Soil Data Explorer - CARDINGTON

Official Series Description

Lab Data Summary

Aggregate lab data for the CARDINGTON soil series. This aggregation is based on all pedons with a current taxon name of CARDINGTON, 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 CARDINGTON were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
111B	SA-013	1961-OH147-013	Cardington	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.0175056,-82.8789368
111B	SA-015	1961-OH147-015	Cardington	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.0374451,-83.0181427
111B	SA-016	1961-OH147-016	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.9942894,-82.978981
111B	SA-023	1962-OH147-023	Cardington	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.01091,-83.1185913
111E	DL-027	1959-OH041-027	Cardington	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.3055,-82.9499444
n/a	HU-E04	1942-OH077-E04	Cardington	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	FA-s06	1949-OH045-S06	Cardington	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	FA-s01	1954-OH045-S01	Cardington	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	SA-s02	1954-OH147-S02	Cardington	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	AS-S01	1955-OH005-S01	Cardington	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	PY-s01	1955-OH129-S01	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	RO-037	1958-OH141-037	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	RO-038	1958-OH141-038	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	RO-061	1958-OH141-061	Cardington	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	AS-S03	1959-OH005-S03	Cardington	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	DL-028	1959-OH041-028	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	DL-029	1959-OH041-029	Cardington	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	DL-030	1959-OH041-030	Cardington	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CR-002	1961-OH033-002	Cardington	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CR-003	1961-OH033-003	Cardington	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CR-005	1961-OH033-005	Cardington	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	RC-s04	1961-OH139-S04	Cardington	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	DL-036	1962-OH041-036	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	PY-004	1962-OH129-004	Cardington	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	PY-005	1962-OH129-005	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MH-046	1964-OH099-046	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	RC-009	1967-OH139-009	Cardington	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MD-019	1970-OH103-019	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	PY-019	1970-OH129-019	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CR-018	1971-OH033-018	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	AS-024	1972-OH005-024	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CR-019	1972-OH033-019	Cardington	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	FR-048	1974-OH049-048	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	FR-054	1974-OH049-054	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	WN-047	1974-OH169-047	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MW-003	YYYY-OH117-003	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MW-006	YYYY-OH117-006	Cardington	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MW-008	YYYY-OH117-008	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MW-009	YYYY-OH117-009	Cardington	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MW-012	YYYY-OH117-012	Cardington	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MW-013	YYYY-OH117-013	Cardington	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 CARDINGTON 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 CARDINGTON 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 CARDINGTON 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 CARDINGTON 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 mountains figure.

Competing Series

Soil series competing with CARDINGTON 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 CARDINGTON 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 CARDINGTON 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.

Soil series sharing subgroup-level classification with CARDINGTON, 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-2010-09-29-16 | Erie County - 2006

   Typical pattern of soils and parent material in the Pewamo-Bennington association (Soil Survey of Erie County, Ohio; 2006).

2. OH-2010-09-29-18 | Fairfield County - 2005

   Typical pattern of soils and parent material in the Bennington-Cardington-Pewamo association (Soil Survey of Fairfield County, Ohio; 2005).

3. OH-2012-02-16-28 | Delaware County - July 1969

   Major soils in the Bennington-Pewamo-Cardington soil association and their underlying material (Soil Survey of Delaware County, Ohio; July 1969).

4. OH-2012-02-16-32 | Huron County - June 1994

   Typical pattern of soils and parent material in the Bennington-Cardington-Condit association (Soil Survey of Huron County, Ohio; June 1994).

Map Units

Map units containing CARDINGTON 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
Cardington silty clay loam, 6 to 12 percent slopes, severely eroded	CeC3	277	288143	9nty	oh005	1976	1:15840
Cardington silt loam, 2 to 6 percent slopes	Crd1B1	2	2996488	2wvgd	oh005	1976	1:15840
Cardington silt loam, 2 to 6 percent slopes, eroded	Crd1B2	10724	2996540	2wvgg	oh033	1975	1:15840
Cardington silt loam, 2 to 6 percent slopes	Crd1B1	9264	2996476	2wvgd	oh033	1975	1:15840
Cardington silt loam, 6 to 12 percent slopes, eroded	Crd1C2	6408	2996690	2wp1z	oh033	1975	1:15840
Cardington silt loam, 12 to 18 percent slopes, moderately eroded	CdD2	736	168549	5nd2	oh033	1975	1:15840
Cardington-Urban land complex, rolling	CeC	486	168550	5nd3	oh033	1975	1:15840
Cardington silt loam, 6 to 12 percent slopes	Crd1C1	2	1019360	2wvgj	oh033	1975	1:15840
Cardington silt loam, 2 to 6 percent slopes	Crd1B1	14599	172042	2wvgd	oh041	1997	1:12000
Cardington silt loam, 6 to 12 percent slopes, eroded	Crd1C2	3879	172043	2wp1z	oh041	1997	1:12000
Cardington silt loam, 2 to 6 percent slopes	Crd1B1	2331	172117	2wvgd	oh043	1998	1:12000
Cardington silty clay loam, 6 to 12 percent slopes, eroded	CbC2	818	172118	5s36	oh043	1998	1:12000
Cardington silt loam, 0 to 2 percent slopes	CaA	67	172116	5s34	oh043	1998	1:12000
Cardington silt loam, 2 to 6 percent slopes	Crd1B1	12619	2996478	2wvgd	oh045	1998	1:12000
Cardington silt loam, 2 to 6 percent slopes, eroded	Crd1B2	5299	2996542	2wvgg	oh045	1998	1:12000
Cardington silt loam, 6 to 12 percent slopes, eroded	Crd1C2	2123	2996694	2wp1z	oh045	1998	1:12000
Urban land-Cardington complex, 2 to 12 percent slopes	UtC	696	172321	5s9r	oh045	1998	1:12000
Cardington silt loam, 12 to 20 percent slopes, eroded	CaD2	321	172230	5s6t	oh045	1998	1:12000
Cardington silt loam, 2 to 6 percent slopes	Crd1B1	5957	2996486	2wvgd	oh049	1977	1:15840
Cardington-Urban land complex, 2 to 6 percent slopes	CbB	5027	167880	5mph	oh049	1977	1:15840
Cardington silt loam, 6 to 12 percent slopes, eroded	Crd1C2	1840	2996696	2wp1z	oh049	1977	1:15840
Cardington-Urban land complex, 6 to 12 percent slopes	CbC	1090	167881	5mpj	oh049	1977	1:15840
Cardington silt loam, 2 to 6 percent slopes, eroded	Crd1B2	510	2996544	2wvgg	oh049	1977	1:15840
Cardington silt loam, 2 to 6 percent slopes	Crd1B1	1024	1398061	2wvgd	oh073	1986	1:15840
Cardington silt loam, 6 to 12 percent slopes, eroded	Crd1C2	950	1398062	2wp1z	oh073	1986	1:15840
Cardington silt loam, 2 to 6 percent slopes	Crd1B1	57355	2996484	2wvgd	oh077	1988	1:15840
Cardington silt loam, 6 to 12 percent slopes, eroded	Crd1C2	5303	2996699	2wp1z	oh077	1988	1:15840
Cardington silt loam, 6 to 12 percent slopes	Crd1C1	19	2996560	2wvgj	oh077	1988	1:15840
Cardington silt loam, 2 to 6 percent slopes, eroded	Crd1B2	2	2996546	2wvgg	oh077	1988	1:15840
Cardington silty clay loam, 6 to 12 percent slopes, eroded	CcC2	2	1605968	1qx4f	oh077	1988	1:15840
Cardington silt loam, 2 to 6 percent slopes	Crd1B1	3219	2996482	2wvgd	oh089	1986	1:15840
Cardington silt loam, 6 to 12 percent slopes, eroded	Crd1C2	1203	2996702	2wp1z	oh089	1986	1:15840
Cardington silt loam, 2 to 6 percent slopes	Crd1B1	86	1605799	2wvgd	oh093	1972	1:15840
Cardington silt loam, 6 to 12 percent slopes, eroded	Crd1C2	5	2996704	2wp1z	oh093	1972	1:15840
Cardington silt loam, 2 to 6 percent slopes	CgB	1042	816732	wdw6	oh099	1966	1:15840
Cardington silt loam, 6 to 12 percent slopes, moderately eroded	CgC2	179	816733	wdw7	oh099	1966	1:15840
Cardington silt loam, 2 to 6 percent slopes	Crd1B1	1779	171184	2wvgd	oh101	1984	1:15840
Cardington silt loam, 6 to 12 percent slopes, eroded	Crd1C2	258	171185	2wp1z	oh101	1984	1:15840
Cardington silt loam, 2 to 6 percent slopes, eroded	Crd1B2	2	1400449	2wvgg	oh101	1984	1:15840
Cardington silt loam, 12 to 25 percent slopes, moderately eroded	CgE2	1220	288323	9p0r	oh103	1974	1:15840
Cardington fine sandy loam, 2 to 6 percent slopes	CfB	270	288320	9p0n	oh103	1974	1:15840
Cardington silt loam, 2 to 6 percent slopes	Crd1B1	16880	2996465	2wvgd	oh117	1986	1:15840
Cardington silt loam, 6 to 12 percent slopes, eroded	Crd1C2	2810	2996708	2wp1z	oh117	1986	1:15840
Cardington silt loam, 6 to 12 percent slopes	Crd1C1	803	2996563	2wvgj	oh117	1986	1:15840
Cardington silt loam, 2 to 6 percent slopes	Crd1B1	4676	2996464	2wvgd	oh129	1977	1:15840
Cardington silt loam, 6 to 12 percent slopes, eroded	Crd1C2	1175	171239	2wp1z	oh129	1977	1:15840
Cardington silt loam, 2 to 6 percent slopes, eroded	Crd1B2	22	1403069	2wvgg	oh129	1977	1:15840
Cardington silt loam, 2 to 6 percent slopes	Crd1B1	4637	2996480	2wvgd	oh139	1971	1:15840
Cardington silt loam, 6 to 12 percent slopes, eroded	Crd1C2	1169	2996711	2wp1z	oh139	1971	1:15840
Cardington silt loam, 2 to 6 percent slopes, eroded	Crd1B2	911	2996552	2wvgg	oh139	1971	1:15840
Cardington silt loam, 6 to 12 percent slopes	Crd1C1	909	2996565	2wvgj	oh139	1971	1:15840
Cardington silty clay loam, 6 to 12 percent slopes, severely eroded	ChC3	299	170738	5qnp	oh139	1971	1:15840
Cardington silt loam, 2 to 6 percent slopes, eroded	Crd1B2	4	1592181	2wvgg	oh147	1978	1:15840
Cardington silt loam, 6 to 12 percent slopes, eroded	Crd1C2	1	1592182	2wp1z	oh147	1978	1:15840
Cardington silt loam, 2 to 6 percent slopes	CgB	3394	287173	9mtn	oh169	1981	1:15840
Cardington silt loam, 6 to 12 percent slopes	CgC	254	287175	9mtq	oh169	1981	1:15840
Cardington silt loam, 6 to 12 percent slopes, eroded	CgC2	250	287176	9mtr	oh169	1981	1:15840
Cardington silt loam, 12 to 25 percent slopes, moderately eroded	CgE2	3	2216979	2ddyg	oh169	1981	1:15840
Cardington silt loam, 6 to 12 percent slopes, eroded	Crd1C2	1746	169600	2wp1z	oh175	1980	1:15840
Cardington silt loam, 2 to 6 percent slopes, eroded	Crd1B2	1473	169599	2wvgg	oh175	1980	1:15840
Cardington silt loam, 12 to 18 percent slopes, eroded	CdD2	282	169601	5ph0	oh175	1980	1:15840
Cardington silt loam, 2 to 6 percent slopes	Crd1B1	3	1542621	2wvgd	oh175	1980	1:15840

Map of Series Extent

Approximate geographic distribution of the CARDINGTON 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).