Soil Data Explorer - SEQUATCHIE

Official Series Description

Lab Data Summary

Aggregate lab data for the SEQUATCHIE soil series. This aggregation is based on all pedons with a current taxon name of SEQUATCHIE, 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 SEQUATCHIE 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
120A	40A4899	S1954KY101010	Sequatchie	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.8658333,-87.6938858
122	40A5018	1959TN141033	Sequatchie	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.0888901,-85.5922241
123	92P0169	1991TN103004	SEQUATCHIE	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.1238899,-86.7147217
n/a	40A5017	1959TN141030	Sequatchie	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	40A4900	S1954KY101011	Sequatchie	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	40A4901	S1957KY111011	Sequatchie	5	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 SEQUATCHIE 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 SEQUATCHIE 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 SEQUATCHIE 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 SEQUATCHIE 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 SEQUATCHIE 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 SEQUATCHIE 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 SEQUATCHIE 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 SEQUATCHIE, 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-2012-04-24-07 | Fayette County - November 1965

   Block diagram showing typical topography and the major soils in the Montevallo-Enders-Townley association (Soil Survey of Fayette County, Alabama; November 1965).

2. KY-2012-01-26-02 | Adair County - April 1964

   Diagram of the Baxter-Christian-Bewleyville association (Soil Survey of Adair County (Soil Survey of Adair County, Kentucky; April 1964).

3. KY-2012-01-26-05 | Adair County - April 1964

   Diagram of the Staser-Taft-Landisburg association on flood plains, terraces, and foot slopes (Soil Survey of Adair County (Soil Survey of Adair County, Kentucky; April 1964).

4. KY-2012-01-27-58 | Elliott County - 1965

   Diagram of Muskingum-Montevallo-Ramsey association, showing relationship of soil series to topography and parent material (Soil Survey of Elliott County, Kentucky; 1965).

5. TN-2012-03-19-02 | Grundy County - 2001

   Typical pattern of soils and the underlying material in the Waynesboro-Etowah general soil map unit (Soil Survey of Grundy County, TN; 2001).

6. 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).

7. 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 SEQUATCHIE 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
Sequatchie fine sandy loam, 0 to 2 percent slopes	ScA	1512	523384	kkmc	al015	1959	1:20000
Sequatchie fine sandy loam, 2 to 6 percent slopes, eroded	ScB2	968	523386	kkmf	al015	1959	1:20000
Sequatchie gravelly fine sandy loam, 2 to 6 percent slopes, eroded	SeB2	670	523387	kkmg	al015	1959	1:20000
Sequatchie fine sandy loam, 2 to 6 percent slopes	ScB	633	523385	kkmd	al015	1959	1:20000
Sequatchie silt loam, 0 to 2 percent slopes	SeA	614	328947	c196	al043	1960	1:20000
Sequatchie silt loam, 2 to 6 percent slopes	SeB	502	328948	c197	al043	1960	1:20000
Sequatchie fine sandy loam, undulating	Sb	500	329211	c1kq	al049	1953	1:20000
Sequatchie fine sandy loam, eroded, undulating	Sa	500	329210	c1kp	al049	1953	1:20000
Sequatchie loam	Sc	1186	329511	c1wd	al057	1963	1:15840
Sequatchie fine sandy loam, 0 to 2 percent slopes	SfA	898	329705	c22n	al063	2013	1:
Sequatchie fine sandy loam, undulating phase	Sfu	4802	522956	kk5k	al071	1943	1:24000
Sequatchie fine sandy loam, level phase	Sfv	1268	522957	kk5l	al071	1943	1:24000
Sequatchie fine sandy loam, eroded, undulating phase	Sa	1423	330169	c2km	al079	1950	1:20000
Sequatchie fine sandy loam, undulating phase	Sb	1098	330170	c2kn	al079	1950	1:20000
Sequatchie fine sandy loam, eroded	Sf	1678	523187	kkf0	al089	1958	1:24000
Sequatchie fine sandy loam	Se	1182	523186	kkdz	al089	1958	1:24000
Sequatchie fine sandy loam	Sa	2541	331151	c3l9	al103	1949	1:15840
Sequatchie fine sandy loam, eroded	Sb	1682	331152	c3lb	al103	1949	1:15840
Sequatchie loam	Se	1269	565819	lzs7	ar067	1971	1:20000
Sequatchie silt loam, 0 to 2 percent slopes, rarely flooded	SaA	1602	2480323	2p7zf	ga619	2012	1:24000
Sequatchie silt loam, 2 to 6 percent slopes	SaB	1243	2480324	2p7zg	ga619	2012	1:24000
Sequatchie loam, 0 to 2 percent slopes, occasionally flooded	SaA	2540	562871	lwq4	ga648	2001	1:12000
Sequatchie loam, 2 to 6 percent slopes	SaB	2235	562872	lwq5	ga648	2001	1:12000
Sequatchie loam, rarely flooded	Se	3819	526684	kp1t	tn007	1987	1:24000
Sequatchie loam, undulating phase	Sa	765	526972	kpc3	tn011	1951	1:20000
Sequatchie loam, 1 to 5 percent slopes, occasionally flooded	SaB	306	524274	klk2	tn013	1993	1:24000
Sequatchie fine sandy loam	St	1258	524553	klv2	tn025	1948	1:24000
Sequatchie fine sandy loam, eroded, gently sloping phase	Se	1403	524986	km91	tn031	1956	1:20000
Sequatchie fine sandy loam, gently sloping phase	Sd	289	524985	km90	tn031	1956	1:20000
Sequatchie fine sandy loam, level phase	Sc	120	524984	km8z	tn031	1956	1:20000
Sequatchie sandy clay loam, severely eroded, sloping phase	Sf	85	524987	km92	tn031	1956	1:20000
Sequatchie loam, 2 to 5 percent slopes	SeB	216	523897	kl4x	tn035	1998	1:24000
Sequatchie fine sandy loam	Se	1867	523438	kkp3	tn037	1977	1:15840
Sequatchie fine sandy loam	Sh	1083	327362	bzn2	tn039	2008	1:24000
Sequatchie fine sandy loam, undulating phase	Sa	2268	527254	kpn6	tn051	1950	1:20000
Sequatchie fine sandy loam, severely eroded rolling phase	Sb	62	527255	kpn7	tn051	1950	1:20000
Sequatchie loam	Sb	399	525199	kmhx	tn059	1954	1:15840
Sequatchie loam, 0 to 2 percent slopes, rarely flooded	SeA	2525	525263	kmkz	tn061	1990	1:24000
Sequatchie loam, 2 to 6 percent slopes	SeB	1170	525264	kml0	tn061	1990	1:24000
Sequatchie loam, 2 to 7 percent slopes	SeB	4855	1017881	1355w	tn065	1980	1:15840
Sequatchie-Urban land complex, 2 to 7 percent slopes	SfB	3567	1017882	1355x	tn065	1980	1:15840
Humphreys silt loam, 2 to 5 percent slopes, eroded (Sequatchie)	HmB2	1277	327577	bzw0	tn071	1961	1:15840
Sequatchie fine sandy loam, 2 to 5 percent slopes, eroded	ScB2	682	327628	bzxn	tn071	1961	1:15840
Sequatchie loam, 2 to 8 percent slopes, severely eroded	SeC3	339	327629	bzxp	tn071	1961	1:15840
Sequatchie fine sandy loam, 0 to 2 percent slopes	ScA	262	327627	bzxm	tn071	1961	1:15840
Sequatchie loam, 2 to 5 percent slopes	ShB	1708	525848	kn5v	tn103	1999	1:24000
Sequatchie fine sandy loam, gently sloping phase	SaB	140	525993	knbj	tn105	1958	1:15840
Sequatchie loam, gently sloping phase	ScB	112	525994	knbk	tn105	1958	1:15840
Sequatchie loam, sloping phase	ScC	108	525995	knbl	tn105	1958	1:15840
Congaree loam, sloping phase (Sequatchie)	CoC	20	525915	kn80	tn105	1958	1:15840
Sequatchie loam, eroded undulating phase	Sg	4174	526305	knnl	tn115	1951	1:20000
Sequatchie loam, undulating phase	Sf	2623	526304	knnk	tn115	1951	1:20000
Sequatchie fine sandy loam, undulating phase	Sd	989	526302	knnh	tn115	1951	1:20000
Sequatchie loam, eroded rolling phase	Sh	721	526306	knnm	tn115	1951	1:20000
Sequatchie fine sandy loam, eroded undulating phase	Se	325	526303	knnj	tn115	1951	1:20000
Sequatchie loam	Sa	362	527926	kqbw	tn123	1974	1:20000
Sequatchie silt loam, 2 to 5 percent slopes, rarely flooded	SeB	2762	523777	kl11	tn139	1997	1:24000
Sequatchie loam, 0 to 2 percent slopes, rarely flooded	SeA	1918	529638	ks43	tn153	1995	1:24000
Sequatchie loam, 0 t0 2 percent slopes	SaA	1529	529637	ks42	tn153	1995	1:24000
Sequatchie loam, 2 to 6 percent slopes	SeB	1210	529639	ks44	tn153	1995	1:24000
Sequatchie fine sandy loam, 0 to 2 percent slopes, occasionally flooded	Sc	105	2396970	2lg7m	tn161	1953	1:20000
Sequatchie fine sandy loam, 2 to 5 percent slopes	Hg	59	2396918	2lg5y	tn161	1953	1:20000
Sequatchie fine sandy loam	Se	245	529996	kshn	tn173	1945	1:24000
Sequatchie loam, 2 to 5 percent slopes	SeB	2258	529918	ksf4	tn177	1965	1:15840
Sequatchie loam, 0 to 2 percent slopes	SeA	740	529917	ksf3	tn177	1965	1:15840
Sequatchie loam, 5 to 12 percent slopes, eroded	SeC2	734	529919	ksf5	tn177	1965	1:15840
Sequatchie loam, 1 to 5 percent slopes, rarely flooded	SeB	1234	1689703	1tq8k	tn179	1955	1:15840
Sequatchie loam, phosphatic	Se	400	523580	kktp	tn187	1961	1:15840
Sequatchie loam	Se	688	528603	kr1q	tn602	1973	1:15840
Sequatchie loam	Sa	3402	528675	kr41	tn604	1974	1:20000
Sequatchie loam, rarely flooded	Sb	2365	529676	ks5b	tn608	2001	1:24000
Sequatchie silt loam	Sd	939	1899553	21rmx	tn609	1955	1:20000
Sequatchie loam	Sc	581	1899552	21rmw	tn609	1955	1:20000
Sequatchie fine sandy loam	Sb	387	1899551	21rmv	tn609	1955	1:20000
Sequatchie loam, 2 to 5 percent slopes	SeB	799	2427500	2mh0g	tn610	1960	1:15840
Sequatchie loam, 5 to 12 percent slopes, eroded	SeC2	226	2427501	2mh0h	tn610	1960	1:15840
Sullivan-Sequatchie-Egam complex, 1 to 6 percent slopes, rarely to occasionally flooded	SnB	4826	2439182	2mw59	tn701	1985	1:24000

Map of Series Extent

Approximate geographic distribution of the SEQUATCHIE 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).