LOCATION DEADMANBAY         WA
Established Series
IRD MPR/SBC
04/2007

DEADMANBAY SERIES


The Deadmanbay series consists of deep, somewhat poorly drained soils formed in glacial drift underlain by dense glaciomarine deposits. Deadmanbay soils are in valleys of drift plains and drainageways of hills and mountains and have slopes of 2 to 15 percent. The mean annual precipitation is about 838 mm and the mean annual temperature is about 9 degrees C.

TAXONOMIC CLASS: Fine-loamy, mixed, superactive, mesic Aquultic Haploxeralfs

TYPICAL PEDON: Deadmanbay silt loam, forested, in a gently sloping mountain valley at 80 m elevation. (Colors are for moist soil unless otherwise noted. When described on July 29, 2004 the soil was dry to 41 cm and moist below.)

Oi--0 to 3 cm; slightly decomposed plant material; abrupt wavy boundary.

A--3 to 13 cm; black (10YR 2/1) silt loam, very dark grayish brown (10YR 3/2) dry; strong coarse granular structure; slightly hard, very friable, nonsticky, nonplastic; many very fine and fine, common medium, and few coarse roots; few fine and medium tubular and common medium irregular pores; 10 percent gravel; very strongly acid (pH 5.0); clear wavy boundary. (7 to 20 cm thick)

Bw--13 to 41 cm; dark brown (10YR 3/3) silt loam, dark yellowish brown (10YR 4/4) dry; moderate coarse subangular blocky structure; moderately hard, friable, moderately sticky, moderately plastic; many very fine and fine, common medium, and few coarse roots; few fine and many medium tubular and common medium irregular pores; 10 percent gravel; moderately acid (pH 5.6); abrupt wavy boundary. (15 to 30 cm thick)

Bg--41 to 74 cm; dark yellowish brown (10YR 4/6) loamy coarse sand, yellowish brown (10YR 5/6) dry; massive; moderately hard, friable, nonsticky, nonplastic; few very fine, fine, and medium roots; many very fine interstitial pores; many fine prominent irregular reddish gray (2.5YR 6/1) dry, and reddish gray (2.5YR 5/1) moist, iron depletions in matrix; moderately acid (pH 6.0); clear wavy boundary. (20 to 40 cm thick)

2Btg--74 to 145 cm; dark yellowish brown (10YR 4/6) gravelly silty clay loam, yellowish brown (10YR 5/6) dry; strong medium subangular blocky structure; hard, friable, moderately sticky, moderately plastic; few fine roots and few medium roots; few very fine interstitial pores; many fine prominent irregular reddish gray (2.5YR 5/1) moist, and reddish gray (2.5YR 6/1) dry, iron depletions in matrix; 30 percent gravel; slightly acid (pH 6.4); gradual wavy boundary. (40 to 80 cm thick)

2Cd--145 to 152 cm; dark reddish gray (2.5YR 4/1) silty clay loam, reddish gray (2.5YR 5/1) dry; massive; very hard, firm, moderately sticky, moderately plastic; 10 percent gravel; neutral (pH 7.3).

TYPE LOCATION: San Juan County, Washington, located about 300 m east and 650 m south of the northwest corner of sec. 19, T. 37 N., R 1 W. Willamette Meridian; False Bay, Washington USGS quadrangle; lat. 48 degrees, 40 minutes, 58 N. and long. 122 degrees, 52 minutes, 30 seconds W.

RANGE IN CHARACTERISTICS: Depths to diagnostic horizons and features start from the mineral soil surface.

Mean annual soil temperature - 9 to 10 degrees C.
Moisture control section - dry 60 to 75 days following the summer solstice
Depth to redoximorphic features - 23 to 46 cm
Depth to densic contact - 100 to 150 cm
Particle-size control section:
Clay content - 18 to 35 percent

A horizon
Value - 2 or 3 moist, 3 to 5 dry
Chroma - 2 or 3 moist, 1 or 2 dry

Bw horizon
Value - 3 or 4 moist, 4 or 5 dry
Chroma - 2 or 3 moist, 3 or 4 dry
Texture - SIL or L
Clay content - 12 to 27 percent
Rock fragments - 0 to 15 percent gravel

Bg horizon
Value - 4 or 5 moist, 5 to 7 dry
Chroma - 4 to 6 moist and dry
Texture - LCOS, LS, or SL
Clay content - 1 to 12 percent
Rock fragments - 0 to 35 percent gravel

2Btg horizons
Value - 4 or 5 moist, 5 to 7 dry
Chroma - 4 to 6 moist and dry
Texture - SICL, SIL, or L
Clay content - 18 to 35 percent
Rock fragments - 0 to 30 percent gravel

2Cd horizon
Value - 3 to 5 moist, 4 to 6 dry
Chroma - 2 or 3 moist and dry
Texture - SICL, SIL, or L
Clay content - 12 to 35 percent
Rock fragments - 0 to 15 percent gravel

COMPETING SERIES: These are the Doolyville (T), Killebrew, Mitchellbay, Quatama, and Stockel series. Doolyville, Quatama, and Stockel do not have a densic contact. Killebrew and Mitchellbay soils are on similar landscape positions but have densic contacts above 100 cm. Wellsdale soils do not have redoximorphic features above 50 cm or a densic contact.

GEOGRAPHIC SETTING: Deadmanbay soils are in valleys of drift plains and drainageways of hills and mountains. Slope ranges from 2 to 15 percent. These soils formed in glacial drift underlain by dense glaciomarine deposits. Elevations are 0 to 198 m. The climate is characterized by warm dry summers and mild moist winters. The mean annual precipitation is 635 to 1016 mm. The mean annual temperature is 9 to 10 degrees C. The frost-free period is about 200 to 240 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Bazal, Morancreek, and Cady soils. Bazal soils are in depressions within valleys and glacial drift plains and have aquic conditions to the surface and a densic contact at 50 to 100 cm. Morancreek soils are in similar landscape positions but do not have redoximorphic features above 38 cm or a densic contact. Cady soils are on slopes and summits of hills and mountains and have a lithic contact at 25 to 50 cm.

DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Somewhat poorly drained. Saturated hydraulic conductivity is moderately high to high in the upper part (A and B horizons) and moderately slow to very slow in the lower part (2Btg and 2Cd horizons).

USE AND VEGETATION: Deadmanbay soils are used for timber production, wildlife habitat, forage crop production, and livestock grazing. Potential natural vegetation consists of western redcedar, Douglas-fir, grand fir, lodgepole pine, red alder, common snowberry, trailing blackberry, salmonberry, stinging nettle, salal, swordfern, and bracken fern.

DISTRIBUTION AND EXTENT: Northwest Washington; MLRA A2, Northern Part. Series is of small extent.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Portland, Oregon

SERIES ESTABLISHED: San Juan County, Washington, 2006.

REMARKS: Diagnostic horizons and other features:

Umbric epipedon - the zone from 3 to 41 cm (A and Bw horizons)
Argillic horizon - 74 to 145 cm (2Btg horizon)
Densic contact - 145 cm (upper boundary of 2Cd horizon)
Particle-size control section - 74 to 124 cm (upper 50 cm of argillic horizon)
Depth to redoximorphic features - 41 cm (iron depletions with a chroma of 2 or less)


National Cooperative Soil Survey
U.S.A.