Soil Data Explorer - SUMTER

Official Series Description

Lab Data Summary

Aggregate lab data for the SUMTER soil series. This aggregation is based on all pedons with a current taxon name of SUMTER, 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 SUMTER 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
133A	12N8054	S2012AL101901	Sumter	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.1019333,-86.2004278
135A	S04AL-041-2	04AL041002-pgm	Sumter	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.3361111,-86.3791667
135A	S99AL-065-3	99AL065003-pgm	Sumter	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.5591667,-87.6472222
135A	40A4834	S1958MS025001	SUMTER	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	33.6051445,-88.5378189
135A	40A4836	S1958MS101002	SUMTER	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.2512894,-89.2522812
135A	40A4837	S1958MS101003	SUMTER	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	32.2479553,-89.1833954
n/a	40A4835	S1958MS095006	SUMTER	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 SUMTER 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 SUMTER 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 SUMTER 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 SUMTER 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 SUMTER 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 SUMTER 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).

Geomorphic description summaries for the SUMTER 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 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 SUMTER, 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. AL-2012-04-24-11 | Greene County - June 1971

   Cross section of association 2 showing topography, important soils, and underlying material (Soil Survey of Greene County, Alabama; June 1971).

2. MS-2012-02-06-08 | Prentiss County - October 1997

   Typical pattern of soils and parent material in the Kipling-Sumter general soil map unit (Soil Survey of Prentiss County, Mississippi; October 1997).

3. MS-2012-02-06-10 | Prentiss County - October 1997

   Typical pattern of soils and parent material in the Leeper-Marietta-Catalpa general soil map unit (Soil Survey of Prentiss County, Mississippi; October 1997).

4. TX-2012-03-20-41 | Ellis County - August 1964

   Block diagram showing relation of eight soil associations in Ellis County to the underlying materials and surface relief (Soil Survey of Ellis County, TX; 1964).

5. TX-2012-03-20-46 | Ellis County - August 1964

   Geographical association of soils on flood plains. The Wilson and the Crockett soils are in soil association 7 (Soil Survey of Ellis County, TX; 1964).

Map Units

Map units containing SUMTER 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
Sumter-Hannon complex, 12 to 40 percent slopes	ShF	1564	3272044	2zkvs	al001	1972	1:20000
Sumter silty clay, 5 to 15 percent slopes, eroded	SuD2	430	328478	c0t2	al013	1996	1:20000
Sumter-Maytag complex, 8 to 15 percent slopes, eroded	StE2	2330	328607	c0y7	al023	1998	1:24000
Sumter-Maytag complex, 3 to 8 percent slopes, moderately eroded	StD2	1740	328578	2x59n	al023	1998	1:24000
Sumter-Hannon complex, 12 to 35 percent slopes, eroded	StE2	2910	1413848	1jg70	al041	2005	1:24000
Hannon-Sumter complex, 2 to 8 percent slopes, eroded	HsC2	1240	1413847	1jg6z	al041	2005	1:24000
Sumter silty clay, 1 to 5 percent slopes	55	16858	329094	c1fy	al047	1977	1:20000
Sumter silty clay, 5 to 12 percent slopes	56	6463	329095	c1fz	al047	1977	1:20000
Sumter-Urban land complex, 1 to 8 percent slopes	57	815	329096	c1g0	al047	1977	1:20000
Sumter silty clay, 3 to 5 percent slopes, eroded	SuC2	8246	329714	c22y	al063	2013	1:
Sumter-Watsonia complex, 5 to 17 percent slopes, eroded	SwE2	5752	329717	c231	al063	2013	1:
Sumter-Watsonia complex, 1 to 5 percent slopes, eroded	SwB2	5036	329716	c230	al063	2013	1:
Sumter silty clay, 1 to 3 percent slopes, eroded	SuB2	4314	329713	c22x	al063	2013	1:
Sumter silty clay, 5 to 12 percent slopes, eroded	SuD2	4095	329715	c22z	al063	2013	1:
Sumter silty clay loam, 1 to 3 percent slopes	SmB	18040	329754	2v5ls	al065	2003	1:24000
Sumter silty clay loam, 3 to 8 percent slopes, moderately eroded	SmD2	12095	329755	2wwly	al065	2003	1:24000
Demopolis-Sumter complex, 3 to 8 percent slopes, eroded	DsD2	7166	329757	2v5lt	al065	2003	1:24000
Demopolis-Sumter complex, 8 to 12 percent slopes, eroded	DsE2	4232	329758	c24c	al065	2003	1:24000
Sumter-Watsonia complex, 3 to 8 percent slopes, eroded	SwD2	4122	329761	2v5lv	al065	2003	1:24000
Sumter-Watsonia complex, 1 to 3 percent slopes	SwB	2025	329760	c24f	al065	2003	1:24000
Sumter-Oktibbeha complex, 3 to 8 percent slopes, eroded	SoD2	404	725105	sbjh	al065	2003	1:24000
Sumter-Watsonia complex, 8 to 12 percent slopes, eroded	SwE2	155	329762	c24h	al065	2003	1:24000
Sumter-Hannon complex, 8 to 12 percent slopes, severely eroded	StE3	35845	2514907	2qdgv	al085	2011	1:24000
Sumter-Hannon complex, 3 to 8 percent slopes, severely eroded	StD3	21421	2514906	2qdgt	al085	2011	1:24000
Sumter-Hannon complex, 12 to 35 percent slopes, severely eroded	StF3	16528	2514908	2qdgw	al085	2011	1:24000
Sumter-Hannon complex, 1 to 3 percent slopes	StB	13513	2514909	2qdgx	al085	2011	1:24000
Sumter silty clay loam, 1 to 3 percent slopes	SmB2	11310	2514947	2v5ls	al085	2011	1:24000
Hannon-Sumter complex, 8 to 15 percent slopes, eroded	HsE2	11284	2514936	2qdw9	al085	2011	1:24000
Hannon-Sumter complex, 15 to 35 percent slopes, eroded	HsF2	9053	2514937	2qdwb	al085	2011	1:24000
Sumter-Demopolis complex, 8 to 25 percent slopes, moderately eroded	SpE2	2580	2514649	2wwm6	al085	2011	1:24000
Sumter silty clay loam, 3 to 8 percent slopes, moderately eroded	SmD2	2305	2514657	2wwly	al085	2011	1:24000
Sumter silty clay loam, 35 to 60 percent slopes, severely eroded	SmG3	485	2514945	2qdwd	al085	2011	1:24000
Sumter-Hannon complex, 12 to 25 percent slopes	StE	5612	330495	c2x4	al087	1997	1:24000
Hannon-Sumter complex, 5 to 12 percent slopes	HsE	1562	330466	c2w6	al087	1997	1:24000
Sumter-Watsonia complex, 3 to 8 percent slopes, eroded	SwC2	11640	330602	2v5lv	al091	1997	1:24000
Sumter silty clay loam, 5 to 12 percent slopes, eroded	SuE2	8980	330600	c30j	al091	1997	1:24000
Sumter-Watsonia complex, 1 to 3 percent slopes	SwB	4480	330601	c30k	al091	1997	1:24000
Sumter clay, eroded, nearly level phase	SmB2	20153	330974	c3dl	al101	1958	1:20000
Sumter clay, severely eroded, very gently sloping phase	SmC3	12718	330977	c3dp	al101	1958	1:20000
Sumter-Oktibbeha-Vaiden clays, severely eroded, gently sloping phases	SnD3	5675	330984	c3dx	al101	1958	1:20000
Sumter-Oktibbeha-Vaiden clays, eroded, nearly level	SnB2	5513	330980	c3ds	al101	1958	1:20000
Sumter clay, severely eroded, gently sloping phase	SmD3	5318	330979	c3dr	al101	1958	1:20000
Sumter-Oktibbeha-Vaiden clays, severely eroded, sloping phases	SnE3	3560	330985	c3dy	al101	1958	1:20000
Sumter clay, eroded, very gently sloping phase	SmC2	3403	330976	c3dn	al101	1958	1:20000
Sumter-Oktibbeha-Vaiden clays, severely eroded, very gently sloping phases	SnC3	3108	330982	c3dv	al101	1958	1:20000
Sumter clay, severely eroded, nearly level phase	SmB3	2889	330975	c3dm	al101	1958	1:20000
Sumter clay, eroded, gently sloping phase	SmD2	911	330978	c3dq	al101	1958	1:20000
Sumter-Oktibbeha-Vaiden clays, eroded, gently sloping phases	SnD2	644	330983	c3dw	al101	1958	1:20000
Sumter-Oktibbeha-Vaiden clays, eroded, very gently sloping phases	SnC2	463	330981	c3dt	al101	1958	1:20000
Sumter-Urban land complex, 1 to 3 percent slopes	SkB	111	3116394	2zkvj	al101	1958	1:20000
Sumter silty clay loam, 1 to 3 percent slopes	SmB	7790	331258	2v5ls	al105	1996	1:24000
Sumter-Oktibbeha complex, 3 to 8 percent slopes, eroded	SoD2	7690	331261	c3pv	al105	1996	1:24000
Sumter silty clay loam, 3 to 8 percent slopes, moderately eroded	SnD2	7200	331259	2wwly	al105	1996	1:24000
Demopolis-Sumter complex, 3 to 8 percent slopes, eroded	DsD2	4650	331229	2v5lt	al105	1996	1:24000
Sumter-Oktibbeha complex, 1 to 3 percent slopes, eroded	SoB2	1920	331260	c3pt	al105	1996	1:24000
Sumter silty clay loam, 1 to 5 percent slopes, eroded	SuC2	4330	331280	c3qg	al107	1997	1:24000
Sumter silty clay loam, 5 to 12 percent slopes, eroded	SuE2	2070	331281	c3qh	al107	1997	1:24000
Sumter-Hannon complex, 12 to 25 percent slopes, severely eroded	ShE3	3730	331345	c3sk	al113	1997	1:24000
Hannon-Sumter complex, 5 to 12 percent slopes, eroded	HsE2	870	331338	c3sb	al113	1997	1:24000
Demopolis-Sumter complex, 1 to 3 percent slopes	DsB	13320	331474	c3xq	al119	1986	1:24000
Sumter silty clay loam, 1 to 5 percent slopes, eroded	SuB2	1335	331492	c3y9	al119	1986	1:24000
Sumter silty clay loam, 5 to 8 percent slopes, moderately eroded	SuC2	205	331493	2x54h	al119	1986	1:24000
Sumter very cobbly silt loam, 1 to 5 percent slopes	SvB	125	331494	c3yc	al119	1986	1:24000
Sumter-Maytag complex, 8 to 15 percent slopes, eroded	StD2	965	2642134	2rrwq	al129	2013	1:24000
Sumter-Maytag complex, 3 to 8 percent slopes, moderately eroded	StC2	562	2642133	2x59n	al129	2013	1:24000
Sumter-Demopolis complex, 8 to 25 percent slopes, moderately eroded	SpE2	12320	331676	2wwm6	al131	1997	1:24000
Sumter-Gullied land complex, 8 to 25 percent slopes, severely eroded	SuE3	380	331677	c448	al131	1997	1:24000
Sumter silty clay, 3 to 12 percent slopes, eroded	80	4013	3179418	lypj	ar019	1983	1:20000
Sumter silty clay, 12 to 20 percent slopes, eroded	81	1112	3179419	lypk	ar019	1983	1:20000
Sumter clay, 3 to 12 percent slopes	48	8912	565675	lzml	ar057	1976	1:20000
Sumter-Oktibbeha association, rolling	SoD	6390	565722	lzp3	ar061	1970	1:24000
Sumter clay, 3 to 12 percent slopes	SmD2	5482	565721	lzp2	ar061	1970	1:24000
Sumter silty clay, 8 to 15 percent slopes, eroded	38D	5651	1707541	1v9tz	ar133	1996	1:24000
Sumter silty clay, 3 to 8 percent slopes, eroded	38C	1792	1707540	1v9ty	ar133	1996	1:24000
Sumter silty clay loam, 5 to 12 percent slopes, eroded	76	3896	564954	lywb	ar670	1981	1:20000
Sumter silty clay loam, 2 to 5 percent slopes	SmB	50	325801	by0q	ga634	1980	1:20000
Sumter clay loam, 2 to 8 percent slopes, eroded	SHC2	645	325932	by4y	ga640	1965	1:15840
Sumter-Oktibbeha complex, 12 to 17 percent slopes, eroded	SoE2	1529	331756	c46t	ms003	1967	1:20000
Sumter-Gullied land complex, 8 to 25 percent slopes	SgE	710	331755	c46s	ms003	1967	1:20000
Sumter clay, 5 to 12 percent slopes, severely eroded	SuD3	2474	332062	c4jp	ms023	1963	1:15840
Sumter clay, 2 to 5 percent slopes, eroded	SuB2	1374	332059	c4jl	ms023	1963	1:15840
Sumter clay, 5 to 8 percent slopes, eroded	SuC2	643	332061	c4jn	ms023	1963	1:15840
Sumter clay, 2 to 5 percent slopes, severely eroded	SuB3	437	332060	c4jm	ms023	1963	1:15840
Sumter silty clay, 5 to 12 percent slopes, moderately eroded	SuC2	2448	332108	2x54k	ms025	1974	1:20000
Sumter silty clay, 2 to 5 percent slopes, moderately eroded	SuB2	1952	332107	2x54j	ms025	1974	1:20000
Sumter silty clay, 8 to 17 percent slopes, eroded	SuE2	365	332488	c4zf	ms057	1975	1:20000
Sumter clay, 2 to 8 percent slopes, eroded	SmC2	5677	332657	c54w	ms061	1974	1:20000
Sumter clay, 8 to 12 percent slopes, eroded	SmD2	1394	332658	c54x	ms061	1974	1:20000
Sumter-Demopolis complex, 5 to 17 percent slopes, severely eroded	SuE3	3786	332798	c59f	ms069	1991	1:20000
Oktibbeha and Sumter soils, 8 to 17 percent slopes, severely eroded	OkE3	11005	333028	c5jv	ms081	1968	1:20000
Sumter silty clay, 5 to 12 percent slopes	SuD2	854	333043	c5kb	ms081	1968	1:20000
Sumter silty clay loam, 5 to 12 percent slopes, eroded	SuC2	10765	333104	c5m9	ms087	1977	1:20000
Sumter silty clay loam, 2 to 5 percent slopes, eroded	SuB2	4474	333103	c5m8	ms087	1977	1:20000
Sumter-Demopolis-Chalk outcrop complex, 5 to 20 percent slopes, severely eroded	SvD3	1595	333105	c5mb	ms087	1977	1:20000
Vaiden and Sumter soils 8 to 17 percent slopes, severely eroded (kipling and sumter)	VsE3	4366	333231	c5rd	ms095	1963	1:15840
Sumter silty clay, 5 to 12 percent slopes, severely eroded	SuD3	3860	333215	c5qw	ms095	1963	1:15840
Sumter silty clay, 2 to 5 percent slopes, severely eroded	SuB3	388	333214	c5qv	ms095	1963	1:15840
Binnsville clay, eroded gently sloping marly phase (sumter) (5 to 8 percent slopes)	BbC3	2103	333300	c5tm	ms101	1957	1:20000
Binnsville clay, eroded very gently sloping marly phase (sumter) (2 to 5 percent slopes)	BbB2	863	333299	c5tl	ms101	1957	1:20000
Sumter clay, eroded gently sloping phase (5 to 8 percent slopes)	SkC2	351	333393	c5xm	ms101	1957	1:20000
Oktibbeha-Sumter complex, 8 to 15 percent slopes, eroded	OuE2	8320	333436	c5z0	ms103	1983	1:20000
Sumter silty clay, 5 to 12 percent slopes, moderately eroded	SuD2	7403	333456	2x54k	ms103	1983	1:20000
Sumter silty clay, 2 to 5 percent slopes, moderately eroded	SuB2	6208	333455	2x54j	ms103	1983	1:20000
Sumter-Demopolis-Rock outcrop, chalk complex, 5 to 20 percent slopes, severely eroded	SvE3	2081	333458	c5zq	ms103	1983	1:20000
Oktibbeha-Sumter complex, 15 to 25 percent slopes, eroded	OuF2	1872	333437	c5z1	ms103	1983	1:20000
Sumter silty clay, 12 to 17 percent slopes, eroded	SuE2	626	333457	c5zp	ms103	1983	1:20000
Kipling and Sumter soils, 17 to 40 percent slopes, severely eroded	KsF3	4929	333488	c60p	ms105	1968	1:20000
Gullied land-Sumter complex, 5 to 20 percent slopes	GsE	3470	333483	c60j	ms105	1968	1:20000
Sumter and Binnsville soils, 5 to 8 percent slopes, eroded	SvC2	2979	333520	c61q	ms105	1968	1:20000
Sumter silty clay loam, 5 to 8 percent slopes, moderately eroded	SuC2	2724	333517	2x54h	ms105	1968	1:20000
Sumter and Binnsville soils, 2 to 5 percent slopes, eroded	SvB2	2398	333519	c61p	ms105	1968	1:20000
Sumter silty clay loam, 8 to 12 percent slopes, eroded	SuD2	1026	333518	c61n	ms105	1968	1:20000
Sumter silty clay, 8 to 12 percent slopes, severely eroded	SuD3	3986	333836	c6cx	ms117	1995	1:24000
Sumter silty clay, 12 to 40 percent slopes, severely eroded	SuF3	3374	333837	c6cy	ms117	1995	1:24000
Sumter-Maytag complex, 3 to 8 percent slopes, moderately eroded	StC2	1482	2403466	2x59n	ms153	2008	1:24000
Sumter silty clay loam, 3 to 12 percent slopes	SuE	562	571188	m5cf	ok089	1970	1:24000
Sumter silty clay, 12 to 35 percent slopes, eroded	SuF2	100	327648	bzy9	tn071	1961	1:15840
Sumter silty clay 5 to 12 percent slopes, eroded	SuD2	47	327647	bzy8	tn071	1961	1:15840
Oktibbeha and Sumter soils, 8 to 20 percent slopes	OsD	11061	327969	c08n	tn109	1994	1:20000

Map of Series Extent

Approximate geographic distribution of the SUMTER 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).