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Peoples of the OT –– Arameans Dr. Rick Griffith, Singapore Bible College Dr. Rick Griffith, Singapore Bible College www.biblestudydownloads.com www.biblestudydownloads.com

Soils of Wisconsin Topic C. Soil Uncemented aggregate of mineral grains and decayed organic matter with liquid and gas in the empty spaces between the

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Soils of Wisconsin

Topic C

Topic C

Soil

Uncemented aggregate of mineral grains and decayed organic matter with liquid and gas in the empty spaces between the solid particles.

Topic C

Topic C

Types of Soils

1. Granular Soils – Sand and Gravel

2. Fine Grained Soils – Clays and Silts

3. Organic Soils – Topsoil and Peat

Topic C

1.Granular Soils • Sand and Gravel• Excellent foundation, embankment and backfill

material.• Not susceptible to frost• High permeability• Settle rapidly while loaded• Develops strength through particle

contact/friction.

Topic C

Granular Soils – StructureStrength Development

Topic C

1.Granular Soils • Sand and Gravel• Excellent foundation, embankment and backfill

material.• Not susceptible to frost• High permeability• Settle rapidly while loaded• Develops strength through particle

contact/friction.

Topic C

Gravel

• Larger Particles• More pervious• More stable• Less affected by

water or frost

Sand

• Finer Particles–Feels gritty

• Finer and smoother it is closer to silt.–Decreased

permeability–Reduced stability

in waterTopic C

2. Fine Grained Soils

1. Silts – Nonplastic

2. Clays - Plastic

Topic C

Plastic

Capable of being shaped or formed.

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2. Fine Grained Soils • Soil passing a No. 200 sieve

• Silts = 0.075 mm to 0.002 mm (0.003 in to 0.00008 in)

• Clays – less than 0.002 mm (0.00008 in)

Topic C

2. Fine Grained SoilsCharacteristics

• Low shear strengths• Poor construction material• Practically impervious• Highly susceptible to frost• Develops strength from particle bonds• Higher amount of energy needed to compact

(particularly clay soils)Topic C

Clay Particles Structure

Topic C

Clay Particles Structure

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• Non-plastic• Unstable in water.• Change volume

when shape changes.

• Pulverized by finger when dry.

Silts Clays• Plastic• Compressible• Wet–Low resistance

to deformation.• Hard cohesive

mass when dry.• Impervious.

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3. Organic Soils• Topsoil

• Peat

• Rootmat

• Organic matter

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3. Organic Soils

• Not suitable for foundations or construction materials.

• Unacceptable roadway material.

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Organic Soils

1. Reduced load-carrying capacity

2. Low Shear Strength

3. Increased compressibility

4. Releases toxic gases upon decay

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Water and Soil• Necessary Evil• Critical to compaction effort• Reduces strength of soil• Loss of Stability• Groundwater moves soil particles• Erosion• Amount of water influences permeability and frost action.

Topic C

Effects of Water on Soil• Concentrated zones of groundwater on a

cut slope cause the soils to flow down the slope.–Often exists where a fine sand or silt

overlays an impervious soil (clay).

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• Seepage zones in backslopes causes slumping or sliding of slopes.

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