Soil Data Explorer - TENSAS

Official Series Description

Lab Data Summary

Aggregate lab data for the TENSAS soil series. This aggregation is based on all pedons with a current taxon name of TENSAS, 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 TENSAS 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
131A	96P0214	1996LA107005	Tensas	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	31.9244442,-91.3994446

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TENSAS 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 TENSAS 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 TENSAS 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 TENSAS 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 TENSAS 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 TENSAS 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 TENSAS 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 flats position figure.

Soil series sharing subgroup-level classification with TENSAS, 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. LA-2012-02-01-02 | East Carroll Parish - February 1988

   Soils-landscape-parent material relationship across East Carroll Parish (Soil Survey of East Carroll Parish, Louisiana; February 1988).

2. LA-2012-02-01-03 | Richland Parish - September 1993

   Relationship of soils, landscape, and parent material in Richland Parish (Soil Survey of Richland Parish, Louisiana; September 1993).

3. LA-2012-04-27-03 | Franklin Parish - August 1981

   Soils, parent material, and landscape position from east to west in the parish (Soil Survey of Franklin Parish, Louisiana; August 1981).

4. MS-2010-09-08-01 | Holmes County -

   Typical pattern of soils and underlying material in the Dundee-Dubbs-Tensas general soil map unit.

Map Units

Map units containing TENSAS 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
Tensas-Sharkey complex, overwash, undulating, occasionally flooded	Ts	24686	1711971	1vgfw	la009	1981	1:24000
Tensas silty clay, overwash, occasionally flooded	Te	10456	1711969	1vgft	la009	1981	1:24000
Tensas-Sharkey complex, undulating	Tn	4658	1711970	1vgfv	la009	1981	1:24000
Tensas silty clay, 0 to 1 percent slopes, rarely flooded	Ta	3666	1711968	2v189	la009	1981	1:24000
Tensas silty clay loam	Bd	834	1715806	1vlfl	la009	1981	1:24000
Tensas-Alligator complex, undulating	Tn	25467	1722428	1vtb6	la025	1983	1:24000
Tensas silty clay, 0 to 1 percent slopes, rarely flooded	Ta	12446	1722426	2v189	la025	1983	1:24000
Tensas-Alligator complex, undulating, occasionally flooded	Ts	11413	1722429	1vtb7	la025	1983	1:24000
Tensas silty clay, occasionally flooded	Te	3708	1722427	1vtb5	la025	1983	1:24000
Tensas-Alligator complex, undulating	To	64351	1723886	1vvv7	la029	1983	1:24000
Tensas-Alligator complex, undulating, occasionally flooded	Tr	17320	1723887	1vvv8	la029	1983	1:24000
Dundee-Alligator-Tensas complex, gently undulating	Dh	12388	1723869	1vvtp	la029	1983	1:24000
Dundee-Alligator-Tensas complex, undulating	Ds	10959	1723870	1vvtq	la029	1983	1:24000
Tensas silty clay, 0 to 1 percent slopes, rarely flooded	Tc	10485	1723884	2v189	la029	1983	1:24000
Tensas silty clay, occasionally flooded	Te	2908	1723885	1vvv6	la029	1983	1:24000
Tensas silty clay, 0 to 1 percent slopes, rarely flooded	Ta	12348	569504	2v189	la035	1985	1:24000
Tensas-Dundee complex, gently undulating	Td	9224	569505	m3m4	la035	1985	1:24000
Tensas-Sharkey complex, 0 to 3 percent slopes, gently undulating	Te	3155	569506	2sscs	la035	1985	1:24000
Tensas-Sharkey complex, 0 to 3 percent slopes, gently undulating	Ts	6722	1711116	2sscs	la041	1979	1:24000
Tensas silty clay, 0 to 1 percent slopes, rarely flooded	Te	5501	1711115	2v189	la041	1979	1:24000
Tensas silty clay, occasionally flooded	Te	1330	1600194	1qq45	la059	1986	1:24000
Tensas-Sharkey complex, 0 to 3 percent slopes, gently undulating	Ts	59753	808558	2sscs	la065	1972	1:24000
Tensas silty clay, 0 to 1 percent slopes, rarely flooded	Ta	11312	808557	2v189	la065	1972	1:24000
Tensas-Sharkey complex, 0 to 3 percent slopes, gently undulating	Ts	1468	1714808	2sscs	la083	1988	1:24000
Dundee-Tensas complex, gently undulating	Ds	1258	1714772	1vkc7	la083	1988	1:24000
Tensas silty clay, 0 to 1 percent slopes, rarely flooded	Tc	213	1714807	2v189	la083	1988	1:24000
Tensas-Sharkey complex, gently undulating	Ts	13130	823559	wmzf	la097	1983	1:24000
Tensas silty clay loam, 0 to 1 percent slopes	Te	25745	1451683	1kqlh	la099	1974	1:24000
Tensas-Sharkey clays, 0 to 3 percent slopes, gently undulating	TeB	111023	577263	2sscr	la107	2001	1:24000
Tensas-Sharkey-Dundee complex, gently undulating	TkB	19476	578950	mfft	la107	2001	1:24000
Tensas clay, 0 to 1 percent slopes	TaA	12867	577262	mcpc	la107	2001	1:24000
Tensas-Sharkey complex, undulating	TeD	3369	577258	mcp7	la107	2001	1:24000
Tensas silty clay loam, 0 to 1 percent slopes, occasionally flooded	Te	10539	2693431	2rv5x	ms051	1997	1:20000
Alligator, Tensas, and Dowling soils, frequently flooded	ATF	4342	567943	m1zr	ms051	1997	1:20000
Tensas silty clay loam, 0 to 1 percent slopes	27	42602	568122	m25j	ms083	1997	1:24000
Tensas-Alligator complex, 0 to 3 percent slopes, occasionally flooded	30	23308	568125	m25m	ms083	1997	1:24000
Alligator, Tensas, and Dowling soils, frequently flooded	7	19494	568120	m25g	ms083	1997	1:24000
Tensas silty clay loam, 1 to 3 percent slopes	28	13037	568123	m25k	ms083	1997	1:24000
Tensas-Alligator-Urban land complex, 0 to 3 percent slopes	31	4385	568126	m25n	ms083	1997	1:24000
Tensas silty clay loam, 3 to 8 percent slopes	29	1297	568124	m25l	ms083	1997	1:24000
Dundee and Tensas silt loams, 0 to 3 percent slopes	DtA	14509	568520	m2lc	ms135	1966	1:24000
Tensas silty clay loam, 0 to 2 percent slopes	120	17690	1715963	1vlln	ms143	2006	1:24000
Askew-Tensas-Openlake complex, undulating	116	6688	1715962	1vllm	ms143	2006	1:24000
Tensas-Sharkey complex, undulating	278	2614	1715974	1vlm0	ms143	2006	1:24000

Map of Series Extent

Approximate geographic distribution of the TENSAS 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).