LOCATION LAZBUDDIE               TX+NM

Established Series
Rev. FBP-WMR-TCB
09/2022

LAZBUDDIE SERIES


The Lazbuddie series consists of very deep, moderately well drained, very slowly permeable soils that formed in calcareous, clayey lacustrine deposits of Quaternary age. These nearly level soils are on playa steps in large playa basins. Slope ranges from 0 to 1 percent. Mean annual precipitation is 483 mm (19 in) and mean annual temperature is 16 degrees C (61 F).

TAXONOMIC CLASS: Fine, smectitic, thermic Calcic Haplusterts

TYPICAL PEDON: Lazbuddie clay, midway on a playa step, slightly concave, 0.4 percent slope in cropland at an elevation of about 1,175 m (3,854 ft). (Colors are for dry soil unless otherwise stated.)

Ap--0 to 10 cm (0 to 3 in); dark grayish brown (10YR 4/2) clay, very dark grayish brown (10YR 3/2) moist; weak fine subangular blocky structure parting to moderate very fine granular structure; hard and firm; very sticky and very plastic; common fine and medium roots throughout; few fine and medium tubular pores; cracks 3 cm wide (1 in) extend through the horizon; strongly effervescent; moderately alkaline; gradual wavy boundary. (6 to 20 cm [2 to 8 in] thick)

Bss1--10 to 34 cm (3 to 13 in); dark grayish brown (10YR 4/2) clay, very dark grayish brown (10YR 3/2) moist; strong coarse wedge-shaped aggregates parting to moderate medium angular blocky structure; very hard and very firm; very sticky and very plastic; common fine and medium roots throughout; common fine and medium tubular pores; common distinct slickensides; few fine nodules of calcium carbonate, about 1 percent; cracks 3 cm (1 inch) wide extend through the horizon; strongly effervescent; moderately alkaline; gradual wavy boundary.

Bss2--34 to 88 cm (13 to 34 in); dark grayish brown (10YR 4/2) clay, very dark grayish brown (10YR 3/2) moist; strong coarse wedge-shaped aggregates parting to moderate medium angular blocky structure; very hard and very firm; very sticky and very plastic; few fine and medium roots throughout; few fine and medium tubular pores; common distinct slickensides; few fine nodules of calcium carbonate, about 1 percent; cracks 2 cm (0.75 inch) wide extend to 75 cm in the horizon; strongly effervescent; moderately alkaline; gradual wavy boundary.

Bss3--88 to 135 cm (34 to 53 in); dark grayish brown (10YR 4/2) clay, very dark grayish brown (10YR 3/2) moist; strong coarse wedge-shaped aggregates parting to moderate medium angular blocky structure; very hard and very firm; very sticky and very plastic; few fine and medium roots throughout; few fine and medium tubular pores; common distinct slickensides; few fine nodules of calcium carbonate, about 1 percent; strongly effervescent; moderately alkaline; gradual wavy boundary. (combined thickness of the Bss horizons is 80 to 140 cm [32 to 55 in] thick)

Bkk--135 to 203 cm (53 to 80 in); pale yellow (2.5Y 8/2) clay, pale yellow (2.5Y 8/3) moist; weak coarse subangular blocky structure; slightly hard and friable; moderately sticky and slightly plastic; few fine and medium roots throughout; few fine tubular pores; about 60 percent calcium carbonate by volume in the form of finely disseminated carbonate and irregular carbonate masses between peds; violently effervescent; strongly alkaline.

TYPE LOCATION: Parmer County, Texas; from the intersection of State Highway 145 and Farm Road 1172 near Lazbuddie, Texas; 14 kilometers (8.7 miles) north on Farm Road 1172; 3.2 kilometers (2 miles) east on county road; 0.3 kilometer (0.2 mile) north on county road; 1 kilometer (0.6 mile) east on county road; 0.5 kilometer (0.3 mile) north into crop field. Latitude - 34 degrees, 30 minutes, 17.2 seconds N; Longitude - 102 degrees, 32 minutes, 34.0 seconds W; Tam Anne, Texas USGS quad; NAD 83.

RANGE IN CHARACTERISTICS:
Soil moisture: An ustic moisture regime bordering on typic. The soil moisture control section is dry in some or all parts for more than 180 but less than 205 cumulative days in normal years. July through August and November through March are the driest months. These soils are intermittently moist in September through October and April through June; however, lower landscape positions result in higher "effective" precipitation.
Mean annual soil temperature: 15 to 18 degrees C (59 to 64 F).
Depth to secondary calcium carbonate: 13 to 100 cm (5 to 40 in).
Depth to calcic horizon: 100 to 150 cm (40 to 60 in).
Depth to slickensides: 6 to 25 cm (2 to 10 in).
Linear extensibility of top 1 meter (40 in): 7 to 10 cm (2.75 to 4 in).
Solum thickness: more than 203 cm (80 in).
Particle-size control section (weighted average): 40 to 60 percent silicate clay.
This is a cyclic soil and undisturbed areas have gilgai microrelief with microhighs 13 to 46 cm (5 to 18 in) higher than microlows. Distance between the center of the microhigh and the center of the microlow is about 1.5 to 6 m (5 to 20 ft). The microhigh makes up about 25 percent, the intermediate area between the high and low about 50 percent, and the microlow about 25 percent. Cracks open and close each year, except during higher than normal rainfall years, and remain open for 150 to 210 cumulative days during most years. When dry, 1.3 to 7.5 cm (0.5 to 3 in) wide cracks extends from the surface to a depth of 100 cm (40 in) or more. Cracks are more prominent in the microlow. The range in characteristics represents 50 percent or more of each pedon unless otherwise stated.

A horizon:
Hue: 10YR or 2.5Y
Value: 5 to 7, 4 to 6 moist
Chroma: 1 or 2
Texture: clay
Visible secondary calcium carbonate: 0 to 2 percent by volume as films, filaments, and nodules
Effervescence: slight to violent
Reaction: moderately alkaline
Thickness of the A horizon varies with microrelief, ranging from 6 to 20 cm (2 to 8 in) thick.

Bw horizon: (where present)
Hue: 10YR or 2.5Y
Value: 6 or 7, 4 to 6 moist
Chroma: 1 or 2
Texture: clay
Secondary calcium carbonate: 0 to 2 percent by volume as films, filaments, and nodules
Effervescence: slight to violent
Reaction: moderately alkaline

Bss horizons:
Hue: 10YR or 2.5Y
Value: 5 to 7, 4 to 6 moist
Chroma: 1 or 2
Texture: clay
Secondary calcium carbonate: 0 to 2 percent by volume as films, filaments, and nodules
Effervescence: slight to violent
Reaction: moderately alkaline

Bkk horizons:
Hue: 10YR or 2.5Y
Value: 5 to 8, 4 to 7 moist
Chroma: 1 or 2
Texture: clay
Secondary calcium carbonate: 50 to 70 percent by volume in the form of filaments, masses, nodules, and finely disseminated carbonates
Calcium carbonate equivalent: 40 to 50 percent by weight
Effervescence: violent
Reaction: strongly alkaline

Bkss horizon (where present):
Hue: 10YR or 2.5Y
Value: 5 to 8, 4 to 7 moist
Chroma: 1 or 2
Texture: clay
Secondary calcium carbonate: 5 to 40 percent by volume in the form of filaments, masses, nodules, and finely disseminated carbonates
Calcium carbonate equivalent: 3 to 30 percent by weight
Effervescence: violent
Reaction: moderately alkaline or strongly alkaline

COMPETING SERIES: There are no competing series. Similar soils include the Chapel, Lockney, Lofton, McLean, Ranco, Randall, Sparenberg, and Yellowlake series.
Chapel series: have a calcic horizon within 100 cm (40 in) of the soil surface and has cracks that remain open less than 150 cumulative days during most years.
Lockney series: have a calcic horizon between 150 and 203 cm (60 and 80 in) of the soil surface.
Lofton series: have an argillic horizon.
McLean and Sparenberg series: have cracks that remain open less than 150 cumulative days during most years and do not have a calcic horizon.
Ranco and Randall series: have aquic conditions and do not have a calcic horizon.
Yellowlake series: have SAR of 13 or more within 102 co (40 in) of the soil surface and do not have a calcic horizon.

GEOGRAPHIC SETTING:
Parent material: calcareous, clayey lacustrine deposits of Pleistocene age.
Landform: playa step 0.5 to 3 m (2 to 10 ft) above the playa floor in large basins and range in size from a few acres to more than 200 acres.
Slopes: range from 0 to 1 percent.
Mean annual air temperature: 14 to 17 degrees C (57 to 63 F).
Mean annual precipitation: 432 to 533 mm (17 to 21 in).
Frost-free period: 180 to 220 days.
Elevation: 975 to 1,402 m (3,199 to 4,600 ft).
Thornthwaite annual P-E Index Values: 25 to 36.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the similar Lockney, McLean, Randall, Ranco, and Sparenberg series and also the Arch, Drake, Estacado, Lofton, Pep, and Portales series.
Lockney and Lofton soils: are on similar playa step landscape positions.
McLean, Randall, Ranco, and Sparenberg soils: are on the floor of playa basins.
Arch and Portales soils: are on playa slopes and interdunes and have 18 to 35 percent clay in the particle-size control section.
Drake soils: are on playa dunes and have 18 to 35 percent clay in the particle-size control section.
Estacado and Pep soils: are on playa slopes and plains and have 18 to 35 percent clay in the particle-size control section.

DRAINAGE AND PERMEABILITY: Moderately well drained. Very slow permeability. Surface runoff is negligible on concave slopes of less than 1 percent. Ponding is occasional for very brief periods during some years.
USE AND VEGETATION: Used mainly for livestock grazing. Some areas are cultivated to wheat, cotton, or grain sorghum. Vegetation varies according to amount of water available. Native vegetation includes buffalograss, blue grama, vine mesquite, and western wheatgrass. This soil has been correlated to the Deep Hardland (R077CY022TX) ecological site in MLRA-77C.

DISTRIBUTION AND EXTENT: Southern High Plains, Southern Part (MLRA 77C of LRR H) of west Texas and eastern New Mexico. The series is of moderate extent.

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

SERIES ESTABLISHED: Deaf Smith County, Texas; 1991

REMARKS: These soils were formerly included in the Lipan and Roscoe series.
Classification change 7/1999 from Chromic Haplusterts to Calcic Haplusterts based on application of the Eighth Edition of Soil Taxonomy.

Diagnostic horizons and features recognized in this pedon are:

Mollic epipedon: 0 to 34 cm (0 to 13 in) (Ap and Bss1 horizons)
Slickensides: 10 to 135 cm (0 to 53 in) (Bss horizons)
Calcic horizon: 135 to 203 cm (53 to 80 in) (Bkk horizon)
Vertic features: cracks extending from 0 to 75 cm (30 in) and wedged-shaped peds that have long axes tilted 10 to 60 degrees from horizontal (Ap and Bss horizons)

ADDITIONAL DATA: KSSL lab data - S06TX369002 (Parmer County, Texas); S94TX359001, S94TX359002 (Oldham County, Texas).

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


National Cooperative Soil Survey
U.S.A.