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Lecture for ESC311-507, Soils and Land Use, January 31, 2002 Alluvial and Peat Soils

Lecture for ESC311-507, Soils and Land Use, January 31, 2002 Alluvial and Peat Soils

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Lecture for ESC311-507, Soils and Land Use, January 31, 2002 Alluvial and Peat Soils. Capillarity. ESC311-507 Week 4 field trip. Alluvial and Organic Soils. 2. 1. 3. 4. ESC311-507 Week 4 field trip. Alluvial and Organic Soils. 2. 1. 3. 4. 1. - PowerPoint PPT Presentation

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Page 1: Lecture for ESC311-507,  Soils and Land Use, January 31, 2002 Alluvial and Peat Soils

Lecture for ESC311-507,

Soils and Land Use, January 31, 2002

Alluvial and Peat Soils

Page 2: Lecture for ESC311-507,  Soils and Land Use, January 31, 2002 Alluvial and Peat Soils

Capillarity

Page 3: Lecture for ESC311-507,  Soils and Land Use, January 31, 2002 Alluvial and Peat Soils
Page 4: Lecture for ESC311-507,  Soils and Land Use, January 31, 2002 Alluvial and Peat Soils
Page 5: Lecture for ESC311-507,  Soils and Land Use, January 31, 2002 Alluvial and Peat Soils

depth (cm)

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sandy loam clay loam

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ESC311-507 Week 4 field trip. Alluvial and Organic Soils

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3

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ESC311-507 Week 4 field trip. Alluvial and Organic Soils

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ESC311-507 Week 4 field trip. Alluvial and Organic Soils

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ESC311-507 Week 4 field trip. Alluvial and Organic Soils

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ESC311-507 Week 4 field trip. Alluvial and Organic Soils

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Page 23: Lecture for ESC311-507,  Soils and Land Use, January 31, 2002 Alluvial and Peat Soils

SEATTLE SERIES

The Seattle series consists of very deep, very poorly drained organic soils formed in herbaceous and woody deposits in depressions in river valleys and glacial till plains. Slopes are 0 to 1 percent. Average annual precipitationis about 40 inches. Mean annual temperature is about 50 degrees F.

TAXONOMIC CLASS: Euic, mesic Hemic Haplosaprists

TYPICAL PEDON: Seattle muck, pasture. (Colors are for moist soil unless otherwise noted.)

Oap--0 to 11 inches; black (5YR 2/1) muck, black (10YR 2/1) dry; about 10 percent fibers, less than 1 percent rubbed; strong fine granular structure; hard, very friable, nonsticky, nonplastic; many roots; strongly acid (pH5.4); clear smooth boundary. (10 to 13 inches thick)

Oe--11 to 17 inches; dark reddish brown (5YR 2/2) mucky peat, black (10YR 2/1) and dark brown (10YR 4/3) dry; about 60 percent fibers, 25 percent rubbed; laminar structure; very hard, very friable, nonsticky, nonplastic;common roots; strongly acid (pH 5.1); clear smooth boundary. (3 to 12 inches thick)

Oa1--17 to 21 inches; black (5YR 2/1) muck, black (5YR 2/1) dry; about 5 percent fibers, less than 1 percent rubbed; massive; very hard, very friable, slightly sticky, slightly plastic; few roots; very strongly acid (pH 4.8);clear wavy boundary. (0 to 6 inches thick)

Oa2--21 to 35 inches; very dark brown (7.5YR 2/2) muck, very dark grayish brown (10YR 3/2) and pale brown (10YR 6/3) dry; about 45 percent fibers, 15 percent rubbed; massive, very hard, very friable, nonsticky,nonplastic; few roots; moderately acid (pH 6.0); clear smooth boundary. (12 to 17 inches thick)

O'e--35 to 60 inches; dark brown (7.5YR 3/4) mucky peat, very dark brown (10YR 2/2) and brown (10YR 5/3) dry; about 70 percent fibers, 35 percent rubbed; massive; very hard, very friable, nonsticky, nonplastic; fewroots; moderately acid (pH 5.8 water).

Page 24: Lecture for ESC311-507,  Soils and Land Use, January 31, 2002 Alluvial and Peat Soils

ALDERWOOD SERIES

The Alderwood series consists of moderately deep, moderately well drained soils formed in glacial till. Alderwood soils are on glacially modified foothills and valleys and have slopes of 0 to 65 percent. The average annualprecipitation is about 40 inches, and the mean annual temperature is about 50 degrees F.

TAXONOMIC CLASS: Loamy-skeletal, isotic, mesic Vitrandic Dystroxerepts

TYPICAL PEDON: Alderwood gravelly loam - forested. (Colors are for moist soil unless otherwise noted.)

Ap--0 to 7 inches; very dark grayish brown (10YR 3/2) gravelly sandy loam, brown (10YR 5/3) dry; moderate fine granular structure; slightly hard, very friable, slightly sticky and slightly plastic; many fine roots; few fineinterstitial pores; slightly acid (pH 6.2); abrupt smooth boundary. (3 to 7 inches thick)

Bs1--7 to 21 inches; dark yellowish brown (10YR 4/4) very gravelly sandy loam, yellowish brown (10YR 5/4) dry; weak medium subangular blocky structure; slightly hard, very friable, nonsticky and nonplastic; many fineroots; many fine tubular and interstitial pores; 35 percent pebbles; diffuse smooth boundary; slightly acid (pH 6.2).

Bs2--21 to 30 inches; dark brown (10YR 4/3) very gravelly sandy loam, pale brown (10YR 6/3); dry; weak medium subangular blocky structure; slightly hard, very friable, nonsticky and nonplastic; common fine roots; fewvery fine tubular pores; 40 percent pebbles; slightly acid (pH 6.2); clear wavy boundary. (Bs horizon 15 to 30 inches thick)

Bs3--30 to 35 inches; 50 percent olive brown (2.5Y 4/4) very gravelly sandy loam, light yellowish brown (2.5Y 6/4) dry and 50 percent dark grayish brown (2.5Y 4/2) cemented fragments with strong brown (7.5YR 5/6)coatings on fragments, light brownish gray (2.5Y 6/2) and reddish yellow (7.5YR 6/6) dry; massive; slightly hard, very friable, nonsticky and nonplastic; few fine roots; common fine tubular and interstitial pores; 45 percentpebbles; moderately acid (pH 6.0); abrupt wavy boundary. (0 to 15 inches thick)

Bsm--35 to 43 inches; dark grayish brown (2.5Y 4/2) cemented layer that crushes to very gravelly sandy loam, light brownish gray (2.5Y 6/2) dry; dark yellowish brown (10YR 4/4), reddish brown (5Y 4/4), yellowish red(5YR 4/8) and strong brown (7.5YR 5/6) in cracks; massive; extremely hard; extremely firm, nonsticky and nonplastic; few fine roots; few fine tubular pores; 40 percent pebbles; moderately acid (pH 6.0); abrupt irregularboundary. (5 to 20 inches thick)

Cd--43 to 60 inches; grayish brown (2.5Y 5/2) compact glacial till that breaks to very gravelly sandy loam, light gray (2.5Y 7/2) dry; massive; extremely hard, extremely firm, nonsticky and nonplastic; 40 percent pebbles;moderately acid (pH 6.0).

Page 25: Lecture for ESC311-507,  Soils and Land Use, January 31, 2002 Alluvial and Peat Soils

SULTAN SERIES

The Sultan series consists of very deep, moderately well drained soils formed in recent alluvium on floodplains at elevations of near sea level to 120 feet. Slopes are 0 to 3 percent. Average annual precipitation is about 45inches. Mean annual temperature is 50 degrees F.

TAXONOMIC CLASS: Fine-silty, isotic, mesic Aquandic Dystroxerepts

TYPICAL PEDON: Sultan silt loam - pasture. (Colors are for moist soil unless otherwise noted.)

Ap--0 to 9 inches; very dark grayish brown (10YR 3/2) silt loam, light brownish gray (10YR 6/2) dry; moderate medium granular structure; hard, firm, moderately sticky, moderately plastic; many roots; slightly acid (pH6.4); abrupt smooth boundary. (6 to 10 inches thick)

Bw1--9 to 21 inches; yellowish brown (10YR 5/4) silty clay loam, pale brown (10YR 6/3) dry; moderate fine subangular blocky structure; hard, friable, moderately sticky, moderately plastic; many roots; slightly acid (pH6.4); clear wavy boundary. (10 to 14 inches thick)

Bw2--21 to 24 inches; light olive brown (2.5Y 5/4) silt loam, pale yellow (2.5Y 7/4) dry; many medium prominent yellowish brown (10YR 5/8) mottles; moderate medium subangular blocky structure; hard, very friable,slightly moderately sticky, slightly plastic; common roots; neutral (pH 6.6); clear wavy boundary. (2 to 5 inches thick)

Bg--24 to 48 inches; grayish brown (2.5Y 5/2) silty clay loam, pale yellow (2.5Y 8/2) dry; many medium prominent yellowish brown (10YR 5/8) mottles; moderate medium prismatic structure; slightly hard, very friable,moderately sticky, moderately plastic; few roots; neutral (pH 6.6); clear wavy boundary. (20 to 30 inches thick)

Cg--48 to 66 inches; olive gray (5Y 5/2) very fine sandy loam stratified with medium sand, light gray (2.5Y 7/2) dry; common fine prominent yellowish red (5YR 4/6) mottles; massive; slightly hard, very friable; few roots;very strongly acid (pH 4.8).

Page 26: Lecture for ESC311-507,  Soils and Land Use, January 31, 2002 Alluvial and Peat Soils
Page 27: Lecture for ESC311-507,  Soils and Land Use, January 31, 2002 Alluvial and Peat Soils