Soil Data Explorer - SENGTOWN

Official Series Description

Lab Data Summary

Aggregate lab data for the SENGTOWN soil series. This aggregation is based on all pedons with a current taxon name of SENGTOWN, 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 SENGTOWN 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
122	40A4923	1954TN031002	Sengtown	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.4969444,-85.9011078
122	85P0274	1984TN165038	Sengtown	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.6208344,-86.4194412
n/a	40A4924	1954TN031013	Sengtown	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 SENGTOWN 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 SENGTOWN 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 SENGTOWN 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 SENGTOWN 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).

Competing Series

Soil series competing with SENGTOWN 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 SENGTOWN 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 SENGTOWN 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 SENGTOWN, 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. TN-2010-11-02-07 | Dickson County -

   The relationship of soils and landscape in the Hawthorne-Sulphura-Sengtown and Wolftever-Beason-Melvin general soil map units (Soil Survey of Dickson County, Tennessee).

2. TN-2010-11-02-08 | Hickman County - 2008

   Typical pattern of soils and parent material in the Humphreys-Riverby-Tarklin and Biffle Sengtown general soil map units (Soil Survey of Hickman County, Tennessee; 2008).

3. TN-2010-11-02-09 | Hickman County - 2008

   Typical pattern of soils and parent material in the Sengtown-Mountview-Dickson and Sengtown general soil map units (Soil Survey of Hickman County, Tennessee; 2008).

4. TN-2010-11-02-27 | Overton County - 2005

   The relationship of soils and landscapes in the Garmon-Newbern and Christian-Sengtown general soil map units (Soil Survey of Overton County, Tennessee; 2005).

5. TN-2012-03-16-01 | Cheatham County - 2002

   Relationship of soils to topography and the underlying material in the Sengtown-Mountview-Dickson general soil map unit (Soil Survey of Cheatham County, TN; 2002).

6. TN-2012-03-16-02 | Cheatham County - 2002

   Relationship of soils to topography and the underlying material in the Beason-Wolftever-Melvin-Arrington and Hawthorne-Sulphura-Sengtown general soil map units (Soil Survey of Cheatham County, TN; 2002).

7. TN-2012-03-16-04 | Dickson County - 2002

   The relationship of soils, landscape, and parent material in the Sengtown general soil map unit (Soil Survey of Dickson County, TN; 2002).

8. TN-2012-03-16-05 | Dickson County - 2002

   The relationship of soils, landscape, and parent material in the Hawthorne-Sulphura-Sengtown and the Wolftever-Beason-Melvin general soil map units (Soil Survey of Dickson County, TN; 2002).

Map Units

Map units containing SENGTOWN 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
Hawthorne-Sengtown-Sugargrove complex, 20 to 70 percent slopes	HsF	6142	2232300	2dxwp	ky610	1968	1:12000
Sugargrove-Sengtown-Hawthorne complex, 12 to 20 percent slopes, severely eroded	ShD3	270	2232260	2dxvd	ky610	1968	1:12000
Hawthorne-Sengtown-Sugargrove complex, 20 to 70 percent slopes, severely eroded	HsF3	226	2623443	2qykj	ky610	1968	1:12000
Sugargrove-Sengtown-Hawthorne complex, 12 to 25 percent slopes	SuE	31650	2545390	2qshn	tn005	2011	1:12000
Hawthorne, Sengtown, and Sugargrove soils, 25 to 70 percent slopes	HTF	25038	2545345	2qsg4	tn005	2011	1:12000
Sugargrove-Sengtown-Hawthorne complex, 5 to 12 percent slopes	SuC	2621	2545391	2qshp	tn005	2011	1:12000
Sengtown gravelly silt loam, 5 to 12 percent slopes	SgC2	28720	527029	2td2n	tn021	1991	1:24000
Sengtown gravelly silt loam, 12 to 20 percent slopes	SgD2	15984	527030	2qh76	tn021	1991	1:24000
Sengtown gravelly silt loam, 30 to 60 percent slopes	SgF	6390	527031	2qh75	tn021	1991	1:24000
Sengtown-Rock outcrop complex, 20 to 60 percent slopes	SrF	2963	527032	kpf1	tn021	1991	1:24000
Sengtown gravelly silt loam, 2 to 5 percent slopes, eroded	SgB2	272	527028	kpdx	tn021	1991	1:24000
Sengtown cobbly loam, 5 to 12 percent slopes, eroded	SeC2	326	531117	ktnt	tn027	2002	1:24000
Sengtown cobbly loam, 20 to 40 percent slopes, eroded	SeE2	199	636838	pcp5	tn027	2002	1:24000
Sengtown cobbly loam, 12 to 20 percent slopes, eroded	SeD2	183	636836	pcp3	tn027	2002	1:24000
Sengtown gravelly silt loam, 5 to 12 percent slopes	SeC	2177	2749933	2td2n	tn031	1956	1:20000
Sengtown gravelly silt loam, 12 to 20 percent slopes	SeD	605	2749950	2qh76	tn031	1956	1:20000
Sengtown gravelly silt loam, 5 to 12 percent slopes	BcC	2354	523405	2td2n	tn037	1977	1:15840
Sengtown gravelly silt loam, 12 to 20 percent slopes	BcD	2095	523406	2qh76	tn037	1977	1:15840
Sengtown gravelly silt loam, 5 to 12 percent slopes	SeC	68047	527125	kpj1	tn043	1993	1:24000
Sengtown gravelly silt loam, 30 to 60 percent slopes	SeF	59652	527128	2qh75	tn043	1993	1:24000
Sengtown gravelly silt loam, 12 to 20 percent slopes	SeD2	44222	527127	2qh76	tn043	1993	1:24000
Sengtown-Urban land complex, 2 to 12 percent slopes	StC	6150	527130	kpj6	tn043	1993	1:24000
Sengtown gravelly silt loam, 5 to 12 percent slopes	SeC2	4276	527126	2td2n	tn043	1993	1:24000
Sengtown-Rock outcrop complex, 20 to 60 percent slopes	SrF	3908	527129	kpj5	tn043	1993	1:24000
Sugargrove-Sengtown-Hawthorne complex, 12 to 25 percent slopes	SuE	2005	2545312	2qs9t	tn079	2012	1:12000
Hawthorne, Sengtown, and Sugargrove soils, 25 to 70 percent slopes	HTF	841	2545261	2qs85	tn079	2012	1:12000
Sugargrove-Sengtown-Hawthorne complex, 5 to 12 percent slopes	SuC	64	2545313	2qs9v	tn079	2012	1:12000
Sengtown-Mountview complex, 5 to 12 percent slopes, eroded	SmC2	56276	527490	kpwt	tn081	1997	1:24000
Sengtown gravelly silt loam, 12 to 20 percent slopes	SeD2	12811	527488	2qh76	tn081	1997	1:24000
Sengtown gravelly silt loam, 30 to 60 percent slopes	SeF	12758	527489	2qh75	tn081	1997	1:24000
Sengtown gravelly silt loam, 5 to 12 percent slopes	SeC	1228	527487	2td2n	tn081	1997	1:24000
Sengtown-Rock outcrop complex, 20 to 60 percent slopes	SrF	488	527491	kpwv	tn081	1997	1:24000
Sengtown gravelly silt loam, 30 to 60 percent slopes	SeF	6599	2749966	2qh75	tn083	1952	1:20000
Sengtown gravelly silt loam, 12 to 20 percent slopes	SeD	4904	2749954	2qh76	tn083	1952	1:20000
Sengtown gravelly silt loam, 5 to 12 percent slopes	SeC	1696	2749937	2td2n	tn083	1952	1:20000
Sengtown gravelly silt loam, 5 to 12 percent slopes	Bl	1144	527558	2td2n	tn085	1943	1:20000
Sengtown gravelly silt loam, 30 to 60 percent slopes	Bsz	107	527560	2qh75	tn085	1943	1:20000
Sengtown-Mountview complex, 5 to 12 percent slopes, eroded	SmC2	139	530883	ktf8	tn101	1999	1:24000
Sengtown gravelly silt loam, 5 to 12 percent slopes	SeC	6120	525849	2zpqg	tn103	1999	1:24000
Sengtown gravelly silt loam, 12 to 20 percent slopes	SeD	4177	525850	2zpqh	tn103	1999	1:24000
Sengtown gravelly silt loam, 5 to 12 percent slopes	SeC2	11147	527718	2td2n	tn111	1992	1:24000
Sengtown gravelly silt loam, 12 to 20 percent slopes	SeD2	4591	527719	2qh76	tn111	1992	1:24000
Sengtown gravelly silt loam, 12 to 20 percent slopes	SeD	78850	527964	2qh76	tn125	1972	1:15840
Sengtown gravelly silt loam, 5 to 12 percent slopes	SeC	40118	2749941	2td2n	tn125	1972	1:15840
Sengtown cobbly loam, 12 to 20 percent slopes, eroded	SeD2	10324	843341	x9kk	tn133	2003	1:24000
Sengtown cobbly loam, 20 to 40 percent slopes, eroded	SeE2	9149	843354	x9kz	tn133	2003	1:24000
Sengtown cobbly loam, 5 to 12 percent slopes, eroded	SeC2	5705	843340	x9kj	tn133	2003	1:24000
Sengtown gravelly silt loam, 5 to 12 percent slopes	SeC	45519	2749942	2td2n	tn147	1965	1:15840
Sengtown gravelly silt loam, 12 to 20 percent slopes	SeD	28476	528160	2qh76	tn147	1965	1:15840
Sengtown gravelly silt loam, 30 to 60 percent slopes	BaF	877	528148	2qh75	tn147	1965	1:15840
Sengtown gravelly silty clay loam, 20 to 30 percent slopes, severely eroded	BcE3	717	528151	2qh77	tn147	1965	1:15840
Sengtown gravelly silt loam, 5 to 12 percent slopes	StC2	1344	529840	2td2n	tn159	1992	1:24000
Sengtown gravelly silt loam, 2 to 5 percent slopes, eroded	StB2	202	529839	ksbl	tn159	1992	1:24000
Sengtown gravelly silt loam, 12 to 20 percent slopes	Be	4282	2396877	2qh76	tn161	1953	1:20000
Sengtown gravelly silt loam, 30 to 60 percent slopes	Bf	3810	2396878	2qh75	tn161	1953	1:20000
Sengtown gravelly silt loam, 5 to 12 percent slopes	SeC	3357	3160450	1kyz9	tn161	1953	1:20000
Sengtown silt loam, 12 to 20 percent slopes	Me	3280	2396934	2lg6g	tn161	1953	1:20000
Bodine and Sengtown soils, 20 to 40 percent slopes	BSE	3227	3160447	1kyyz	tn161	1953	1:20000
Sengtown-Rock outcrop complex, 20 to 60 percent slopes	Rf	1649	2396963	2lg7d	tn161	1953	1:20000
Sengtown gravelly silt loam, 12 to 20 percent slopes, severely eroded	Bd	1401	2396876	2lg4l	tn161	1953	1:20000
Sengtown silty clay loam, 5 to 12 percent slopes, severely eroded	Mk	823	2396938	2lg6l	tn161	1953	1:20000
Sengtown-Gullied land complex, 12 to 20 percent slopes	Rc	733	2396960	2lg79	tn161	1953	1:20000
Sengtown gravelly silt loam, 12 to 20 percent slopes	SeD2	11445	528383	2qh76	tn165	1993	1:20000
Sengtown gravelly silt loam, 5 to 12 percent slopes	SeC2	10046	528382	2td2n	tn165	1993	1:20000
Sengtown gravelly silt loam, 20 to 35 percent slopes, eroded	SeE2	796	528384	kqtn	tn165	1993	1:20000
Sengtown gravelly silt loam, 12 to 20 percent slopes	BaD	6850	529857	2qh76	tn177	1965	1:15840
Sengtown gravelly silt loam, 5 to 12 percent slopes	BaC	5527	529856	2td2n	tn177	1965	1:15840
Sengtown gravelly silty clay loam, 20 to 30 percent slopes, severely eroded	BcE3	1017	529862	2qh77	tn177	1965	1:15840
Sengtown gravelly silt loam, 30 to 60 percent slopes	BaF	684	529859	2qh75	tn177	1965	1:15840
Sengtown gravelly silt loam, 12 to 20 percent slopes	SeD	7189	2749961	2qh76	tn187	1961	1:15840
Sengtown gravelly silt loam, 5 to 12 percent slopes	BaC	4846	523463	2td2n	tn187	1961	1:15840
Sengtown gravelly silt loam, 12 to 20 percent slopes	SeD	4341	2749962	2qh76	tn610	1960	1:15840
Sengtown gravelly silt loam, 5 to 12 percent slopes	BaC2	3388	2427394	2td2n	tn610	1960	1:15840
Sengtown gravelly silty clay loam, 20 to 30 percent slopes, severely eroded	BcE3	1040	2427399	2qh77	tn610	1960	1:15840

Map of Series Extent

Approximate geographic distribution of the SENGTOWN 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).