Soil Data Explorer - LEWISVILLE

Official Series Description

Lab Data Summary

Aggregate lab data for the LEWISVILLE soil series. This aggregation is based on all pedons with a current taxon name of LEWISVILLE, 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 LEWISVILLE 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
n/a	S97TX099001	S97TX099001	Lewisville	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 LEWISVILLE 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 LEWISVILLE 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 LEWISVILLE 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 LEWISVILLE 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.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with LEWISVILLE 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 LEWISVILLE 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 LEWISVILLE 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 LEWISVILLE, 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. TX-2010-11-04-06 | McLennan County - 2001

   Pattern of soils in the Crawford-Purves and Slidell-Sanger general soil map units (Soil Survey of McLennan County, Texas; 2001).

2. TX-2010-11-04-09 | Milam County - 2004

   Typical pattern of soils and underlying material in the Branyon-Burleson general soil map unit (Soil Survey of Milam County, Texas; 2004).

3. TX-2012-03-20-21 | Comal and Hays Counties - June 1984

   Pattern of soils in the Brackett-Comfort-Real general soil map unit (Soil Survey of Comal and Hays Counties, TX; 1984).

4. TX-2012-03-20-24 | Comal and Hays Counties - June 1984

   Pattern of soils in the Lewisville-Gruene-Krum and Branyon-Krum general soil map units (Soil Survey of Comal and Hays Counties, TX; 1984).

5. TX-2012-03-20-27 | Coryell County - May 1985

   Typical pattern of soils in the Nuff-Cho map unit and the Doss-Real-Krum map unit (Soil Survey of Coryell County, TX; 1985).

6. TX-2012-03-20-29 | Coryell County - May 1985

   Typical pattern of soils in the Bosque-Frio-Lewisville map unit and the Bastsil-Minwells map unit (Soil Survey of Coryell County, TX; 1985).

7. TX-2012-03-20-42 | Ellis County - August 1964

   Geographical association of soils on benches. Burleson clay, terrace; Houston Black clay, terrace; and Lewisville soils are in soil association 1 (Soil Survey of Ellis County, TX; 1964).

Map Units

Map units containing LEWISVILLE 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
Lewisville silty clay, 1 to 3 percent slopes	LeB	14129	391107	2vtgn	tx027	1972	1:24000
Lewisville silty clay, 3 to 5 percent slopes, eroded	LeC2	7111	391108	2vth0	tx027	1972	1:24000
Lewisville-Altoga complex, 2 to 5 percent slopes	LegC	6488	391109	2s1s0	tx027	1972	1:24000
Lewisville-Krum complex, 1 to 3 percent slopes	LekB	1192	3130052	2s1s2	tx027	1972	1:24000
Lewisville-Urban land complex, 1 to 5 percent slopes	LeuC	449	391110	f3zg	tx027	1972	1:24000
Lewisville silty clay, 0 to 1 percent slopes	LeA	314	3130050	2vtgz	tx027	1972	1:24000
Lewisville silty clay, 0 to 1 percent slopes	LvA	42276	390488	2vtgz	tx029	2000	1:24000
Lewisville silty clay, 1 to 3 percent slopes	LvB	32018	390489	2vtgn	tx029	2000	1:24000
Lewisville silty clay, 3 to 5 percent slopes, eroded	LvC	468	390490	2vth0	tx029	2000	1:24000
Lewisville silty clay, 0 to 1 percent slopes	LeA	6141	363520	2vtgz	tx055	1972	1:20000
Lewisville silty clay, 1 to 3 percent slopes	LeB	6020	363521	2vtgn	tx055	1972	1:20000
Lewisville silty clay, 3 to 5 percent slopes, eroded	LeC2	1277	363522	2vth0	tx055	1972	1:20000
Lewisville silty clay, 3 to 5 percent slopes, eroded	LeC2	12137	364084	2vth0	tx085	1965	1:20000
Lewisville silty clay, 1 to 3 percent slopes	LeB	2032	364083	2vtgn	tx085	1965	1:20000
Lewisville clay loam, 1 to 3 percent slopes	LeB	7533	364388	2wn9n	tx093	1974	1:20000
Lewisville clay loam, 3 to 5 percent slopes	LeC	5002	364389	2wn9p	tx093	1974	1:20000
Lewisville clay loam, 1 to 5 percent slopes	41	3433	364491	d78s	tx097	1973	1:24000
Lewisville clay loam, 5 to 8 percent slopes	42	1990	364492	d78t	tx097	1973	1:24000
Lewisville clay loam, 1 to 3 percent slopes	LeB	15921	391161	2wn9n	tx099	1983	1:24000
Lewisville-Urban land complex, 0 to 4 percent slopes	49	10158	364832	d7ms	tx113	1975	1:20000
Austin-Lewisville complex, 5 to 8 percent slopes, erode d	7	3965	364855	d7nj	tx113	1975	1:20000
Lewisville silty clay, 3 to 5 percent slopes, eroded	47	3932	364830	2vth0	tx113	1975	1:20000
Lewisville silty clay, 1 to 3 percent slopes	46	3783	364829	2vtgn	tx113	1975	1:20000
Lewisville-Urban land complex, 4 to 8 percent slopes	50	3294	364834	d7mv	tx113	1975	1:20000
Lewisville silty clay, 5 to 8 percent slopes	48	856	364831	d7mr	tx113	1975	1:20000
Lewisville clay loam, 3 to 5 percent slopes	53	2775	365006	2wn9p	tx121	1975	1:24000
Lewisville clay loam, 1 to 3 percent slopes	52	1771	365005	2wn9n	tx121	1975	1:24000
Lewisville silty clay, 5 to 8 percent slopes, eroded	LeD2	5727	365320	d84j	tx139	1962	1:20000
Lewisville silty clay, 3 to 5 percent slopes, eroded	LeC2	4594	365319	2vth0	tx139	1962	1:20000
Lewisville silty clay, 1 to 3 percent slopes	LeB	3745	365318	2vtgn	tx139	1962	1:20000
Lewisville association, 3 to 5 percent slopes, moderately eroded	LWC2	1341	365313	2vv4r	tx139	1962	1:20000
Lewisville association, 1 to 3 percent slopes	LWB	808	365312	2vv4q	tx139	1962	1:20000
Lewisville silty clay, 0 to 1 percent slopes	LeA	693	365317	2vtgz	tx139	1962	1:20000
Lewisville association, 5 to 8 percent slopes, eroded	LWD2	554	365314	d84b	tx139	1962	1:20000
Altoga-Lewisville-Duffau complex, 3 to 20 percent slopes, moderately eroded	AdE2	17798	365346	2xsln	tx143	1966	1:20000
Lewisville clay loam, 3 to 5 percent slopes	LeC	16116	365382	2wn9p	tx143	1966	1:20000
Altoga-Lewisville clay loams, 5 to 8 percent slopes, eroded	AlD2	12561	365347	2xslp	tx143	1966	1:20000
Lewisville clay loam, 1 to 3 percent slopes	LeB	11498	365381	2wn9n	tx143	1966	1:20000
Lewisville-Altoga clay loams, 3 to 5 percent slopes, eroded	LgC2	3780	365383	2xslq	tx143	1966	1:20000
Lewisville silty clay, 3 to 5 percent slopes, eroded	37	3872	365456	2vth0	tx145	1975	1:20000
Lewisville silty clay, 1 to 3 percent slopes	36	3331	365455	2vtgn	tx145	1975	1:20000
Lewisville silty clay, 1 to 3 percent slopes	LvB	1026	365535	2sshh	tx147	1989	1:24000
Lewisville clay loam, dry, 0 to 1 percent slopes	LeA	4743	366200	3125b	tx171	1970	1:20000
Lewisville clay loam, dry, 1 to 3 percent slopes	LeB	1773	366201	3125f	tx171	1970	1:20000
Lewisville clay loam, dry, 3 to 5 percent slopes	LeC	773	366202	3125g	tx171	1970	1:20000
Lewisville silty clay, 3 to 5 percent slopes, eroded	47	4164	366684	2vth0	tx181	1977	1:20000
Lewisville silty clay, 1 to 3 percent slopes	46	2150	366683	2vtgn	tx181	1977	1:20000
Lewisville silty clay, 1 to 3 percent slopes	LeB	6070	366864	2vtgn	tx187	1973	1:20000
Lewisville silty clay, 0 to 1 percent slopes	LeA	5086	366863	2vtgz	tx187	1973	1:20000
Lewisville silty clay, 1 to 3 percent slopes	LeB	2393	368182	2vtgn	tx251	1981	1:20000
Lewisville silty clay, 3 to 5 percent slopes, eroded	LeC	1676	368183	2vth0	tx251	1981	1:20000
Lewisville silty clay, 1 to 3 percent slopes	LeB	13273	370107	2vtgn	tx309	1992	1:24000
Lewisville-Altoga complex, 2 to 5 percent slopes	LegC	2135	3130083	2s1s0	tx331	1988	1:24000
Lewisville-Krum complex, 1 to 3 percent slopes	LekB	1533	3130084	2s1s2	tx331	1988	1:24000
Lewisville silty clay, 1 to 3 percent slopes	LeB	1359	370680	2vtgn	tx331	1988	1:24000
Lewisville silty clay, 0 to 1 percent slopes	LeA	100	3130082	2vtgz	tx331	1988	1:24000
Lewisville silty clay, 1 to 3 percent slopes	LcB	6181	393219	2vtgn	tx453	1969	1:20000
Lewisville silty clay, 0 to 1 percent slopes	LcA	4452	393218	2vtgz	tx453	1969	1:20000
Lewisville soils and Urban land, 0 to 2 percent slopes	LeB	2252	393220	f65j	tx453	1969	1:20000
Lewisville-Altoga complex, 2 to 5 percent slopes	LegC	6542	3130118	2s1s0	tx491	1981	1:20000
Lewisville-Krum complex, 1 to 3 percent slopes	LekB	1244	3130119	2s1s2	tx491	1981	1:20000
Lewisville silty clay, 0 to 1 percent slopes	LeA	856	3130120	2vtgz	tx491	1981	1:20000
Lewisville clay loam, 1 to 3 percent slopes	27	8431	373920	31258	tx601	1977	1:31680
Lewisville clay loam, 0 to 1 percent slopes	26	5482	373919	30gjn	tx601	1977	1:31680
Lewisville silty clay, 1 to 3 percent slopes	LeB	9029	393472	2vtgn	tx604	1981	1:20000
Lewisville silty clay, 0 to 1 percent slopes	LeA	4111	393471	2vtgz	tx604	1981	1:20000
Lewisville silty clay, 3 to 8 percent slopes	LeC	1223	374487	dkp7	tx612	1973	1:20000
Lewisville silty clay, 1 to 3 percent slopes	LeB	854	374486	2vtgn	tx612	1973	1:20000

Map of Series Extent

Approximate geographic distribution of the LEWISVILLE 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).