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Engineering Properties of Soils Soil Types
foundation for the project construction material (road embankments,earth dams) Soil Definition (Engineering) “refers to all unconsolidated material in the earth’s crust, all material above bedrock” mineral particles (sands, silts, clays) organic material (topsoil, marshes) + air + water Soils ENCI 579
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Engineering Properties of Soils Soil Types
Mineral Soil Particles weathering of rock from the crust of the earth physical weathering and chemical weathering Physical Weathering action of frost, water, wind, glaciers, plant/animals, etc. breaking particles away from original bedrock particles transported by wind, water, ice >rounding and reducing their size soils formed are called granular soil type “grains are similar to the original bedrock” Soils ENCI 579
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Engineering Properties of Soils Soil Types
Chemical weathering occurs when water flows through rocks and leaches out some of the mineral components of the rock soils formed are called clays “clay particles are mineral crystals that have very different properties from those of the original bedrock” Soils ENCI 579
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Engineering Properties of Soils Mineral Soils
Soils ENCI 579
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Engineering Properties of Soils Soil Types
Granular and Cohesive soil types difference in engineering properties result from the large variation in size and shape of the grains Cohesive soil type (clays) grains are extremely small and flat the mass of a grain as a force is negligible when compared to the forces resulting from the surface properties of the grain Soils ENCI 579
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Engineering Properties of Soils Soil Types
Water Holding Capacity of Clays Shrinkage evaporation of exposed clays loading Expansion dry side may absorb moisture Structure of Clays deposited by settling out in lakes Soils ENCI 579
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Engineering Properties of Soils Soil Types
Structure of Clays surface charges forces grains to edge to side pattern flocculent structure as opposed to granular soils which are deposited in a denser configuration because the force of gravity on the mass of these grains is more important Soils ENCI 579
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Engineering Properties of Soils Soil Types
Clays have surface charges due to the very large surface area per gram of material Chemical composition results in: negative charges along the sides of a grain positive charges at the ends of a grain Results of these surface properties water holding capacity of clays surface charges attract water structure of clay deposits clay grain Soils ENCI 579
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Engineering Properties of Soils Soil Types
Soils ENCI 579
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Engineering Properties of Soils Soil Types
Clay Soils Small flat shape Negative/positive surface charges Bound water on the surface Different clay minerals are different in size Swelling clays absorb water into the crystal lattice Shrinkage due to evaporation or loading Soils ENCI 579
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Engineering Properties of Soils Soil Types
Granular Soils Larger grain sizes than clays Particles tend to be more or less spheres/cubes Bound water is small compared to overall mass Silt particles may not be visible to eye but tend to be gritty, have dull appearance and lack cohesion when dry Soils ENCI 579
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Engineering Properties of Soils Soil Types
Organic Soils Tend to be fibrous and/or amorphous Brown to Black in color High moisture holding capacity Water may run out when squeezed Dried organic soils may combust Soils ENCI 579
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Engineering Properties of Soils Soil Types
Silts are coarser than clays and not bond tightly together Silts are gritty, less plastic and dull when cut Dry Strength-silts loose “apparent cohesion” when dried Shaking test-saturated silt samples become denser water seeps to the surface - “dilantancy” Soils ENCI 579
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Engineering Properties of Soils Mass-Volume Relationships
Soils ENCI 579
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Engineering Properties of Soils Mass-Volume Relationships
Example 1-2 A soil sample has a volume of 175cm3 and a total mass of 300g. Mass when dried is 230g. Relative density of the soil solids is Find r, rD, w, e, S and n Given: Mw = M - MD = 70g MD = 230g M = 300g V = 175cm3 Air Water Solids Soils ENCI 579
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Engineering Properties of Soils Mass-Volume Relationships
Calculations: Vw = Mw/rw = 70g/(1 g/cm3) =70 cm3 VD = MD/(RD x rw) = 230g/(2.70 x 1 g/cm3) = 85 cm3 VA = V- (VD + Vw ) = = 20 cm3 VA = 20 cm3 VW = 70 cm3 VD = 85 cm3 V = 175 cm3 Soils ENCI 579
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Engineering Properties of Soils Mass-Volume Relationships
Answer: r = M/V = 300g/175cm3 = 1.71 g/cm3 rD = MD/V = 230g/175cm3 = 1.31g/cm3 w = Mw / MD = 70g/230 g = 30.4 % e = Vv / VD = 90 cm3/85 cm3 = 1.06 S = VW /Vv = 70 cm3/90 cm3 = 78 % n = Vv /V = 90 cm3/ 175 cm3 = 51 % Soils ENCI 579
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Engineering Properties of Soils Mass-Volume Relationships - Rules
1. Density is given assume total unit volume 1 cm3 or 1 m3 2. Water content is given along with total density or total mass. Use MD = M or rD = r 1 + w 1+w 3. Void Ratio is given and RD assume a unit volume of soil solids VD = 1 m3 Soils ENCI 579
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Engineering Properties of Soils Mass-Volume Relationship
Density Index Field soil condition referred to as loose or dense Density Index is insitu soil’s density relative to the maximum and minimum for that type of soil Assessing the stability of granular soils Known as relative density ID = r DRY MAX x r D - r DRY MIN r D r DRY MAX - r DRY MIN Soils ENCI 579
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Engineering Properties of Soils
Soils ENCI 579
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Engineering Properties of Soils Classification Tests
Two types of tests used in classifying soils Grain size, measures grain sizes Plasticity, measures grain types Grain Size grain size distribution curve Sieve analysis gravel and sand Hydrometer test for silt and clay Soils ENCI 579
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Engineering Properties of Soils Classification Tests
Hydrometer Test Used to find the size of smaller grains to plot a grain size distribution curve Stokes Law particles in suspension settle out at a rate which varies with their size hydrometer measures the density of a soil-water mix at various times as the grain settles The size of particle to the center of the bulb can be calculated and density of the solution indicates the percentage of the sample still in solution Soils ENCI 579
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Engineering Properties of Soils Sieve Analysis
Soils ENCI 579
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Engineering Properties of Soils Classification Tests
Soils ENCI 579
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Engineering Properties of Soils Classification Tests
Grain Size Distribution Curve Shape Uniform soil is composed of mainly one size grain Well graded soil contains a wide range of grain sizes Effective Size Effective size is the grain size that only 10% of the grain sizes are finer than. The amount and type of fine grains in a soil are important in assessing the properties of that soil Soils ENCI 579
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Engineering Properties of Soils Classification Tests
Grain Size Distribution Curve Uniformity Coefficient Cu indication of the shape of the curve and range of particle sizes that the soil contains Cu = D60 / D10 Coefficient of Curvature Cc indication of the shape of the curve. Cc = (D30)2 / (D60 x D10) Soils ENCI 579
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Engineering Properties of Soils Classification Tests
Curve A - Uniform Soil Curve B - Well Graded Soil Soil B Effective size = .09 mm Cu = 7/.09=78 Cc = 1.12/(7x.09)=1.9 Soils ENCI 579
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Engineering Properties of Soils Classification Tests
Textural Classification based entirely on grain size ASTM System Gravel larger than 4.75 mm (No. 4) Sand mm mm (No.4-No. 200) Silt mm mm Clay smaller than mm Identify % of the grains as classified Soils ENCI 579
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Engineering Properties of Soils Classification Tests
Soils ENCI 579
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Engineering Properties of Soils Classification Tests
Plasticity Test (grain type) Measures the amount of water that a soil absorbs Plastic Limit w/c where the soil behaves like a plastic material Liquid Limit w/c where the soil behaves more like a liquid Plasticity Index (Atterberg Limits Test) the range of w/c’s where soil is plastic Soils ENCI 579
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Engineering Properties of Soils Classification Tests
Soils ENCI 579
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Engineering Properties of Soils Classification Tests
Atterberg Limits test measures the consistency of the soil deposit Soil A: Wp=25 Wl=32 w/c=35 Soil B: Wp=40 Wl=80 w/c=45 Atterberg Limits Test soil rolled into a thread Wp soil flow measured in a cup Wl Soils ENCI 579
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Engineering Properties of Soils Soil Classification
Unified Soil Classification ASTM D2487 general engineering purposes AASHTO Soil Classification highway engineering purposes classifies soils to it’s suitability as a subgrade Soils ENCI 579
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