LOCATION WARRENLAKE              TX

Established Series
JKW-AKS
08/2019

WARRENLAKE SERIES


The Warrenlake series consists of very deep, somewhat poorly drained soils. These nearly level soils formed in loamy fluviomarine deposits of the Lissie Formation. Slope ranges from 0 to 1 percent. Mean annual air temperature is about 20 degrees C (68 degrees F). Mean annual precipitation is about 1118 mm (44 in).

TAXONOMIC CLASS: Coarse-loamy, siliceous, superactive, hyperthermic Typic Natraqualfs

TYPICAL PEDON: Warrenlake very fine sandy loam, in slight depression in rangeland at an elevation of 38 m (125 ft) (Colors are for moist soil unless otherwise stated.)

A1--0 to 15 cm, (0 to 6 in), (0 to 15 cm); brown (10YR 5/3), very fine sandy loam, pale brown (10YR 6/3) dry; massive; very friable; common fine roots and many very fine roots; common very fine tubular pores; 1 percent fine prominent yellowish brown (10YR 5/8) masses of oxidized iron with clear boundaries lining pores; EC is 16.4 dS/m; SAR is 48; slightly acid; abrupt wavy boundary.

A2--15 to 29 cm, (6 to 11 in); dark gray (10YR 4/1), very fine sandy loam, gray (10YR 5/1) dry; weak medium and coarse columnar structure parting to moderate coarse angular blocky; friable; many very fine roots; common very fine tubular pores; 3 percent prominent very pale brown (10YR 8/3) sand coats on vertical faces of peds; 1 percent fine distinct dark yellowish brown (10YR 4/4) masses of oxidized iron with clear boundaries lining pores; 1 percent fine threadlike white (5Y8/1) salt crystals; EC is 19.7 dS/m; SAR is 57; slightly alkaline; clear wavy boundary.

Btnz--29 to 46 cm, (11 to 18 in); grayish brown (10YR 5/2), very fine sandy loam, light brownish gray (10YR 6/2) dry; moderate coarse subangular blocky structure; friable; common very fine roots; many very fine tubular pores; 20 percent distinct gray (10YR 5/1)clay films on all faces of peds; 1 percent fine prominent yellowish brown (10YR 5/6)masses of oxidized iron with clear boundaries lining pores; 1 percent fine prominent strong brown (7.5YR 4/6)masses of oxidized iron with clear boundaries lining pores; 2 percent fine threadlike white (5Y 8/1) salt crystals; EC is 23.6 dS/m; SAR is 59; slightly alkaline; gradual broken boundary.

Btnzy1--46 to 67 cm, (18 to 26 in); gray (10YR 5/1), loam gray (10YR 6/1); moderate coarse subangular blocky structure; firm; common very fine roots; common very fine tubular pores; 50 percent prominent grayish brown (10YR 5/2) clay films on vertical faces of peds; 1 percent fine dark brown (7.5YR 3/4)iron-manganese nodules with sharp boundaries in matrix; 1 percent fine black (10YR 2/1)iron-manganese masses with sharp boundaries in matrix; 6 percent medium prominent yellowish brown (10YR 5/8) masses of oxidized iron with diffuse boundaries in matrix; 15 percent medium prominent strong brown (7.5YR 5/8) masses of oxidized iron with clear boundaries in matrix; 2 percent fine white (10YR 8/1) gypsum crystals; 10 percent fine white (5Y 8/1) salt masses; EC is 22.5 dS/m; SAR is 55; slightly alkaline; diffuse broken boundary.

Btnzy2--67 to 97 cm, (26 to 38 in); light brownish gray (10YR 6/2), loam, light gray (10YR 7/2) dry; moderate coarse subangular blocky structure; firm; common very fine roots; common very fine tubular pores; 20 percent prominent grayish brown (10YR 5/2) clay films on vertical faces of peds; 2 percent fine prominent yellowish red (5YR 5/8) masses of oxidized iron with sharp boundaries in matrix; 4 percent fine and medium prominent strong brown (7.5YR 5/8) masses of oxidized iron with clear boundaries in matrix; 8 percent medium and coarse prominent black (10YR 2/1)iron-manganese masses with sharp boundaries in matrix; 10 percent fine and medium prominent brownish yellow (10YR 6/8), moist, masses of oxidized iron with diffuse boundaries in matrix; 2 percent fine white (10YR 8/1) gypsum crystals; 6 percent fine white (5Y 8/1) salt masses; EC is 20.4 dS/m; SAR is 51; slightly alkaline; gradual smooth boundary.

Btnzy3--97 to 180 cm, (38 to 71 in); light brownish gray (2.5Y 6/2), sandy clay loam, light gray (2.5Y 7/2) dry; weak very coarse subangular blocky structure; friable; common very fine roots; common very fine tubular pores; 25 percent prominent gray (10YR 5/1) clay films on vertical faces of peds; 4 percent fine distinct yellowish brown (10YR 5/8) masses of oxidized iron with diffuse boundaries in matrix; 4 percent medium prominent black (10YR 2/1)masses of oxidized iron with sharp boundaries in matrix; 8 percent fine and medium prominent strong brown (7.5YR 5/8) masses of oxidized iron with clear boundaries in matrix; 1 percent fine white (10YR 8/1) gypsum crystals; 2 percent fine white (5Y 8/1)salt masses; EC is 13.8 dS/m; SAR is 45; slightly alkaline; diffuse broken boundary.

Btnzy4--180 to 203 cm, (71 to 80 in); gray (2.5Y 5/1), clay loam light gray (2.5Y 7/1)dry; massive; firm; common very fine roots; common very fine tubular pores; 1 percent faint pressure faces; 10 percent prominent very pale brown (10YR 8/3) sand coats on vertical faces of peds; 20 percent faint gray (10YR 5/1) clay films on vertical faces of peds; 3 percent fine prominent black (10YR 2/1) iron-manganese masses with sharp boundaries in matrix; 5 percent medium prominent bluish gray (5PB 5/1) iron depletions with clear boundaries in matrix; 10 percent medium prominent strong brown (7.5YR 5/6) iron-manganese masses with diffuse boundaries in matrix; 20 percent coarse prominent strong brown (7.5YR 4/6) iron-manganese masses with clear boundaries in matrix; 1 percent fine white (5Y 8/1) gypsum crystals; 2 percent fine white (5Y 8/1)salt masses; EC is 11.2 dS/m; SAR is 68; slightly alkaline.

TYPE LOCATION: Harris County, Texas; from the intersection of U.S. Highway 290 and Katy-Hockley Road; about 3.7 miles south on Katy-Hockley Road to Jack Road; 1.4 miles west on Jack Road to old railroad grade; 2.6 miles south on old railroad grade; 850 feet east in rangeland

USGS topographic quadrangle: Warren Lake
Latitude: 29 degrees, 56 minutes, 59.7 seconds N;
Longitude: 95 degrees, 49 minutes, 42.8 seconds W;

Decimal Degrees:
Std Latitude: 29.9499167
Std Longitude: -95.8285556
Datum: WGS 84

RANGE IN CHARACTERISTICS:
Soil Moisture: An udic soil moisture regime. The soil moisture control section is not dry in some or all parts for less than 90 cumulative days in normal years.

Mean annual soil temperature: 21.7 to 22 degrees C (71 to 72 degrees F)

Depth to salt accumulations: 13 to 20 cm (5 to 8 in)
Depth to natric horizon: 15 to 30 cm (6 to 12 in)
Particle-size control section (weighted average)
Clay content: 15 to 18 percent
CEC/clay ratio: 0.60 to 0.70

A Horizon
Hue: 10YR
Value: 4 or 5
Chroma: 2 or 3
Texture: very fine sandy loam, fine sandy loam, or loam
Clay content: 3 to 13 percent
Redox concentrations: amount-2 to 8 percent, shades-brown
EC (dS/m): 6 to 18
Sodium Adsorption Ratio: 4 to 50
Reaction: moderately acid to slightly alkaline

Btnz Horizon
Hue: 10YR
Value: 4 to 6
Chroma: 1 or 2
Texture: very fine sandy loam, fine sandy loam, or loam
Clay content: 10 to 25 percent
Redox concentrations: amount-8 to 20 percent, shades-brown or yellow
Redox depletions: amount-0 to 2 percent, size-, shades-gray
EC (dS/m): 6 to 65
Sodium Adsorption Ratio: 20 to 50
Reaction: moderately acid to slightly alkaline

Btnzy Horizon (upper part)
Hue: 10YR or 2.5Y
Value: 5 to 7
Chroma: 1 or 2
Texture: fine sandy loam, loam, sandy clay loam, or clay loam
Clay content: 13 to 28 percent
Redox concentrations: amount-8 to 20 percent, shades-brown or yellow
Redox depletions: amount-0 to 2 percent, size-, shades-gray
Iron-manganese concentrations: amount-0 to 5 percent, shades-black
Gypsum: 1 to 3 percent
EC (dS/m): 7 to 25
Sodium Adsorption Ratio: 15 to 60
Reaction: slightly alkaline or moderately alkaline

Btnzy Horizon (lower part)
Hue: 10YR or 2.5Y
Value: 5 to 7
Chroma: 1 or 2
Texture: loam, sandy clay loam, or clay loam
Clay content: 8 to 33 percent
Redox concentrations: amount-8 to 20 percent, shades-brown or yellow
Redox depletions: amount-0 to 2 percent, size-, shades-gray
Iron-manganese concentrations: amount-0 to 5 percent, shades-black
Gypsum: 0 to 2 percent
EC (dS/m): 6 to 20
Sodium Adsorption Ratio: 30 to 45
Reaction: slightly alkaline or moderately alkaline

COMPETING SERIES: There are no series in the same family. Similar soils are the Addicks, Clodine, Magotha, and Sauz series.
Addicks soils: do not have a natric horizon; have a mollic epipedon
Clodine soils: do not have a natric horizon
Magotha soils: in a thermic soil temperature regime; have higher electrical conductivity values at the surface
Sauz soils: have a mixed mineralogy; have an active CEC to clay class

GEOGRAPHIC SETTING: Parent material: fluviomarine deposits of the Lissie Formation
Landscape: coastal plains
Landform: slight depression
Slope: 0 to 1 percent
Mean annual precipitation range: 1016 to 1245 mm (40 to 49 in)
Precipitation Pattern: Rainfall is fairly uniform throughout the year. Slight peaks occur in May through June and in September through November. March is typically the driest month.
Thornthwaite annual P-E indices: 62 to 68
Mean annual air temperature range: 20 to 21 degrees C (68 to 70 degrees F)
Frost-free period: 270 to 300 days
Elevation: 38 to 53 m (125 to 175 ft)

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Clodine, Garwood (TX), Katy (TX), and Cyfair (TX) (T) and Prairieview (TX) (T) series.
Clodine soils: do not have salt crystals and are on a similar landform
Garwood soils: have a clayey argillic horizon; on rises on the coastal plains
Katy soils: are moderately well drained; more than 18 percent clay in the argillic horizon; on rises on the coastal plains
Cyfair and Prairieview soils: more than 18 percent clay in the argillic horizon; on rises on the coastal plains

DRAINAGE AND PERMEABILITY:
Drainage class: Somewhat poorly drained
Permeability class: slow
Runoff: negligible
These soils are saturated with aquic conditions from 15 to 46 cm (6 to 18 in) for periods up to two weeks during the months of December to March.

USE AND VEGETATION: Used for rangeland. Native vegetation consists of rushes, sedges, and salt tolerant plants. (Salty Prairie range site, R150AY540TX).

DISTRIBUTION AND EXTENT:
General area: Coastal Prairie of Texas
Land Resource Region: T (Atlantic and Gulf Coast Lowland Forest and Crop Region)
Major Land Resource Area: 150A (Gulf Coast Prairies)
Extent: The series is of small extent

SOIL SURVEY REGIONAL OFFICE (SSRO) RESPONSIBLE: Temple, Texas

SERIES ESTABLISHED: Harris County, Texas, 2019.

REMARKS:
The series was formerly included in the Gessner series. The series was separated based on taxonomy. Gessner soils do not have a natric horizon.

Diagnostic horizons and features recognized in this pedon are:

Particle size control section: 29 to 79 cm (11 to 31 in) (Btnz, Btnzy1, and Btnzy2 horizon)

Ochric epipedon: 0 to 29 cm (0 to 11 in. (A1 and A2 horizons)

Natric horizon: 29 to 203 cm (11 to 80 in) (Btnz, Btnzy1, Btnzy2, Btnzy3, and Btnyg horizons)

Aquic conditions: 15 to 46 cm (6 to 18 in) (Btnz, Btnzy1

Additional Comments:
The assignment of the cation-exchange activity class is supported by laboratory data number S06TX201-001 from Harris County, Texas.

ADDITIONAL DATA:
TAMU Characterization Data from type location S06TX201-001 and from a similar site, S06TX201-002, from Harris County, Texas.

Taxonomic Version: Keys to Soil Taxonomy, Twelfth Edition, 2014.


National Cooperative Soil Survey
U.S.A.