Soil Data Explorer - COOLVILLE

Official Series Description

Lab Data Summary

Aggregate lab data for the COOLVILLE soil series. This aggregation is based on all pedons with a current taxon name of COOLVILLE, 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 COOLVILLE 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
114B	JN7803	1978IN071003	Coolville	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.8605278,-86.0113222
114B	90P0293	89IN143004	Coolville	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.6005554,-85.8375015
114B	03N0619	S2003IN019001	Coolville	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.5636101,-85.7811127
n/a	MG-S01	1954-OH105-S01	Coolville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MG-s06	1957-OH105-S06	Coolville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MG-s07	1957-OH105-S07	Coolville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MG-s09	1957-OH105-S09	Coolville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	RO-053	1958-OH141-053	Coolville	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MG-s10	1959-OH105-S10	Coolville	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	RO-066	1959-OH141-066	Coolville	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	PK-s10	1960-OH131-S10	Coolville	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	JF-w01	1962-OH081-W01	Coolville	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	WS-015	1968-OH167-015	Coolville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	PK-003	1979OH131003	Coolville	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	SC-012	1980OH145012	Coolville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

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

Select annual climate data summaries for the COOLVILLE 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 COOLVILLE 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 COOLVILLE share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-02) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the COOLVILLE 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 COOLVILLE 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 terrace figure.

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

Soil series sharing subgroup-level classification with COOLVILLE, 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. OH-2010-09-29-23 | Ross County - 2003

   Typical pattern of soils and parent material in the Cruze-Rossmoyne-Shelocta general soil map unit (Soil Survey of Ross County, Ohio; 2003).

2. OH-2012-02-16-40 | Scioto County - January 1989

   Typical pattern of soils and parent material in the Latham-Wharton-Shelocta association (Soil Survey of Scioto County, Ohio; January 1989).

3. WV-2010-11-08-06 | Jackson and Mason Counties -

   The typical pattern of upland soils and parent materials that are dominant throughout the survey area (Soil Survey of Jackson and Mason Counties, West Virginia).

4. WV-2010-11-08-07 | Jackson and Mason Counties -

   The dominant upland and high terrace soils in the Upper Flats area of northern Mason County. These high terrace soils have their origins associated with the ancient Teays River system (Soil Survey of Jackson and Mason Counties, West Virginia).

Map Units

Map units containing COOLVILLE 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
Coolville-Rarden-Stonehead silt loams, 12 to 18 percent slopes, eroded	ColD2	545	202290	6shh	in005	2002	1:12000
Rarden-Coolville complex, 12 to 22 percent slopes, severely eroded	RctD3	390	202291	6shj	in005	2002	1:12000
Stonehead-Coolville silt loams, 6 to 12 percent slopes, eroded	SucC2	386	202288	6shf	in005	2002	1:12000
Coolville-Rarden complex, 6 to 12 percent slopes, severely eroded	ConC3	56	246119	883b	in005	2002	1:12000
Coolville-Rarden complex, 12 to 18 percent slopes	ConD	4831	200943	6r31	in019	2001	1:12000
Coolville silt loam, 6 to 12 percent slopes	ComC	3204	200941	6r2z	in019	2001	1:12000
Coolville-Rarden complex, 6 to 12 percent slopes, severely eroded	ConC3	617	200942	6r30	in019	2001	1:12000
Rarden-Coolville complex, 12 to 22 percent slopes, severely eroded	RctD3	480	185181	66pl	in043	2000	1:12000
Coolville-Rarden complex, 6 to 12 percent slopes, severely eroded	ConC3	208	271437	93g1	in043	2000	1:12000
Coolville silt loam, 12 to 20 percent slopes	ComD	3599	1906761	2204f	in071	1985	1:15840
Stonehead-Coolville silt loams, 6 to 12 percent slopes, eroded	SucC2	11	620353	ntjd	in071	1985	1:15840
Coolville-Rarden complex, 6 to 12 percent slopes, severely eroded	ConC3	2	2027077	261bl	in071	1985	1:15840
Coolville-Rarden complex, 12 to 18 percent slopes	ConD	857	165633	5kc0	in143	1995	1:12000
Coolville silt loam, 6 to 12 percent slopes	ComC	280	165631	5kby	in143	1995	1:12000
Coolville silt loam, 6 to 12 percent slopes, severely eroded	ComC3	201	165632	5kbz	in143	1995	1:12000
Coolville silt loam, 1 to 8 percent slopes	CoB	585	536798	2x9zr	oh053	1988	1:15840
Coolville silt loam, 3 to 8 percent slopes	CpB	2	1460324	2x9zt	oh053	1988	1:15840
Coolville silt loam, 3 to 8 percent slopes	CoB	917	536015	2x9zt	oh079	1981	1:15840
Coolville-Tilsit silt loams, 2 to 6 percent slopes	CtB	8	1460507	1l0s4	oh079	1981	1:15840
Coolville-Tilsit silt loams, 2 to 6 percent slopes	CtB	1669	536139	kzwt	oh087	1989	1:15840
Rarden-Coolville silt loams, 12 to 18 percent slopes, moderately eroded	RcD2	330	537814	l1mv	oh111	1968	1:15840
Coolville-Rarden silt loams, 6 to 12 percent slopes, moderately eroded	CrC2	241	537761	l1l4	oh111	1968	1:15840
Coolville-Rarden silt loams, 12 to 18 percent slopes, moderately eroded	CrD2	158	537762	l1l5	oh111	1968	1:15840
Coolville silt loam, 1 to 8 percent slopes	CoB	9425	537618	2x9zr	oh131	1984	1:15840
Coolville-Blairton association, rolling	CpC	8657	537620	l1fl	oh131	1984	1:15840
Coolville silt loam, 8 to 15 percent slopes	CoC	2116	537619	2x9zw	oh131	1984	1:15840
Coolville-Rarden silt loams, 8 to 15 percent slopes	CtC	483	1689044	1tpl9	oh131	1984	1:15840
Coolville silt loam, 6 to 12 percent slopes, eroded	CmC2	194	1688996	2x9zv	oh131	1984	1:15840
Coolville silt loam, 2 to 6 percent slopes	CmB	124	1688995	2x9zs	oh131	1984	1:15840
Coolville silt loam, 6 to 12 percent slopes, eroded	CrC2	4595	170857	2x9zv	oh141	1997	1:15840
Coolville silt loam, 2 to 6 percent slopes	CrB	1743	170856	2x9zs	oh141	1997	1:15840
Coolville silt loam, 0 to 2 percent slopes	CrA	261	170855	2x9zq	oh141	1997	1:15840
Coolville-Rarden silt loams, 8 to 15 percent slopes	CpC	7911	537230	l110	oh145	1984	1:15840
Tilsit-Coolville association, undulating	TcB	5029	537319	l13w	oh145	1984	1:15840
Coolville silt loam, 1 to 8 percent slopes	CoB	1513	537229	2x9zr	oh145	1984	1:15840
Coolville silt loam, 3 to 8 percent slopes	CoB	450	513643	2x9zt	wv011	1984	1:20000
Coolville silt loam, 10 to 20 percent slopes	CoC	916	512833	2x9zx	wv039	1976	1:20000
Coolville silt loam, 3 to 10 percent slopes	CoB	444	512832	2xb1x	wv039	1976	1:20000
Coolville silty clay loam, 10 to 20 percent slopes, severely eroded	CrC3	263	512834	k6n1	wv039	1976	1:20000
Coolville silt loam, 3 to 8 percent slopes	CoB	800	513155	2x9zt	wv079	1981	1:20000
Coolville silt loam, 8 to 15 percent slopes	CoC	225	513156	2x9zw	wv079	1981	1:20000
Coolville and Tilsit soils, 3 to 8 percent slopes	CsB	12018	1384184	1hgc3	wv600	2005	1:24000
Coolville and Latham silt loams, 3 to 15 percent slopes	CTC	2870	2516634	261bd	wv713		1:24000
Coolville and Latham silt loams, 15 to 25 percent slopes	CTD	1174	2516635	261bf	wv713		1:24000

Map of Series Extent

Approximate geographic distribution of the COOLVILLE 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).