Soil Data Explorer - CONOTTON

Official Series Description

Lab Data Summary

Aggregate lab data for the CONOTTON soil series. This aggregation is based on all pedons with a current taxon name of CONOTTON, 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 CONOTTON 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
101	59PA049001	1959PA049001	Conotton	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.205,-79.8683333
115A	KX7515	1975IN083015	Conotton	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.588075,-87.5998
148	92P0342	91PA017008	Conotton	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.3827782,-74.9622192
n/a	AB-064	1955-OH007-064	Conotton	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	AB-099	1960-OH007-099	Conotton	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	LK-028	1971-OH085-028	Conotton	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	LK-018	1972-OH085-018	Conotton	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	KX7502	1975IN083002	Conotton	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	TU-017	1979-OH157-017	Conotton	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MG-001	1984-OH105-001	Conotton	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 CONOTTON 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 CONOTTON 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 CONOTTON 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 CONOTTON 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 CONOTTON 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 CONOTTON 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 CONOTTON 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 flats position figure.

Soil series sharing subgroup-level classification with CONOTTON, 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 CONOTTON 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
Conotton sandy loam, 0 to 3 percent slopes	CoA	6117	164471	5j4j	in083	1979	1:15840
Chili and Conotton gravelly loams, 12 to 18 percent slopes	CkD	2447	288150	9nv5	oh005	1976	1:15840
Chili and Conotton gravelly loams, 18 to 35 percent slopes	CkE	1096	288151	9nv6	oh005	1976	1:15840
Chili and Conotton soils, 12 to 18 percent slopes	CoD	16	1592605	1qg7c	oh005	1976	1:15840
Chili and Conotton soils, 18 to 25 percent slopes	CoE	12	1592606	1qg7d	oh005	1976	1:15840
Conotton gravelly loam, 2 to 12 percent slopes	CsC	1	1592607	1qg7f	oh005	1976	1:15840
Conotton gravelly loam, 2 to 6 percent slopes	CmB	431	298752	b0w5	oh029	2005	1:12000
Conotton gravelly loam, 6 to 12 percent slopes	CmC	201	298753	b0w6	oh029	2005	1:12000
Conotton loam, 2 to 6 percent slopes	CtB	940	172126	5s3g	oh043	1998	1:12000
Conotton gravelly loam, 6 to 12 percent slopes	CuC	146	172127	5s3h	oh043	1998	1:12000
Chili and Conotton gravelly loams, 18 to 35 percent slopes	CrE	5	1677341	1t9ds	oh075	1989	1:15840
Chili and Conotton gravelly loams, 12 to 18 percent slopes	CrD	4	1677340	1t9dr	oh075	1989	1:15840
Conotton gravelly loam, 2 to 6 percent slopes	CyB	1278	286798	9mfk	oh085	1976	1:15840
Conotton loam, 0 to 2 percent slopes	CxA	697	286797	9mfj	oh085	1976	1:15840
Conotton gravelly loam, 6 to 15 percent slopes	CyC	132	286799	9mfl	oh085	1976	1:15840
Conotton gravelly loam, 2 to 6 percent slopes	CoB	441	287748	9nf6	oh093	1972	1:15840
Conotton gravelly loam, 6 to 12 percent slopes	CoC	62	287749	9nf7	oh093	1972	1:15840
Chili and Conotton gravelly soils, 18 to 25 percent slopes	CnE	297	816741	wdwh	oh099	1966	1:15840
Chili and Conotton gravelly soils, 25 to 50 percent slopes	CnF	149	816742	wdwj	oh099	1966	1:15840
Conotton gravelly loam, 0 to 2 percent slopes	CnA	746	537147	2xqwf	oh105	1991	1:15840
Conotton gravelly loam, 18 to 40 percent slopes	CnE	278	537149	2xqwp	oh105	1991	1:15840
Conotton gravelly loam, 6 to 12 percent slopes	CnC	153	537148	2xqwm	oh105	1991	1:15840
Conotton gravelly loam, 0 to 2 percent slopes	CoA	108	537759	2xqwf	oh111	1968	1:15840
Conotton gravelly loam, 6 to 18 percent slopes	CoD	96	537760	2xqwn	oh111	1968	1:15840
Conotton gravelly loam, 3 to 8 percent slopes	Cnt6B1	355	3175562	2zfvf	oh115	1992	1:15840
Conotton gravelly loam, 6 to 12 percent slopes, eroded	CoC2	216	537430	2xqwk	oh115	1992	1:15840
Conotton gravelly loam, 0 to 3 percent slopes	Cnt6A1	77	3175561	2zfvd	oh115	1992	1:15840
Conotton gravelly loam, 18 to 25 percent slopes, moderately eroded	CyE2	1	1717872	1vnl7	oh133	1973	1:15840
Chili and Conotton soils, 12 to 18 percent slopes	CoD	1427	170742	5qnt	oh139	1971	1:15840
Chili and Conotton soils, 18 to 25 percent slopes	CoE	400	170744	5qnw	oh139	1971	1:15840
Conotton gravelly loam, 2 to 12 percent slopes	CtC	247	170747	5qnz	oh139	1971	1:15840
Chili and Conotton soils, 12 to 18 percent slopes, severely eroded	CoD3	138	170743	5qnv	oh139	1971	1:15840
Chili and Conotton soils, 25 to 40 percent slopes	CoF	104	170745	5qnx	oh139	1971	1:15840
Chili and Conotton gravelly loams, 25 to 50 percent slopes, moderately eroded	CvF2	1495	287981	9nnq	oh151	1967	1:15840
Conotton gravelly loam, 12 to 18 percent slopes, moderately eroded	CyD2	1190	287985	9nnv	oh151	1967	1:15840
Conotton gravelly loam, 18 to 25 percent slopes, moderately eroded	CyE2	969	287986	9nnw	oh151	1967	1:15840
Conotton gravelly loam, 6 to 12 percent slopes	CyC	486	287984	9nnt	oh151	1967	1:15840
Conotton gravelly loam, 2 to 6 percent slopes	CyB	335	287983	9nns	oh151	1967	1:15840
Conotton loam, 0 to 2 percent slopes	CwA	217	287982	9nnr	oh151	1967	1:15840
Conotton gravelly loam, 15 to 25 percent slopes	CcD	36	1595459	1qk6f	oh151	1967	1:15840
Conotton-Oshtemo complex, 12 to 18 percent slopes	CjD	24	1595534	1qk8v	oh151	1967	1:15840
Conotton-Oshtemo complex, 12 to 18 percent slopes	CyD	991	825328	wpth	oh153	1969	1:20000
Conotton-Oshtemo complex, 18 to 25 percent slopes	CyE	914	825329	wptj	oh153	1969	1:20000
Conotton-Oshtemo complex, 25 to 50 percent slopes	CyF	710	825330	wptk	oh153	1969	1:20000
Chili and Conotton gravelly loams, 25 to 50 percent slopes, moderately eroded	CtF2	5	2376137	2krkl	oh153	1969	1:20000
Conotton gravelly loam, 12 to 18 percent slopes, moderately eroded	CsD2	3	2376136	2krkk	oh153	1969	1:20000
Conotton gravelly loam, 6 to 12 percent slopes	CsC	2	2376135	2krkj	oh153	1969	1:20000
Conotton gravelly loam, 2 to 6 percent slopes	CsB	1	2376134	2krkh	oh153	1969	1:20000
Conotton gravelly loam, 0 to 3 percent slopes	CoA	800	536294	2xqwg	oh157	1981	1:15840
Conotton gravelly loam, 3 to 8 percent slopes	CoB	330	536295	2xqwl	oh157	1981	1:15840
Conotton gravelly loam, 15 to 25 percent slopes	CoD	250	536296	2xqwq	oh157	1981	1:15840
Conotton gravelly loam, 2 to 6 percent slopes	CvB	69	1589426	1qbxt	oh157	1981	1:15840
Chili and Conotton gravelly loams, 25 to 50 percent slopes, moderately eroded	CxF2	2	1589425	1qbxs	oh157	1981	1:15840
Conotton gravelly loam, 12 to 18 percent slopes, moderately eroded	CvD2	1	1589427	1qbxv	oh157	1981	1:15840
Conotton gravelly loam, 0 to 3 percent slopes	Cnt6A1	270	3175560	2zfvd	oh167	1973	1:15840
Conotton-Chili gravelly loams, 18 to 25 percent slopes	CpE	125	536467	l07d	oh167	1973	1:15840
Conotton gravelly loam, 3 to 8 percent slopes	Cnt6B1	35	3175559	2zfvf	oh167	1973	1:15840
Conotton gravelly loam, 6 to 12 percent slopes	CvC	10	2217029	2df02	oh169	1981	1:15840
Urban land-Conotton complex, 0 to 8 percent slopes	UfB	6322	2900313	l6mk	pa007	1978	1:15840
Conotton gravelly loam, 3 to 8 percent slopes	CoB	1151	2900252	l6kl	pa007	1978	1:15840
Urban land-Conotton complex, 8 to 25 percent slopes	UfD	822	2900314	l6ml	pa007	1978	1:15840
Conotton gravelly loam, 8 to 15 percent slopes	CoC	504	2900253	l6km	pa007	1978	1:15840
Conotton gravelly loam, 15 to 25 percent slopes	CoD	381	2900254	l6kn	pa007	1978	1:15840
Conotton gravelly loam, 0 to 3 percent slopes	CtA	369	539308	l361	pa025	1960	1:20000
Conotton gravelly loam, 3 to 8 percent slopes	CtB	51	539309	l362	pa025	1960	1:20000
Conotton gravelly loam, 15 to 25 percent slopes	CtD	27	539310	l363	pa025	1960	1:20000
Conotton gravelly loam, 8 to 15 percent slopes	CoC	4858	2900405	l6km	pa073	1978	1:15840
Conotton gravelly loam, 15 to 25 percent slopes	CoD	3604	2900406	l6kn	pa073	1978	1:15840
Conotton gravelly loam, 3 to 8 percent slopes	CoB	1852	2900404	l6kl	pa073	1978	1:15840
Conotton gravelly loam, 25 to 50 percent slopes	CoF	1437	2900407	l6kp	pa073	1978	1:15840
Urban land-Conotton complex, 0 to 8 percent slopes	UfB	1087	2900465	l6mk	pa073	1978	1:15840
Urban land-Conotton complex, 8 to 25 percent slopes	UfD	482	2900466	l6ml	pa073	1978	1:15840
Conotton gravelly loam, 3 to 8 percent slopes	CtB	2749	1948774	23dvp	pa095	2007	1:12000
Conotton gravelly loam, 8 to 15 percent slopes	CtC	1251	1948775	23dvq	pa095	2007	1:12000
Conotton gravelly loam, 0 to 3 percent slopes	CtA	905	1948773	23dvn	pa095	2007	1:12000
Conotton gravelly loam, 25 to 65 percent slopes	CtF	336	1948777	23dvs	pa095	2007	1:12000
Conotton gravelly loam, 15 to 25 percent slopes	CtD	316	1948776	23dvr	pa095	2007	1:12000
Urban land-Conotton complex, 0 to 8 percent slopes	UmB	225	1948970	23f20	pa095	2007	1:12000
Conotton gravelly sandy loam, 0 to 3 percent slopes	CoA	262	1384221	2xqwj	wv600	2005	1:24000

Map of Series Extent

Approximate geographic distribution of the CONOTTON 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).