LOCATION CAMBERN            AZ
Established Series
Rev. MLM/YHH
06/2009

CAMBERN SERIES


The Cambern series consists of well drained, moderately slowly permeable soils that are moderately deep to tuff and ash. Cambern soils formed in ash and tuff, with some influence from basalt and cinders on mountain side slopes and mountain tops. Permeability is moderately slow. Slopes range from 1 to 25 percent. Mean annual precipitation is about 25 inches and mean annual temperature is about 42 degrees F.

TAXONOMIC CLASS: Fine-loamy, mixed, superactive, frigid Pachic Argiustolls

TYPICAL PEDON: Cambern sandy loam - forest. (Color for dry conditions unless otherwise noted.)

0i--0 to 1 inch; pine needles.

A1--1 to 4 inches; dark gray (10YR 4/1) sandy loam, very dark brown (10YR 2/2) moist; moderate medium platy structure; slightly hard, very friable, nonsticky and slightly plastic; abundant fine and medium roots; many fine interstitial and few fine tubular pores; noneffervescent; slightly acid (pH 6.5); clear smooth boundary. (2 to 6 inches thick.)

A2--4 to 11 inches; dark gray (10YR 4/1) loam, very dark brown (10YR 2/2) moist; weak medium and coarse subangular blocky structure; slightly hard, friable, slightly sticky and plastic; abundant fine and plentiful medium roots; many fine interstitial and few fine tubular pores; noneffervescent; neutral (pH 7.0); gradual smooth boundary. (6 to 10 inches thick)

Bw--11 to 15 inches; dark gray (10YR 4/1) loam, very dark brown (10YR 2/2) moist; moderate medium and coarse subangular blocky structure; hard, friable, slightly sticky and plastic; few fine, medium and large roots; common fine interstitial and few fine tubular pores; noneffervescent; neutral (pH 7.0); gradual smooth boundary. (1 to 6 inches thick.)

Bt1--15 to 21 inches; dark gray (10YR 4/1) clay loam, very dark brown (10YR 2/2) moist; weak and moderate medium and coarse subangular blocky structure; hard, firm, sticky and plastic; abundant fine and few medium roots; common fine interstitial and few fine tubular pores; common thin clay films on ped faces and in pores; noneffervescent; neutral (pH 7.0); clear smooth boundary. (5 to 7 inches thick.)

Bt2--21 to 29 inches; dark grayish brown (10YR 4/2) clay loam, very dark brown (10YR 2/2) moist; weak medium subangular blocky structure; hard, firm, sticky and plastic; abundant fine and few medium roots; common fine interstitial and tubular pores; common moderately thick clay films on ped faces and in pores; 10 percent by volume of very pale brown (10YR 7/3) fragments of decomposing tuff, yellowish brown (10YR 5/4) moist; noneffervescent; neutral (pH 7.0); abrupt irregular boundary. (6 to 11 inches thick)

R--29 to 41 inches; white (7.5YR 8/1) tuff and ash, brown (7.5YR 4/2) moist, with tongues 3mm to 1 inch thick of the Bt2 horizon extending approximately 12 inches into the seams and fractures; massive; hard, extremely firm; few fine and medium roots in fractures; few fine interstitial pores in interfaces; common thin clay films in seams; noneffervescent; slightly alkaline (pH 7.5).

TYPE LOCATION: Apache County, Arizona, about 3 miles east of Alpine; 300 feet north and 50 feet west of the SE corner of sec. 16, T. 5 N. R. 31 E.

RANGE IN CHARACTERISTICS:

Mean annual soil temperature: 36 to 47 degrees F.

Soil moisture: typic ustic moisture regime

Depth to the R horizon: 20 to 40 inches but is normally 24 to 40 inches

These soils may have a thin C horizon immediately above the R horizon

Cementation: hard weakly cemented ash and tuff to extremely hard tuff

A horizon

Reaction: medium acid to neutral

Bt horizon

Reaction: medium acid to moderately alkaline in the lower part

A horizon
Hues: 10YR and 7.5YR
Value: 3 and 5 dry, 2 to 3 moist
Chroma: 1 to 3
Texture: sandy loam, silt loam, loam, gravelly or cobbly sandy loam, silt loam, gravelly loam.

B horizons
Hue: 7.5 and 10YR
Value: 3 to 5 dry, 2 to 4 moist
Chroma: 1 to 4, dry or moist
Texture: loam, light clay loam, gravelly clay loam
Clay content: greater than 18 percent but less than 35 percent clay

Rock fragments: When gravel, cobbles and stones occur on the surface and throughout the profile they are less than 50 percent by volume.

COMPETING SERIES: These are the Bowbells (ND), Carfall (MT), Center Creek (UT), Chugcreek (WY), Detra (UT), Fiesta (NM), Flaxton (ND), Gordo (AZ), Hereford (AZ), Hesperus (CO), Jaythree (NM), Laceycreek (MT), Ohwiler (CO), Pachel (MT), Schauson (UT), Shermap (T)(CO), Todacheene (NM), Tschicoma (T)(NM) and Weed (CO) series. Bowbells, Carfall, Center Creek, Fiesta, Flaxton, Hereford, Hesperus, Jaythree, Laceycreek, Ohwiler, Pachel, Schauson, Shermap, Todacheene, Tschicoma and Weed soils are very deep. Detra soils have a lithic contact of limestone between 40 and 60 inches deep. Chugcreek soils have a lithic contact of granite at moderate depths. Gordo soils have a paralithic contact of basalt and cinders at moderate depths.

GEOGRAPHIC SETTING: The Cambern soils are on nearly level to moderately steep mountain side slopes and mountain tops. Slopes range from 1 to 25 percent but are dominantly 2 to 15 percent. The soils are formed from ash and tuff, with some influence from basalt and cinders. These soils occur at elevations of 7,000 to 9,000 feet in a continental climate. The average annual precipitation ranges from 18 to 30 inches and the mean annual temperature ranges from about 37 to 47 degrees F. The frost-free period ranges from 70 to 120 days.

GEOGRAPHICALLY ASSOCIATED SOILS: In addition to the Sponseller and Gordo soils these include the Bushvalley, Luna, Brolliar, Sizer, Tatiyee and Kessay series. Bushvalley soils are shallow to bedrock and have over 50 percent coarse fragments in the control section. Luna and Brolliar soils have fine-textured argillic horizons. Sizer soils are shallow to very cindery materials. Tatiyee soils have over 50 percent coarse fragments and are members of a clayey-skeletal, montmorillonitic family. The Kessay soils are similar but lack the R horizon that is characteristic of the Cambern soils and are formed from basalt.

DRAINAGE AND PERMEABILITY: Well-drained with slow to medium runoff. Permeability is moderately slow.

USE AND VEGETATION: These soils are used for grazing and the production of timber. A few minor areas are dry farmed to small grains. Natural vegetation consists of ponderosa pine, fir, spruce and quaking aspen with an understory of Kentucky bluegrass, Arizona fescue, blue grama, sideoats grama and mountain muhly.

DISTRIBUTION AND EXTENT: East central Arizona. The series is moderately extensive. MLRA 39.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Phoenix, Arizona

SERIES ESTABLISHED: St. Johns-Springerville Area, Apache Co., Arizona, 1971. Cambern is the name of an old townsite about 10 miles southeast of the sample site.

REMARKS: Diagnostic horizons and features recognized in this pedon are:

Mollic epipedon: the zone from 1 to 29 inches (A, Bw, Bt horizons)

Argillic horizon: the zone from 15 to 29 inches (Bt1 and Bt2 horizons)

Lithic contact: 29 inches--basalt (R horizon)

Classified according to Soil Taxonomy, Second Edition, 1999; Keys to Soil Taxonomy, Tenth Edition, 2006.

Revised for the correlation of AZ675, 5/2009, WWJ

ADDITIONAL DATA: NSSL data numbers; S65AZ 001 017, S65AZ 001 018, and S65AZ 001 021,


National Cooperative Soil Survey
U.S.A.