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Vertical Stresses within Soils

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... Poisson's Ratio (strain normal to applied stress : strain parallel to ... Ratio (m) = 0, that is, if lateral strain = 0 then no bulging of the soil occurs ... – PowerPoint PPT presentation

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Title: Vertical Stresses within Soils


1
Vertical Stresses within Soils
  • Evaluation of Concentrated and Uniformly
    Distributed Loads for Pavement Design

2
Objectives
  • Analyze incremental stress at a given point in
    the subsurface due to external load on soil

3
Pavement Design
  • Types of pavement
  • soil
  • soil-cement
  • asphalt (flexible) - multi-layered system
  • concrete (rigid)

4
Shear Strength
  • Coulomb Equation
  • s c s tan f
  • c 0 cohesionless soils (sand, gravel)
  • f 0 cohesive soils (clay)
  • Cohesion unconfined compressive strength
  • c qu/2

5
Analysis of Vertical Pressure Beneath
Concentrated Load
  • Approximate Method
  • Elastic Theory
  • Westergaard Equation (1938)
  • alternating layers of elastic and nonelastic
    material
  • Boussinesq Equation (1885)
  • homogeneous, isotropic soil
  • Influence Charts

6
Westergaard Theory
  • q vertical stress increment at depth z this is
    in addition to prior stress (overburden pressure)
  • Q concentrated load
  • r horizontal distance from point of application
    of Q to the point at which q is desired
  • m Poissons Ratio (strain normal to applied
    stress strain parallel to applied stress)

7
Westergaard Equation
  • To simplify analysis, use Poissons Ratio (m)
    0, that is, if lateral strain 0 then no bulging
    of the soil occurs

8
Boussinesq Equation
  • Generally, more widely used for analysis
  • At low ratios of r/z, this will yield a greater
    vertical stress increment than Westergaards
    method

9
Example
  • A concentrated 250 ton load is applied to the
    ground surface. Find the vertical stress
    increment
  • at 20 feet below the load
  • at 20 feet deep and 16 feet from the line of the
    load

10
Uniform LoadApproximate Method
  • Simply assumes that the horizontal area of stress
    increases linearly with depth

L
B
Q
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