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Soil
Uncemented aggregate of mineral grains and decayed organic matter with liquid and gas in the empty spaces between the solid particles.
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
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 • 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
• 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.
Topic C
3. Organic Soils
• Not suitable for foundations or construction materials.
• Unacceptable roadway material.
Topic C
Organic Soils
1. Reduced load-carrying capacity
2. Low Shear Strength
3. Increased compressibility
4. Releases toxic gases upon decay
Topic C
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).
Topic C
• Seepage zones in backslopes causes slumping or sliding of slopes.