LOCATION GRECAN             ID
Established Series
FRK/RJS
07/2008

GRECAN SERIES


The Grecan series consists of very deep, well drained soils formed in alluvium derived from sandstone, limestone, dolomite and conglomerate. These soils are on terraces and hills. Slopes are 4 to 20 percent. Mean annual precipitation is about 432 mm and mean annual temperature is about 6 degrees C.

TAXONOMIC CLASS: Fine, smectitic, frigid Calcic Pachic Argixerolls

TYPICAL PEDON: Grecan loam, rangeland (colors are for dry soil unless otherwise noted)

A1--0 to 8 cm; dark grayish brown (10YR 4/2) loam, very dark grayish brown (10YR 3/2) moist; moderate fine granular structure; soft, very friable, nonsticky and nonplastic; many very fine and fine roots, common medium roots; common very fine irregular pores; 5 percent gravel; slightly acid (pH 6.2); abrupt smooth boundary. (8 to 25 cm thick)

A2--8 to 23 cm; dark grayish brown (10YR 4/2) loam, very dark grayish brown (10YR 3/2) moist; moderate medium subangular blocky parting to moderate fine granular structure; soft, very friable, nonsticky and nonplastic; common very fine and fine roots, few medium roots; common very fine and fine irregular pores; 5 percent gravel; neutral (pH 6.6); clear smooth boundary. (0 to 25 cm thick)

BAt--23 to 56 cm; dark grayish brown (10YR 4/2) clay loam, very dark grayish brown (10YR 3/2) moist; strong medium subangular blocky structure; slightly hard, friable, slightly sticky and slightly plastic; common fine and few medium roots; common very fine and fine tubular pores; common distinct clay films on faces of peds; 10 percent gravel; neutral (pH 7.0); clear smooth boundary. (13 to 33 cm thick)

Bt--56 to 71 cm; pale brown (10YR 6/3) clay, brown (10YR 5/3) moist; strong medium subangular blocky structure; very hard, very firm, moderately sticky and moderately plastic; few fine and very fine roots; common very fine and fine tubular pores; many distinct clay films on faces of peds and in pores; 10 percent gravel; neutral (pH 7.2); clear smooth boundary. (15 to 61 cm thick)

Btk--71 to 81 cm; pale brown (10YR 6/3) clay, yellowish brown (10YR 5/4) moist; moderate medium subangular blocky; very hard, very firm, moderately sticky and moderately plastic; few very fine roots; common very fine and fine irregular pores; few distinct clay films on faces of peds and in pores; few fine soft masses of lime and disseminated lime; 10 percent gravel; slightly effervescent; moderately alkaline (pH 8.0); clear wavy boundary. (10 to 61 cm thick)

Bk1--81 to 104 cm; yellowish brown (10YR 5/4) clay loam, dark yellowish brown (10YR 4/4) moist; weak medium and coarse subangular blocky; hard, firm, slightly sticky and slightly plastic; few very fine roots; few very fine and fine irregular pores; common large soft masses of lime and few thin pendant lime coatings on the underside of rocks; 10 percent gravel; violently effervescent; moderately alkaline (pH 8.2); clear wavy boundary. (23 to 46 cm thick)

Bk2--104 to 152 cm; very pale brown (10YR 7/3) loam, light yellowish brown (10YR 6/4) moist; weak coarse subangular blocky; soft, friable, nonsticky and slightly plastic; few very fine and fine irregular pores; common large soft masses of lime and few thin pendant lime coatings on the underside of rocks; 10 percent gravel; violently effervescent; moderately alkaline (pH 8.2). (0 to 48 cm thick)

TYPE LOCATION: Bear Lake County, Idaho; 2200 feet south and 25 feet west of the NE corner of section 21, T. 15 S., R.43 E. St. Charles topographic quadrangle. UTM NAD 83 Zone 12: Northing 4661539, Easting 464862.

RANGE IN CHARACTERISTICS:
Soil temperature - 4 to 7 degrees C.
Soil moisture control section: between 10 and 30 centimeters; dry in all parts for 45 consecutive days or more in the four months following the summer solstice. Xeric moisture regime.
Thickness of the mollic epipedon - 50 to 71 cm
Depth to secondary carbonates: 41 to 81 cm

A horizons
Value: 3 or 4 dry, 2 or 3 moist
Chroma: 2 dry, 1 or 2 moist
Clay content: 15 to 25 percent
Rock fragments: 0 to 10 percent gravel
Reaction: pH 6.1 to 7.3

BAt horizon
Value: 3 or 4 dry; 2 or 3 moist
Chroma: 2 or 3, dry or moist
Clay content: 30 to 40 percent
Rock fragments: 0 to 10 percent gravel
Reaction: 6.6 to 7.8

Bt horizon
Hue: 10YR or 7.5YR
Value: 4 to 6 dry; 3 to 5 moist
Chroma: 2 or 3, dry or moist
Clay content: 35 to 45 percent
Texture: clay loam or clay
Rock fragments: 0 to 10 percent gravel
Reaction: 6.6 to 7.8

Btk horizon
Hue: 10YR or 7.5YR
Value: 4 to 6 dry; 3 to 5 moist
Chroma: 2 to 4, dry or moist
Clay content: 35 to 45 percent
Texture: clay loam or clay
Rock fragments: 0 to 10 percent gravel
Calcium carbonate equivalent: 2 to 10 percent
Reaction: 7.4 to 8.4

Bk horizons
Hue: 10YR or 7.5YR
Value: 5 to 8 dry; 4 to 7 moist
Chroma: 2 to 4, dry or moist
Clay content: 18 to 35 percent
Texture: loam or clay loam
Rock fragments: 0 to 15 percent gravel
Calcium carbonate equivalent: 5 to 15 percent
Reaction: 7.9 to 8.4

COMPETING SERIES: These are the Iwica and Siroco series. The Iwica series has a duripan at 107 to 152 cm. The Siroco series has greater than 15 percent rock fragments in the particle size control section.

GEOGRAPHIC SETTING: Grecan soils are on terraces and hillsides. Elevations are 1798 to 2175 m. Slopes are 4 to 20 percent. These soils formed in alluvium derived from sandstone, limestone, dolomite and conglomerate. The climate is characterized by long, cold winters; moist springs; and warm, dry summers. Mean annual precipitation is 381 to 508 mm, much of which falls as snow or spring rain. Mean annual temperature is 4 to 7 degrees C. Frost-free period is 70 to 90 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Clegg, Hagenbarth, Hutchley, and Swanpeak soils. Clegg and Hagenbarth soils have a fine-loamy particle size control section and occupy similar landform positions. Hutchley soils are shallow to lithic contact, have a loamy-skeletal particle size control section and are on summits and shoulders. Swanpeak soils have a clayey-skeletal particle size control section and occupy similar landform positions.

DRAINAGE AND PERMEABILITY: Well drained, slow permeability.

USE AND VEGETATION: Grecan soils are used for rangeland and wildlife habitat. Potential native vegetation is mountain big sagebrush, antelope bitterbrush, serviceberry, snowberry, bluebunch wheatgrass, and western wheatgrass.

DISTRIBUTION AND EXTENT: Grecan soils are of limited extent in southeastern Idaho. MLRA 43B.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Bozeman, Montana

SERIES ESTABLISHED: Bear Lake County, Idaho 2008. The name is coined.

REMARKS: Diagnostic horizons and features recognized in this pedon are:
Mollic epipedon - from the soil surface to 56 cm (A1, A2, and BAt horizons)
Argillic horizon - from 23 to 81 cm (BAt, Bt, and Btk horizons)
Secondary carbonates - from 71 to 152 cm (Btk, Bk1 and Bk2 horizons)
Particle-size control section - upper 50 cm of the argillic horizon - from 23 to 73 cm (BAt, Bt, and part of the Btk horizons).
Grecan soils have a xeric moisture regime and a frigid temperature regime.


National Cooperative Soil Survey
U.S.A.