LOCATION RAISIN             TX
Established Series
JAD-JKW-JAG
02/2010

RAISIN SERIES


The Raisin series consists of very deep, well drained soils that formed in loamy alluvium of Quaternary age. These nearly level to gently sloping soils are on high stream terraces. Slope ranges from 1 to 5 percent. Mean annual precipitation is about 965 mm (38 in) and the mean annual air temperature is about 21 degrees C (70 degrees F).

TAXONOMIC CLASS: Fine-loamy, mixed, superactive, hyperthermic Typic Haplustalfs

TYPICAL PEDON: Raisin loamy fine sand, on west-facing, convex, 1 percent slope in rangeland at an elevation of 68 m (225 ft) (Colors are for dry soil unless otherwise stated.)

A--0 to 12 cm (0 to 5 in); grayish brown (10YR 5/2) loamy fine sand, dark grayish brown (10YR 4/2),moist; single grain; loose, loose; common fine roots and many very fine roots; common fine interstitial and common medium interstitial pores; slightly acid; clear smooth boundary. (10 to 28 cm [4 to 11 in] thick)

E--12 to 48 cm (5 to 19 in); light brownish gray (10YR 6/2) loamy fine sand, dark grayish brown (10YR 4/2), moist; single grain; very friable, soft; many very fine roots; common fine tubular and common very fine tubular pores; 1 percent fine distinct dark yellowish brown (10YR 4/6) masses of oxidized iron with sharp boundaries lining pores; slightly acid; abrupt smooth boundary. (0 to 38 cm [0 to 15 in] thick)

Bt1--48 to 64 cm (19 to 25 in); dark grayish brown (10YR 4/2) sandy clay loam, very dark grayish brown (10YR 3/2), moist; moderate medium prismatic structure parting to moderate fine and medium angular blocky; firm, hard; many very fine roots; common fine tubular and common very fine tubular pores; 5 percent prominent pale brown (10YR 6/3) sand coats on vertical faces of peds; 10 percent prominent black (10YR 2/1) organic stains on all faces of peds; 20 percent prominent very dark gray (10YR 3/1) clay films on all faces of peds; 2 percent fine distinct light brownish gray (10YR 6/2) iron depletions with sharp boundaries in matrix surrounding redox concentrations; 2 percent fine and medium prominent yellowish red (5YR 5/8) masses of oxidized iron with sharp boundaries in matrix; 4 percent fine and medium prominent brownish yellow (10YR 6/8) masses of oxidized iron with sharp boundaries in matrix surrounding redox concentrations; slightly acid; gradual wavy boundary.

Bt2--64 to 89 cm (25 to 35 in); light gray (10YR 7/2) sandy clay loam, light brownish gray (10YR 6/2), moist; strong medium prismatic structure parting to strong medium angular blocky; firm, hard; common very fine roots; common very fine tubular pores; 5 percent prominent pale brown (10YR 6/3) sand coats on vertical faces of peds; 7 percent prominent very dark grayish brown (10YR 3/2) organic stains on all faces of peds; 25 percent prominent grayish brown (10YR 5/2) clay films on all faces of peds; 3 percent medium prominent yellowish red (5YR 5/8) masses of oxidized iron with sharp boundaries in matrix; 4 percent medium prominent strong brown (7.5YR 5/8) masses of oxidized iron with sharp boundaries in matrix surrounding redox concentrations; 5 percent medium and coarse prominent brownish yellow (10YR 6/8) masses of oxidized iron with sharp boundaries in matrix surrounding redox concentrations; slightly acid; gradual wavy boundary.

Bt3--89 to 117 cm (35 to 46 in); light gray (2.5Y 7/2) sandy clay loam, light brownish gray (2.5Y 6/2), moist; strong medium prismatic structure parting to strong medium angular blocky; firm, hard; common very fine roots between peds; common very fine tubular pores; 3 percent prominent pale brown (10YR 6/3) sand coats on vertical faces of peds; 10 percent prominent very dark grayish brown (10YR 3/2) organic stains on all faces of peds; 30 percent prominent light brownish gray (10YR 6/2) clay films on all faces of peds; 5 percent medium prominent red (2.5YR 4/6) masses of oxidized iron with sharp boundaries in matrix; 8 percent medium and coarse prominent strong brown (7.5YR 5/6) masses of oxidized iron with sharp boundaries in matrix surrounding redox concentrations; slightly acid; gradual wavy boundary.

Bt4--117 to 138 cm (46 to 54 in); 50 percent pale brown (10YR 6/3) and 40 percent yellowish red (5YR 5/6)sandy clay loam, 50 percent light brownish gray (10YR 6/2) and 40 percent yellowish red (5YR 5/6), moist; strong medium prismatic structure parting to moderate medium and coarse angular blocky; firm, hard; common very fine roots between peds; common very fine tubular pores; 3 percent prominent dark grayish brown (10YR 4/2) organic stains on all faces of peds and 5 percent prominent pale brown (10YR 6/3) sand coats on vertical faces of peds; 25 percent prominent light brownish gray (10YR 6/2) clay films on all faces of peds; 3 percent fine and medium prominent red (2.5YR 4/6) masses of oxidized iron with sharp boundaries in matrix; neutral; gradual wavy boundary.

Bt5--138 to 171 cm (54 to 67 in); yellowish red (5YR 5/6) sandy clay loam, strong brown (7.5YR 5/6), moist; moderate coarse prismatic structure parting to moderate coarse angular blocky; firm, slightly hard; common very fine roots between peds; common very fine tubular pores; 3 percent prominent dark grayish brown (10YR 4/2) organic stains on all faces of peds; 5 percent prominent pale brown (10YR 6/3) sand coats on vertical faces of peds; 20 percent prominent brown (7.5YR 5/3) clay films on all faces of peds; neutral; clear smooth boundary. (Combined thickness of the Bt horizons is 155 to 193 cm [61 to 76 in])

Btk--171 to 203 cm (67 to 80 in); brown (7.5YR 5/4) loam, brown (7.5YR 4/4), moist; weak coarse subangular blocky structure; friable, slightly hard; common very fine roots between peds; few very fine tubular pores; 2 percent distinct dark grayish brown (10YR 4/2) organic stains on vertical faces of peds; 10 percent distinct brown (7.5YR 4/4) clay films on vertical faces of peds; 8 percent fine and medium carbonate nodules; 12 percent medium and coarse carbonate masses; moderately alkaline.

TYPE LOCATION: Goliad County, Texas; from the intersection of US Highway 59 and FM 883 in Berclair; 1.57 miles northeast on US Highway 59 to ranch road; 0.4 mile north and 0.4 mile west on ranch road; 350 feet north in rangeland; Berclair USGS quad; Latitude: 28 degrees 32 minutes 43.80 seconds N; Longitude: 97 degrees 34 minutes 47.90 seconds W NAD 83.

RANGE IN CHARACTERISTICS:
Solum thickness is more than 80 inches.
Soil Moisture: An ustic soil moisture regime. The soil moisture control section, 4 to 12 inches, is dry in some or all parts for more than 90 but less than 180 cumulative days in normal years. July through September, December, and March are the driest months.

Mean annual soil temperature: 22 to 23.5 degrees C (72 to 74 degrees F)
Depth to argillic horizon: 10 to 19 cm (4 to 19 in).

Particle-size control section (weighted average)
Clay content: 27 to 35 percent
CEC to clay: 0.6 to 1.5

A Horizon
Hue: 10YR
Value: 4 or 5
Chroma: 2 or 3
Texture: fine sandy loam, loamy fine sand, or loamy sand
Clay content: 3 to 12 percent
Reaction: moderately acid to neutral

E Horizon
(where present)
Hue: 10YR
Value: 5 to 7
Chroma: 2 or 3
Texture: fine sandy loam, loamy fine sand, or loamy sand
Clay content: 3 to 12 percent
Reaction: moderately acid to neutral

Bt Horizon
(Upper Bt Horizons)
Hue: 10YR
Value: 4 to 7
Chroma: 2
Texture: sandy clay loam, or sandy clay
Clay content: 30 to 38 percent
Iron concentrations: amount-2 to 5, size-fine, shades-brown or red,
Iron depletions: amount-0 to 2, size-fine or medium, shades-gray
Reaction: moderately acid to neutral

Bt Horizon
(lower Bt Horizons)
Hue: 5YR to 10YR
Value: 4 to 6
Chroma: 4 to 6
Texture: sandy clay loam
Clay content: 22 to 30 percent
Iron concentrations: amount-2 to 15, size-fine, shades-yellow, brown or red,
Iron depletions: amount-0 to 2, size-fine or medium, shades-gray
Reaction: slightly acid to slightly alkaline

Btk Horizon
(where present)
Hue: 5YR to 10YR
Value: 4 to 6
Chroma: 4 to 6
Texture: fine sandy loam, loam, or sandy clay loam
Clay content: 18 to 28 percent
Iron concentrations: amount-2 to 15, size-fine, shades-yellow, brown or red,
Iron depletions: amount-0 to 2, size-fine or medium, shades-gray
Calcium carbonate equivalent: 5 to 45 percent
Identifiable secondary carbonate: amount-0 to 15 percent, kind-masses or nodules
Effervescence: none to slight
Reaction: slightly alkaline or moderately alkaline

COMPETING SERIES: This the Premont series in the same family. Similar soils are the Grandfield (OK), Honeycreek (TX), Hye (TX), Inari (TX), Papalote (TX), Rochelle, Runge (TX), and Seagraves series.
Grandfield, Honeycreek, Hye, Rochelle, and Seagraves soils: These soils have a surface horizon redder than 10YR and are in the thermic soil temperature regime.
Papalote soils: These soils have a fine particle-size control section.
Inari and Runge soils: These soils have a mollic epipedon.

GEOGRAPHIC SETTING:
Parent material: loamy alluvium of Quaternary age
Landscape: inland dissected coastal plain
Landform: high stream terraces
Slope: 1 to 5 percent
Mean annual air temperature: 21 to 24 degrees C (70 to 74 degrees F)
Mean annual precipitation: 652 to 918 mm (26 to 36 in)
Precipitation Pattern: The majority of the yearly amount occurs during the fall and spring months. The summer months are normally dry with infrequent coastal showers. The late summer months are subject to periods of high intense rainfall as a result of tropical disturbances.
Frost-free period: 260 to 340 days
Elevation: 30.5 to 91 m (100 to 300 ft)
Thornthwaite annual P-E indices: 40 to 46

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Ander (TX) Papalote (TX), Weesatche (TX) series.
Ander soils: These soils have a fine particle-size argillic horizon, a mollic epipedon, and are on a similar landform.
Papalote soils: These soils have a fine particle-size argillic horizon and are on a similar landform.
Weesatche soils: These soils have a mollic epipedon and are on a hill backslope.

DRAINAGE AND PERMEABILITY: Well drained. moderate permeability. Runoff is negligible on slopes less than 1 percent and low on slopes from 1 to 5 percent.

USE AND VEGETATION: Used mainly as rangeland and wildlife habitat. The vegetation is live oak, post oak, bluestems, gramas, and threeawns. Mesquite and huisache have encroached in some areas. The ecological site for phases with a sandy surface layer is loamy sand 25 to 35 inch PZ (R083AY396TX ) and Sandy Loam 25 to 35 inch PZ (R083AY407TX) for loamy surface phases.

DISTRIBUTION AND EXTENT: South Central Texas; MLRA 83A; LRR I; moderate extent

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

SERIES ESTABLISHED: Goliad County, Texas 2009. The name is for a community in Victoria County.

REMARKS: These soils were formerly included in the Delfina series. The Delfina series has aquic conditions and the series province is confined to MLRA 83D in the lower Rio Grande valley. The redoximorphic features in the argillic horizon are not contemporary. These soils are in association with other soils that have borderline siliceous/mixed mineralogy.

Diagnostic horizons and features recognized in this pedon are:
Particle size control section: 48 to 98 cm (19 to 39 in) (Bt1 and Bt2 horizons)
Ochric epipedon: 0 to 48 cm (0 to 19 in) (A and E horizons)
Argillic horizon: 48 to 203 cm (19 to 80 in) (Bt1, Bt2, Bt3, Bt5, Bt5, Btk horizons)
Calcic horizon: 171 to 203 cm (67 to 80 in). (Btk horizon)
Redoximorphic concentrations: 12 to 138 cm (5 to 54 in) (Bt horizons)
Abrupt textural change: 47 to 49 cm (19 to 20 in) (Contact between E and Bt1 horizons
The assignment of the cation-exchange activity class is inferred from lab data from Goliad and Refugio Counties.

ADDITIONAL DATA: National Soil Survey Lab data on pedon number 08N0164 from the type location and on pedon number 08N0163 in Goliad County, Texas.

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


National Cooperative Soil Survey
U.S.A.