LOCATION LIPSCOMB                OK+TX

Established Series
SLM-JTM
06/2019

LIPSCOMB SERIES


The Lipscomb series consists of very deep, well drained, moderately permeable soils that formed in sandy eolian deposits derived from the Laverne Member, Ogallala Formation of Miocene-Pliocene age. These nearly level to moderately sloping soils occur on undulating to rolling dunes and sandsheets emplaced over hillslopes. Slope ranges from 0 to 8 percent. Mean annual precipitation is about 584 mm (23 in) and mean annual air temperature is about 14.4 degrees C (58 degrees F).

TAXONOMIC CLASS: Coarse-loamy, mixed, superactive, thermic Aridic Haplustalfs

TYPICAL PEDON: Lipscomb sandy loam--on a 2 percent convex slope in improved pasture at approximately 721 m (2365 ft) elevation.
(Colors are for dry soil unless otherwise stated.)

Ap--0 to 10 cm (0 to 4 in); brown (7.5YR 4/3), dark brown (7.5YR 3/3), moist; loamy sand; weak medium subangular blocky parting to moderate medium granular structure; slightly hard, very friable; noneffervescent; moderately acid (pH 5.8); clear smooth boundary. Thickness is 9 to 32 cm (3 to 13 in)

Bt1--10 to 41 cm (4 to 16 in); brown (7.5YR 4/4), dark brown (7.5YR 3/4), moist; sandy loam; moderate medium subangular blocky parting to moderate fine subangular blocky structure; slightly hard, very friable; few distinct clay films on all faces of peds; noneffervescent; moderately acid (pH 6.0); gradual smooth boundary. Thickness of the upper Bt is 18 to 119 cm (7 to 47 in)

Bt2--41 to 100 cm (16 to 39 in); brown (7.5YR 5/4), brown (7.5YR 4/4), moist; sandy loam; moderate medium subangular blocky parting to moderate fine subangular blocky structure; slightly hard, very friable; few faint clay films on all faces of peds; noneffervescent; slightly acid (pH 6.2); clear smooth boundary. Thickness of the lower Bt horizons is 15 to 124 cm (6 to 49 in). Combined thickness of the Bt horizons is 19 to 160 cm (8 to 63 in)

BC--100 to 149 cm (39 to 59 in); strong brown (7.5YR 5/6), strong brown (7.5YR 4/6), moist; loamy sand; weak medium subangular blocky structure; slightly hard, very friable; noneffervescent; neutral (pH 6.6); clear smooth boundary. Thickness of the BC horizons 26 to 71 cm (10 to 28 in)

C1--149 to 173 cm (59 to 68 in); reddish yellow (7.5YR 7/6), reddish yellow (7.5YR 6/6), moist; sand; structureless massive; slightly hard, loose; noneffervescent; neutral (pH 6.8); clear smooth boundary.

C2--173 to 203 cm (68 to 80 inches); reddish yellow (7.5YR 8/6), reddish yellow (7.5YR 7/6), moist; fine sand; structureless single grain; slightly hard, loose; noneffervescent; neutral (pH 6.9).

TYPE LOCATION:
Roger Mills County, Oklahoma; From the intersection of Highway 283 and Highway 33 north of Roll, OK; 3.5 miles west on Highway 33, then 0.6 miles north on NS 1800, then 0.3 miles west on EW 0830; 1650 ft (503 m) west and 1100 ft (335 m) north of the southeast corner of Section 31, Township 16N, Range 24W (Indian meridian).

USGS topographic quadrangle: Crawford, Oklahoma
Latitude: 35 degrees 48 minutes 55.20 seconds N
Longitude: 99 degrees 47 minutes 19.15 seconds W
Datum WGS84

Decimal Degrees
Latitude: 35.8153337
Longitude: -99.7886526

UTM Northing: 3963753
UTM Easting: 428755
UTM zone 14S

RANGE IN CHARACTERISTICS:
Soil moisture: An ustic moisture regime bordering on aridic. The soil moisture control section is dry in some or all parts for more than 180 but less than 220 days, cumulative, in normal years.
Thickness of ochric epipedon: 9 to 32 cm (3 to 13 in)
Thickness of the argillic horizon: 15 to 190 cm (6 to 75 in)
Depth to buried horizons (where present): 55 to 131 cm (22 to 52 in)
Depth to secondary carbonates (where present): more than 48 cm (19 in)

Particle-size control section (weighted average):
Total clay content: 9 to 18 percent
Silicate clay content: 9 to 18 percent
Total sand content: 52 to 75 percent
Rock fragments: 0 to 3 percent as subrounded to well-rounded indurated quartzite gravels

A or Ap horizons:
Hue: 7.5YR, 10YR
Value: 4 to 5, 2 to 4 moist
Chroma: 2 to 4 moist or dry
Texture: loamy fine sand, loamy sand, sandy loam, fine sandy loam
Total clay content: 2 to 15 percent
Total sand content: 55 to 87 percent
Effervescence: none
Reaction (pH): strongly acid to slightly acid (5.1-6.5)

Upper Bt horizons:
Hue: 5YR to 10YR
Value: 4 to 6, 3 to 5 moist
Chroma: 2 to 6 moist or dry
Texture: sandy loam, fine sandy loam
Total clay content: 9 to 18 percent
Total sand content: 52 to 75 percent
Rock fragments: 0 to 3 percent; fine gravel; rounded or subrounded indurated quartzite
Effervescence: none
Reaction (pH): strongly acid to slightly acid (5.1-6.5)

Lower Bt and/or BC horizons:
Hue: 5YR to 10YR
Value: 4 to 7, 3 to 6 moist
Chroma: 2 to 6 moist or dry
Texture: sandy loam, fine sandy loam, loamy sand, or loamy fine sand
Total clay content: 5 to 18 percent
Total sand content: 55 to 87 percent
Rock fragments: 0 to 5 percent; fine gravel; rounded or subrounded indurated quartzite
Effervescence: none
Reaction (pH): moderately acid to neutral (5.6-7.3)

C horizons (where present):
Thickness when present: 20 to 109 cm (8 to 43 in)
Hue: 7.5YR, 10YR
Value: 5 to 7, 4 to 6 moist
Chroma: 3 to 6 moist or dry
Texture: sand, fine sand, loamy fine sand, loamy sand, sandy loam, or fine sandy loam
Total clay content: 1 to 12 percent
Total sand content: 65 to 95 percent
Rock fragments: 0 to 5 percent; fine gravel; rounded or subrounded indurated quartzite
Calcium carbonate equivalent: 0 to 5 percent
Effervescence: none to slight
Reaction (pH): slightly acid to slightly alkaline neutral (6.1-7.8)

Btb, Btkb, 2Bk, 2Bt, and 2Btk horizons (where present):
Hue: 5YR to 10YR
Value: 4 to 7, 3 to 6 moist
Chroma: 2 to 6 moist or dry
Texture: loamy sand, fine sandy loam, sandy loam, loam, or sandy clay loam
Rock fragments: 0 to 10 percent; fine and medium gravel; rounded or subrounded indurated quartzite
Identifiable secondary carbonate: 0 to 10 percent; masses and nodules
Calcium carbonate equivalent: 0 to 5 percent
Effervescence: none to slight
Reaction (pH): slightly acid to slightly alkaline (6.1-7.8)

COMPETING SERIES:
This is the Spantara series in the same family. Similar soils are the Devol, Fortyone, and Springer series.
Spantara soils: formed in eolian and alluvial sediments in the Blackwater Draw formation and occur in a slightly drier climate
Devol and Springer soils: occur on terraces at lower elevation
Fortyone soils: formed in loamy and sandy alluvium and have 2 to 15 percent rounded gravels throughout the solum

GEOGRAPHIC SETTING:
Parent Material: loamy and sandy eolian sediments derived from the Laverne Member of the Ogallala Formation of Miocene-Pliocene age.
Landscape: Dissected high plains
Landform: summit, shoulder, and backslopes of undulating to rolling dunes and sandsheets emplaced over hillslopes of the Laverne Member, Ogallala Formation
Slope: 0 to 8 percent
Precipitation Pattern: These soils are intermittently moist in September through November and March through June. July through August and December through February are the driest months.
Mean annual precipitation: 508 to 660 mm (20 to 26 in)
Thornthwaite annual P-E Index: 34 to 40
Mean annual air temperature: 13.3 to 15.0 degrees C (56 to 59 degrees F)
Frost-free period: 180 to 210 days
Elevation: 609.6 to 914.4 m (2,000 to 3,000 ft)

GEOGRAPHICALLY ASSOCIATED SOILS:
These are the Abbie, Ady, Dreyfoos, Texroy, and Vici soils.
Abbie and Texroy soils: occur on similar landscape positions, have a mollic epipedon and a fine-loamy argillic horizon
Ady soils: occur on similar landscape positions and have a fine-loamy argillic horizon
Dreyfoos soils: occur on larger dune landforms and do not have a diagnostic argillic horizon
Vici soils: occur on slightly higher landscape positions and have a sandy argillic horizon

DRAINAGE AND PERMEABILITY:
Drainage class: well drained
Permeability class: moderately rapid
Runoff: negligible on 0 to 1 percent slopes, very low on 1 to 5 percent slopes, and low on 5 to 8 percent slopes

USE AND VEGETATION:
Major uses: Crop production and livestock grazing
Native vegetation: Predominantly little bluestem, sideoats grama, Indiangrass, and sand bluestem with smaller amounts of switchgrass, blue grama, and purple threeawn. Sand Sagebrush and Chickasaw sandplum are the major woody species, with lesser amounts of yucca.
Ecological sites assigned to phases and components of this series are listed below. Current ecological site assignments are in Web Soil Survey. Components of this series include the following ecological sites: Sandy Loam (R077EY066TX)

DISTRIBUTION AND EXTENT:
General area: Northwestern Oklahoma and the Texas and Oklahoma Panhandles
Land Resource Region: H - Central Great Plains Winter Wheat and Range Region
MLRA 77E - Southern High Plains, Breaks
Extent: Moderate

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

SERIES ESTABLISHED: Roger Mills County, OK 2019. The name of the series is from Lipscomb County, Texas.

REMARKS:
These soils were formerly included in the Devol and Springer series.

Diagnostic horizons and features in this pedon are:
Particle-size control section: 10 to 60 cm (4 to 24 in) (Bt1 and Bt2 horizons)
Ochric epipedon: 0 to 10 cm (0 to 4 in) (Ap horizon)
Argillic horizon: 10 to 100 cm (4 to 39 in) (Bt1 and Bt2 horizons)

ADDITIONAL DATA: none available

TAXONOMIC VERSION: Keys to Soil Taxonomy, Twelfth Edition, 2014.


National Cooperative Soil Survey
U.S.A.