	1974	1:24000
Collinsville-Bates fine sandy loams, 2 to 8 percent slopes	6930	2630	1453308	30wzg	ks049	1984	1:24000
Bates-Collinsville complex, 1 to 3 percent slopes	8625	26	1453329	2tgtb	ks049	1984	1:24000
Bates-Collinsville complex, 3 to 15 percent slopes	8627	10784	1460718	2tgt8	ks059	1979	1:24000
Bates-Collinsville complex, 3 to 7 percent slopes	8626	7579	1460717	2tgtc	ks059	1979	1:24000
Eram-Collinsville complex, 5 to 15 percent slopes	8749	15	1453677	2q01z	ks073	1981	1:24000
Bates-Collinsville complex, 3 to 15 percent slopes	8627	5	1453666	2tgt8	ks073	1981	1:24000
Bates-Collinsville complex, 3 to 15 percent slopes	8627	6049	1426855	2tgt8	ks099	1987	1:24000
Bates-Collinsville complex, 1 to 3 percent slopes	8625	10	1426854	2tgtb	ks099	1987	1:24000
Collinsville-Bates complex, 3 to 15 percent slopes	8673	757	1427471	2wwdd	ks107	1979	1:24000
Bates-Collinsville complex, 3 to 15 percent slopes	8627	1979	1453734	2tgt8	ks111	1977	1:24000
Bates-Collinsville complex, 3 to 15 percent slopes	8627	35250	1426927	2tgt8	ks125	1978	1:24000
Bates-Collinsville complex, 1 to 3 percent slopes	8625	15679	1426925	2tgtb	ks125	1978	1:24000
Eram-Collinsville complex, 1 to 5 percent slopes	8747	14	1426937	1jwv7	ks125	1978	1:24000
Bates-Collinsville complex, 3 to 7 percent slopes	8626	6	1426926	2tgtc	ks125	1978	1:24000
Bates-Collinsville complex, 3 to 15 percent slopes	8627	3808	1427015	2tgt8	ks133	1980	1:20000
Bates-Collinsville complex, 1 to 3 percent slopes	8625	1834	1427014	2tgtb	ks133	1980	1:20000
Bates-Collinsville complex, 7 to 20 percent slopes	8628	20539	1426979	2tgtd	ks205	1985	1:20000
Bates-Collinsville complex, 3 to 7 percent slopes	8626	4403	1426977	2tgtc	ks205	1985	1:20000
Bates-Collinsville complex, 3 to 15 percent slopes	8627	3596	1426978	2tgt8	ks205	1985	1:20000
Bates-Collinsville complex, 1 to 3 percent slopes	8625	145	1426976	2tgtb	ks205	1985	1:20000
Eram-Collinsville complex, 5 to 15 percent slopes	8749	28489	1427195	2q01z	ks207	1973	1:20000
Bates-Collinsville complex, 7 to 20 percent slopes	8628	2026	1427179	2tgtd	ks207	1973	1:20000
Bates-Collinsville complex, 3 to 7 percent slopes	8626	122	1427178	2tgtc	ks207	1973	1:20000
Collinsville-Bates complex, 3 to 15 percent slopes	8673	83	1427183	2wwdd	ks207	1973	1:20000
Collinsville fine sandy loam, 2 to 5 percent slopes	40046	6082	886800	2wwf6	mo011	1969	1:24000
Collinsville fine sandy loam, 5 to 14 percent slopes	40047	5543	886801	2wwf7	mo011	1969	1:24000
Collinsville fine sandy loam, 2 to 14 percent slopes, stony	40048	3781	886802	2wwf9	mo011	1969	1:24000
Collinsville-Rock outcrop complex, 3 to 15 percent slopes	40010	1647	2532317	2zcd3	mo039	2001	1:24000
Collinsville-Rock outcrop complex, 3 to 15 percent slopes	40010	182	2532319	2zcd3	mo077	1979	1:24000
Collinsville fine sandy loam, 2 to 20 percent slopes	70112	96	2534192	2wwf8	mo083	1972	1:24000
Collinsville-Rock outcrop complex, 3 to 15 percent slopes	40010	112	2532316	2zcd3	mo109	1979	1:24000
Collinsville fine sandy loam, 2 to 20 percent slopes	70112	15455	2534191	2wwf8	mo185	1984	1:24000
Collinsville-Rock outcrop complex, 3 to 15 percent slopes	40010	475	2532318	2zcd3	mo185	1984	1:24000
Collinsville fine sandy loam, 3 to 12 percent slopes	19	707	381798	dt92	ok013	1974	1:24000
Collinsville-Vinita complex, 2 to 30 percent slopes	CoF	38748	106500	2xvh7	ok035	1968	1:20000
Bates-Collinsville complex, 1 to 5 percent slopes	BcC	8476	106491	2tgt9	ok035	1968	1:20000
Collinsville and Talihina soils, 5 to 12 percent slopes	Ce	39868	382272	2xvh9	ok037	1952	1:24000
Collinsville and Talihina soils, 12 to 20 percent slopes	Cf	19223	382273	2xvhb	ok037	1952	1:24000
Collinsville and Coweta soils, 1 to 3 percent slopes	Cd	7040	382271	2xvh8	ok037	1952	1:24000
Sobol and Collinsville soils, 5 to 20 percent slopes, stony	LdE	9675	571689	m5wl	ok061	1972	1:24000
Bates-Collinsville complex, 1 to 5 percent slopes	BcC	17940	106539	2tgt9	ok097	1972	1:24000
Collinsville loam, 5 to 30 percent slopes, extremely stony	CoE	16403	106547	2wwfb	ok097	1972	1:24000
Collinsville-Talihina complex, 10 to 30 percent slopes	CtE	50068	106454	2xvhc	ok111	1968	1:24000
Bates-Collinsville complex, 1 to 5 percent slopes	BcC	30467	106450	2tgt9	ok111	1968	1:24000
Collinsville stony loam, 3 to 20 percent slopes	Co	2627	106619	2wwdf	ok115	1961	1:24000
Talihina-Eram-Collinsville complex, 5 to 20 percent slopes	TcE	76712	571567	m5rn	ok121	1966	1:24000
Eram-Talihina-Collinsville complex, 3 to 15 percent slopes, rocky	ETCF	2888	697353	rdn8	ok121	1966	1:24000
Bates-Collinsville complex, 3 to 8 percent slopes	Bc	39498	106650	2xvgn	ok131	1963	1:24000
Collinsville stony loam, 3 to 20 percent slopes	Co	11391	106656	2wwdf	ok131	1963	1:24000

Map of Series Extent

Approximate geographic distribution of the COLLINSVILLE 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).