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Published byAnastasia Dean Modified over 9 years ago
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Soil Stresses (ch10)
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Stress Assumptions Continuous material Homogeneous (eng. props. = at all locations) Isotropic (Modulus and are = in all directions) Linear-elastic stress-strain properties
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Stress Concept
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x z normal stresses shear stresses Ten (-), Comp (+) Clock (+), CC (-)
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Strain Concept normal strain shear strain = shear strain [radians]
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Stress vs. Strain = Modulus
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Stresses in Soils 1. Geostatic Stresses Due to soil’s self weight 2. Induced Stresses Due to added loads (structures) 3. Dynamic Stresses e.g., earthquakes
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Geostatic Stresses TOTAL VERTICAL STRESS AT A POINT z = depth = 5 m A Ground surface Soil, = 18 kN/m 3 “total vertical stress at A”
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Geostatic Stresses SHEAR STRESSES If ground surface is flat, all geostatic shear stresses = zero
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Geostatic Stresses PORE WATER PRESSURE AT A POINT z = 5 m A Ground surface Soil, = 18 kN/m 3 “pore water pressure at A” h pA
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Geostatic Effective Stress board
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Example board
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Special Case Board – submerged soils
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Induced Stresses z A z A P = z = z + = =
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Bousinnesq - point loads zfzf A Point load See page 324 of your book…
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Area loads q = bearing pressure = P/A z A P Area, A B L Terminology: B < or = to L
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Area loads – z below corner zfzf B L z below corner of a loaded area: see page 327 (book)
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Area loads – z below center Circular loaded area zfzf A q
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Area loads – z below center Square loaded area Strip loads Rectangular area See page 332 (text)
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Lateral Stresses z A Ground surface Soil, = 18 kN/m 3 = Vertical effective stress = = Horiz. eff. stress = ?
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Lateral Stresses “Coefficient of lateral earth pressure”
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Superposition We can only add total stresses
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Stresses on other planes… So far we have x and z Now we want Stresses acting on other planes
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The Mohr Circle Describes 2-D stresses at a point in a material Plots and on an = scale Each point on the MC represents the and on one side of an element oriented at a certain angle The angle between two points in the MC is = 2 times the angle between the planes they represent
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The Mohr Circle A1A1 A2A2 B1B1 B2B2 B2 B1 A2 A1 A2 A1 B2 B1 If we change we will get two more points on the same MC. A B
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The Mohr Circle 2121 11
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The Mohr Circle – Principal Stresses Planes A and B are called principal planes when there are no shear stresses (only normal stresses) acting on them. 1 = major principal stress 3 = minor principal stress
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The Mohr Circle
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Direction of max principal stresses is 17 degrees c.c. from the vertical
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Effective Stress Mohr Circle board
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Seepage Force board
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Seepage Force - Example board
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