Soil Data Explorer - CUMBERLAND

Official Series Description

Lab Data Summary

Aggregate lab data for the CUMBERLAND soil series. This aggregation is based on all pedons with a current taxon name of CUMBERLAND, 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 CUMBERLAND 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
122	40A4945	1955TN031027	Cumberland	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.3594437,-85.9427795
122	40A4946	1955TN031028	Cumberland	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.4066658,-85.9355545
122	96KY-227-008	96KY-227-008	Cumberland	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.9961891,-86.4635925
122	97KY-227-003	97KY-227-003	Cumberland	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.952301,-86.3883133
128	40A4943	S1953TN009013	Cumberland	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.7964859,-84.165741
128	40A4944	S1953TN009018	Cumberland	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.7747231,-83.8719406
n/a	40A4356	1965TN149001	Cumberland	6	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 CUMBERLAND 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 CUMBERLAND 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 CUMBERLAND 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 CUMBERLAND 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.

Competing Series

Soil series competing with CUMBERLAND 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 CUMBERLAND 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the CUMBERLAND 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 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 CUMBERLAND, 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. KY-2012-02-01-47 | Pulaski County - December 1974

   Pattern of soils and underlying material in association 2 (Soil Survey of Pulaski County, Kentucky; December 1974).

2. KY-2012-02-01-48 | Pulaski County - December 1974

   Pattern of soils and underlying material in association 3 (Soil Survey of Pulaski County, Kentucky; December 1974).

3. TN-2012-03-19-17 | Loudon County - June 1961

   Diagram showing distribution and pattern of soils in area 5 (Soil Survey of Loudon County, TN; 1961).

4. TN-2012-03-19-32 | Warren County - September 1967

   Major and minor soils and underlying parent materials in the Waynesboro-Cumberland association (Soil Survey of Warren County, TN; 1967).

Map Units

Map units containing CUMBERLAND 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
Decatur and Cumberland clay loams, 2 to 6 percent slopes, severely eroded	DcB3	7168	523307	kkjw	al015	1959	1:20000
Decatur and Cumberland clay loams, 6 to 10 percent slopes, severely eroded	DcC3	5052	523308	kkjx	al015	1959	1:20000
Decatur and Cumberland loams, 2 to 6 percent slopes, eroded	DdB2	3342	523311	kkk0	al015	1959	1:20000
Cumberland gravelly loam, 2 to 6 percent slopes eroded	CoB2	2490	523303	kkjr	al015	1959	1:20000
Decatur and Cumberland clay loams, 10 to 25 percent slopes, severely eroded	DcD3	1438	523309	kkjy	al015	1959	1:20000
Cumberland gravelly clay loam, 6 to 10 percent slopes, severely eroded	CrC3	1435	523305	kkjt	al015	1959	1:20000
Cumberland gravelly clay loam, 2 to 6 percent slopes, severely eroded	CrB3	1143	523304	kkjs	al015	1959	1:20000
Cumberland gravelly clay loam, 10 to 25 percent slopes, severely eroded	CrD3	1010	523306	kkjv	al015	1959	1:20000
Decatur and Cumberland loams 6 to 10 percent slopes, eroded	DdC2	643	523312	kkk1	al015	1959	1:20000
Decatur and Cumberland loams, 0 to 2 percent slopes	DdA	382	523310	kkjz	al015	1959	1:20000
Decatur and Cumberland loams, 10 to 25 percent slopes, eroded	DdD2	324	523313	kkk2	al015	1959	1:20000
Cumberland silty clay loam, eroded, undulating phase	Cme	1984	522834	kk1m	al071	1943	1:24000
Cumberland silty clay loam, eroded, rolling phase	Cmn	1769	522836	kk1p	al071	1943	1:24000
Cumberland silty clay loam, severely eroded, rolling phase	Cmd	1582	522833	kk1l	al071	1943	1:24000
Cumberland silt loam, undulating phase	Csu	747	522842	kk1w	al071	1943	1:24000
Cumberland silty clay loam, severely eroded, hilly phase	Cmr	685	522837	kk1q	al071	1943	1:24000
Cumberland silty clay loam, eroded, hilly phase	Cmh	208	522835	kk1n	al071	1943	1:24000
Cumberland loam, undulating phase	Cuu	202	522846	kk20	al071	1943	1:24000
Cumberland silt loam, rolling phase	Cso	145	522841	kk1v	al071	1943	1:24000
Cumberland loam, 2 to 6 percent slopes, eroded	Cb	7462	330085	2yn7y	al079	1950	1:20000
Cumberland loam, 2 to 6 percent slopes, eroded	Cv	7000	330102	2ykcy	al079	1950	1:20000
Cumberland loam, 6 to 12 percent slopes, eroded	Ca	1287	330084	2yn7z	al079	1950	1:20000
Cumberland loam, 6 to 12 percent slopes, eroded	Cu	1200	330101	2ykcz	al079	1950	1:20000
Cumberland loam, 2 to 6 percent slopes	Cc	400	330086	2yn7x	al079	1950	1:20000
Cumberland loam, 2 to 6 percent slopes	Cw	279	330103	2ykcx	al079	1950	1:20000
Cumberland silty clay loam eroded undulating phase	Cme	4837	522741	kjym	al083	1953	1:20000
Cumberland silty clay loam severely eroded rolling phase	Cmd	2549	522740	kjyl	al083	1953	1:20000
Cumberland silty clay loam eroded rolling phase	Cmn	1112	522742	kjyn	al083	1953	1:20000
Cumberland silt loam undulating phase	Csu	765	522743	kjyp	al083	1953	1:20000
Cumberland fine sandy loam undulating phase	Cfu	744	522734	kjyd	al083	1953	1:20000
Cumberland silt loam level phase	Csv	574	522744	kjyq	al083	1953	1:20000
Cumberland clay loam eroded undulating phase	Cde	435	522733	kjyc	al083	1953	1:20000
Cumberland gravelly silty clay loam eroded rolling phase	Cgn	342	522735	kjyf	al083	1953	1:20000
Cumberland loam, eroded, undulating	Cv	5112	523099	kkb5	al089	1958	1:24000
Cumberland loam, eroded, rolling	Cw	887	523100	kkb6	al089	1958	1:24000
Cumberland loam, undulating	Cu	302	523098	kkb4	al089	1958	1:24000
Cumberland and Hermitage silty clay loams, severely eroded, sloping	CnC3	2220	330684	c337	al095	1956	1:20000
Cumberland and Hermitage silty clay loams, severely eroded, gently sloping	CnB3	2220	330683	c336	al095	1956	1:20000
Cumberland and Hermitage silt loams, eroded, gently sloping	CmB2	777	330681	c334	al095	1956	1:20000
Cumberland and Hermitage silty clay loams, severely eroded, strongly sloping	CnD3	389	330685	c338	al095	1956	1:20000
Cumberland and Hermitage silt loams, eroded, sloping	CmC2	222	330682	c335	al095	1956	1:20000
Cumberland and Hermitage silty clay loams, severely eroded, moderately steep	CnE3	139	330686	c339	al095	1956	1:20000
Cumberland silty clay loam, eroded, undulating	Cy	3717	331055	c3h6	al103	1949	1:15840
Cumberland silt loam, undulating	Cx	799	331054	c3h5	al103	1949	1:15840
Cumberland silty clay loam, severely eroded, rolling	Cz	687	331056	c3h7	al103	1949	1:15840
Cumberland silt loam, level	Cw	308	331053	c3h4	al103	1949	1:15840
Cumberland silt loam, 2 to 6 percent slopes	CvB	1318	548700	ldz0	ky141	1972	1:20000
Cumberland silt loam, 6 to 12 percent slopes	CvC	1309	548701	ldz1	ky141	1972	1:20000
Cumberland silty clay loam, 6 to 12 percent slopes, severely eroded	CwC3	329	548702	ldz2	ky141	1972	1:20000
Cumberland silt loam, 6 to 12 percent slopes	CuC	3078	552388	ljsz	ky199	1969	1:12000
Cumberland silt loam, 2 to 6 percent slopes	CuB	1143	552387	ljsy	ky199	1969	1:12000
Cumberland silty clay loam, eroded rolling phase	Cp	671	526871	kp7v	tn011	1951	1:20000
Cumberland silty clay loam, eroded undulating phase	Cr	439	526872	kp7w	tn011	1951	1:20000
Cumberland silty clay loam, severely eroded hilly phase	Cs	97	526873	kp7x	tn011	1951	1:20000
Cumberland silty clay loam, severely eroded rolling phase	Ct	92	526874	kp7y	tn011	1951	1:20000
Cumberland silt loam, eroded, gently sloping phase	Cr	2562	524884	km5r	tn031	1956	1:20000
Cumberland silty clay loam severely eroded sloping phase	Cu	970	524887	km5v	tn031	1956	1:20000
Cumberland silty clay loam, severely eroded, gently sloping phase	Ct	484	524886	km5t	tn031	1956	1:20000
Cumberland silt loam, gently sloping phase	Cp	275	524883	km5q	tn031	1956	1:20000
Cumberland silt loam, eroded, sloping phase	Cs	264	524885	km5s	tn031	1956	1:20000
Cumberland and Etowah silty clay loams, eroded undulating phase	Cp	17033	527168	kpkf	tn051	1950	1:20000
Cumberland and Etowah silty clay loams, eroded rolling phase	Cr	4013	527169	kpkg	tn051	1950	1:20000
Cumberland and Etowah loams, eroded, undulating phase	Cm	3306	527165	kpkb	tn051	1950	1:20000
Cumberland silty clay loam, severely eroded rolling phase	Cf	2138	527161	kpk6	tn051	1950	1:20000
Cumberland and Etowah loams, eroded rolling phase	Cn	1731	527166	kpkc	tn051	1950	1:20000
Cumberland and Etowah silt loams, undulating phase	Co	462	527167	kpkd	tn051	1950	1:20000
Cumberland clay loam, severely eroded rolling phase	Cd	349	527159	kpk4	tn051	1950	1:20000
Cumberland and Etowah loams, undulating phase	Ck	281	527164	kpk9	tn051	1950	1:20000
Cumberland silty clay loam, severely eroded hilly phase	Ch	210	527163	kpk8	tn051	1950	1:20000
Cumberland silt loam, rolling phase	Ce	150	527160	kpk5	tn051	1950	1:20000
Cumberland silty clay loam, eroded hilly phase	Cg	133	527162	kpk7	tn051	1950	1:20000
Cumberland silty clay loam, eroded sloping phase	CmC2	2503	525909	kn7t	tn105	1958	1:15840
Cumberland silty clay loam, severely eroded moderately steep phase	CmD3	861	525912	kn7x	tn105	1958	1:15840
Cumberland silty clay loam, eroded moderately steep phase	CmD2	811	525911	kn7w	tn105	1958	1:15840
Cumberland silty clay loam, severely eroded sloping phase	CmC3	661	525910	kn7v	tn105	1958	1:15840
Cumberland silty clay loam, eroded gently sloping phase	CmB2	376	525908	kn7s	tn105	1958	1:15840
Cumberland and Decatur silty clay loams, severely eroded steep phases	CrE3	362	525916	kn81	tn105	1958	1:15840
Cumberland silty clay loam 5 to 12 percent slopes, eroded	CsC2	3423	527978	kqdk	tn125	1972	1:15840
Cumberland soils, cherty variant, 10 to 25 percent slopes, eroded (Baxter)	CuD2	1945	527979	kqdl	tn125	1972	1:15840
Cumberland silty clay loam, 5 to 12 percent slopes, severely eroded	CuC3	679	528163	kqlj	tn147	1965	1:15840
Cumberland silt loam, 2 to 5 percent slopes	CuB	15862	528218	kqn9	tn149	1974	1:15840
Cumberland silt loam, 0 to 2 percent slopes	CuA	4228	528217	kqn8	tn149	1974	1:15840
Cumberland silty clay loam, 2 to 5 percent slopes, severely eroded	CvB3	1447	528220	kqnc	tn149	1974	1:15840
Cumberland silt loam, 5 to 12 percent slopes, eroded	CuC2	1249	528219	kqnb	tn149	1974	1:15840
Cumberland silty clay loam, 5 to 12 percent slopes, severely eroded	CvC3	507	528221	kqnd	tn149	1974	1:15840
Cumberland silt loam, 2 to 5 percent slopes	CsB	4180	529875	kscr	tn177	1965	1:15840
Cumberland silt loam, 5 to 12 percent slopes, eroded	CsC2	2683	529876	kscs	tn177	1965	1:15840
Cumberland silty clay loam, 5 to 12 percent slopes, severely eroded	CuC3	1112	529877	ksct	tn177	1965	1:15840
Cumberland silt loam, 0 to 2 percent slopes	CsA	680	529874	kscq	tn177	1965	1:15840
Cumberland silty clay loam, 12 to 20 percent slopes, severely eroded	CuD3	602	529878	kscv	tn177	1965	1:15840
Cumberland silty clay loam, 5 to 12 percent slopes, eroded	CuC2	1096	1689642	1tq6l	tn179	1955	1:15840
Cumberland silt loam, 2 to 5 percent slopes	CuB	1057	1689643	1tq6m	tn179	1955	1:15840
Cumberland silty clay loam, 12 to 25 percent slopes, eroded	CuD2	529	1689641	1tq6k	tn179	1955	1:15840
Cumberland silty clay loam, eroded sloping phase	Cm	1922	1899461	21rjy	tn609	1955	1:20000
Cumberland silty clay, severely eroded moderately steep phase	Ck	936	1899459	21rjw	tn609	1955	1:20000
Cumberland silty clay loam, eroded moderately steep phase	Cn	656	1899462	21rjz	tn609	1955	1:20000
Cumberland silty clay loam, eroded gently sloping phase	Cl	402	1899460	21rjx	tn609	1955	1:20000
Cumberland silty clay, severely eroded sloping phase	Ch	348	1899458	21rjv	tn609	1955	1:20000
Cumberland silt loam, 2 to 5 percent slopes	CsB	549	2427426	2mgy2	tn610	1960	1:15840
Cumberland silt loam, 5 to 12 percent slopes, eroded	CsC2	251	2427427	2mgy3	tn610	1960	1:15840
Cumberland silty clay loam, 5 to 12 percent slopes, severely eroded	CuC3	181	2427428	2mgy4	tn610	1960	1:15840

Map of Series Extent

Approximate geographic distribution of the CUMBERLAND 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).