LOCATION ESTES              TX
Established Series
Rev. CLN-MLG-KLG
11/2009

ESTES SERIES


The Estes series consists of very deep, somewhat poorly drained soils. These nearly level floodplain soils formed in acid clayey and loamy alluvium in the Coastal Plains. Slope ranges from 0 to 1 percent. Mean annual air temperature is about 18 degrees C (65 degrees F); mean annual precipitation is about 1168 mm (46 in).

TAXONOMIC CLASS: Fine, smectitic, thermic Aeric Dystraquerts

TYPICAL PEDON: Estes clay, in floodplain, elevation is 64 m (210 ft) (Elevation estimated from topographic software, following location directions below). (Colors are for moist soil unless otherwise stated.)

A--0 to 10 cm (0 to 4 in); brown (10YR 4/3) clay; moderate fine and medium subangular blocky structure; very hard, firm; many fine, medium and coarse roots; extremely acid; clear wavy boundary.? (Thickness is 8 to 23 cm [3 to 9 in].)

Bw--10 to 30 cm (in); pale brown (10YR 6/3) clay; moderate fine and medium subangular blocky structure; very hard, firm; common fine and medium roots; few fine and medium pores; few pressure surfaces; many fine and medium prominent yellowish red (5YR 5/6) masses of iron accumulation; extremely acid; clear smooth boundary. (Thickness is 0 to 38 cm [0 to 15 in].)

Bg--30 to 97 cm (in); light brownish gray (10YR 6/2) clay; weak medium and coarse subangular blocky structure; very hard, very firm; few fine and medium roots; few fine pores; few pressure surfaces and slickensides; few lenses of light gray sand on vertical surfaces of peds; common fine and medium prominent yellowish red (5YR 5/8) masses of iron accumulation; extremely acid; gradual smooth boundary. (Thickness is 20 to 89 cm [8 to 35 in].)

Bssg--97 to 165 cm (in); light brownish gray (10YR 6/2) clay; weak coarse angular blocky structure; very hard, very firm; few fine roots; common fine pores; few pressure surfaces and common prominent slickensides; many medium distinct strong brown (7.5YR 5/8) and yellowish brown (10YR 5/8) and common coarse prominent red (2.5YR 4/6) masses of iron accumulation; extremely acid; gradual smooth boundary. (Thickness is 51 to 102 cm [20 to 60 in].)

BCg--165 to 203 cm (in); light brownish gray (10YR 6/2) clay loam; weak coarse subangular blocky structure; very hard, firm; few fine roots; few pressure surfaces; common medium distinct brownish yellow (10YR 6/6) and many coarse prominent red (2.5YR 4/6) masses of iron accumulation; extremely acid.

TYPE LOCATION: Harrison County, Texas; from U.S. Highway 80 in Marshall, 15.7 miles south on U.S. Highway 59; 100 feet east of fence in woodland (Site is also 0.4 mile north of Sabine River bridge). (Latitude: 32 degrees, 20 minutes, 6.18 seconds N; Longitude: 94 degrees, 21 minutes, 9.55 seconds W. (Coordinates estimated from location directions and topographic software) Grand Bluff, TX TOPOGRAPHIC QUADRANGLE; NAD 83).

RANGE IN CHARACTERISTICS:

Soil Moisture: An udic soil moisture regime. The soil moisture control section is moist in some or all parts for more than 210 days in normal years.

Mean annual soil temperature: 19 to 21 degrees C (66 to 70 degrees F)
Depth to cambic horizon: 8 to 23 cm (3 to 9 in), where present
Depth to redox concentrations: 8 to 23 cm (3 to 9 in)
Depth to episaturation: 0 to 46 cm (0 to 18 in)
Vertic features: 46 to 200 cm (18 to 80 in)

Particle-size control section (weighted average):
Clay content: 40 to 50 percent

A Horizon
Hue: 10YR
Value: 3 to 5
Chroma: 2 or 3
Texture: clay, clay loam, or silty clay loam
Clay content: 28 to 59 percent
Redox concentrations: none to common, shades of brown
Redox depletions: none to common, shades of gray
Iron-manganese concentrations: none to common, soft masses
EC (dS/m): ranges from 0 to 4, typically less than 1
SAR: 1 to 5
Reaction: extremely acid to moderately acid (3.6 to 6.0)

Bw Horizon (where present)
Hue: 10YR
Value: 4 to 6
Chroma: 3 or 4
Texture: clay or silty clay
Clay content: 40 to 60 percent
Redox concentrations: few to many, shades of brown
Redox depletions: few to many, shades of gray
Iron-manganese concentrations: none to common, soft masses
EC (dS/m): ranges from 0 to 4, typically less than 1
SAR: 1 to 5
Reaction: extremely acid to strongly acid (3.6 to 5.5)

Bg Horizon
Hue: 10YR
Value: 4 to 6
Chroma: 1 or 2
Texture: clay or silty clay
Clay content: 40 to 60 percent
Redox concentrations: few to many, shades of brown, red and yellow
Redox depletions: few to many, shades of gray
Iron-manganese concentrations: none to many, soft masses
EC (dS/m): ranges from 0 to 4, typically less than 1
SAR: 1 to 5
Reaction: extremely acid to strongly acid (3.6 to 5.5)

Bssg Horizon
Hue: 10YR or 2.5Y
Value: 4 to 7
Chroma: 1 or 2
Texture: clay or silty clay
Clay content: 40 to 60 percent
Redox concentrations: few to many, shades of brown, red and yellow
Redox depletions: few to many, shades of gray
Iron-manganese concentrations: none to many, soft masses
EC (dS/m): ranges from 0 to 4, typically less than 1
SAR: 1 to 5
Reaction: extremely acid or very strongly acid (3.6 to 5.0)

BCg Horizon (where present)
Hue: 10YR or 2.5Y
Value: 6 or 7
Chroma: 1 or 2
Texture: sandy clay loam, silty clay loam or clay loam
Clay content: 25 to 39 percent
Redox concentrations: few to many, shades of brown, red and yellow
EC (dS/m): ranges from 0 to 4, typically less than 1
SAR: 1 to 5
Reaction: extremely acid to moderately acid (3.6 to 6.0)

COMPETING SERIES: This is the Ozias series. Similar soils are the Gladewater, Kobel, Leeper, Litro, Overton, Tamba, Tuscumbia, Una and Urbo series.
Ozias soils: have electrical conductivity of more than 4 dS/m within a depth of 102 cm (40 inches)
Gladewater soils: have a pH value of more than 5.0 throughout the upper 20 inches
Kobel soils: are members of a Vertic subgroup
Leeper soils: are members of a Vertic subgroup
Litro soils: have mixed mineralogy
Overton soils: are calcareous
Tamba soils: have mixed mineralogy
Tuscumbia soils: are members of a Vertic subgroup
Una soils: have mixed mineralogy
Urbo soils: have mixed mineralogy

GEOGRAPHIC SETTING:
Parent material: clayey and loamy alluvium derived from the Coastal Plains
Landscape: Coastal Plain
Landform: floodplain
Slope: 0 to 1 percent
Mean annual air temperature range: 18 to 20 degrees C (64 to 68 degrees F)
Mean annual precipitation range: 1145 to 1400 mm (45 to 55 in)
Frost-free period: 235 to 250 days
Elevation: 61 to 137 m (200 to 450 ft)
Thornthwaite annual P-E indices: exceeds 64

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Alaga(TX), Bienville(TX), Bleakwood(TX), Bruno(TX), Hainesville(TX) Iulus(TX, Laneville(TX), Mantachie(TX), Mathiston(TX), Mooreville(TX), Sardis(TX) and Thenas(TX) series.
Alaga soils: are sandy soils on stream terraces
Bienville soils: are sandy soils on stream terraces
Bleakwood soils: have a fine-loamy particle size control section
Bruno soils: are sandy and are located on point bars and natural levees along major streams
Hainesville soils: are sandy soils on stream terraces
Iulus soils: are coarse-loamy soils on slightly higher positions
Laneville soils: are fine-loamy soils in lateral flood plains
Mantachie soils: are fine-loamy soils in lateral flood plains
Mathiston soils: are fine-silty soils in lateral flood plains
Mooreville soils: are fine-loamy soils in lateral flood plains
Sardis soils: are coarse-loamy soils on slightly higher positions
Thenas soils: are coarse-loamy soils on slightly higher positions

DRAINAGE AND PERMEABILITY: somewhat poorly drained. Runoff is high. Commonly flooded for 2 to 60 days per year. Flooding occurs mainly from November to May and ranges from a few up to about 900 mm (a few up to about 36 inches) in depth.

USE AND VEGETATION: Used primarily for woodland and/or wildlife. A few areas are used for improved pastures of bahiagrass, fescue or dallisgrass. Native vegetation consists of a mixed hardwood forest. The major commercial trees are water oak, willow oak and sweetgum. Other vegetation includes a few scattered green ash, elm, hackberry, mulberry, hickory, pecan and widely scattered native pine with an understory of grasses and shrubs.

DISTRIBUTION AND EXTENT: Eastern Texas and western Louisiana,; Land Resource Region (P); MLRA 133B and some MLRA 150; the series is of large extent.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Temple, Texas

SERIES ESTABLISHED: Harrison County, Texas, 1984, Harrison County soil survey area, Texas, 1989.

REMARKS: The soil was formerly included with the Urbo series.

DIAGNOSTIC HORIZONS AND FEATURES recognized in this pedon are:

Particle size control section: 25 to 100 cm (10 to 40 in). (Bw, Bg and Bssg horizons)
Ochric epipedon: 0 to 10 cm (0 to 4 in) (A horizon)
Aeric feature: 10 to 30 cm (4 to 12 in) (Bw horizon)
Aquic conditions: 30 to 203 cm (12 to 80 in) (Bg, Bssg and BCg horizons)
Redoximorphic concentrations: 10 to 203 cm (4 to 80 in). (Bw, Bg, Bssg and BCg horizons)
Vertic features: The presence of slickensides at 97 to 165 cm (38 to 65 in). (Bssg horizon)
Episaturation: The zone of saturation at 30 to 203 cm (12 to 80 in). (Bg, Bssg and BCg horizons)
Aquic conditions: 30 to 203 cm (12 to 80 in)

ADDITIONAL DATA: NSSL data from 5 pedons:
Gregg Co 81TX183001; Harrison Co 82TX203001; Newton Co 82TX351001; Panola Co 82TX365001; Titus Co 81TX449001
SOIL INTERPRETATION RECORD NUMBER: TX1063 and TX1265

TAXONOMIC VERSION: Keys to Soil Taxonomy, Tenth Edition, 2006


National Cooperative Soil Survey
U.S.A.