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Shear Strength of Cohesive (Clay) Soil

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Shear Strength of Cohesive (Clay) Soil Introduction Soil failure usually occurs in the form of shearing along internal surface within the soil. – PowerPoint PPT presentation

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Title: Shear Strength of Cohesive (Clay) Soil


1
Shear Strength of Cohesive (Clay) Soil
2
Introduction
  • Soil failure usually occurs in the form of
    shearing along internal surface within the
    soil.
  • Thus, structural strength is primarily a function
    of shear strength.
  • Shear strength is a soils ability to resist
    sliding along internal surfaces within the soil
    mass.

3
Slope Stability Failure is an Example of
Shearing Along Internal Surface
4
Mass Wasting Shear Failure
5
Shear Failure Earth Dam
6
Shear Failure Under Foundation Load
7
What is Shear Strength?
  • Shear strength in soils is the resistance to
    movement between particles due to physical bonds
    from
  • Particle interlocking
  • Atoms sharing electrons at surface contact points
  • Chemical bonds (cementation) such as crystallized
    calcium carbonate

8
Influencing Factors on Shear Strength
  • The shearing strength, is affected by
  • soil composition mineralogy, grain size and
    grain size distribution, shape of particles, pore
    fluid type and content, ions on grain and in pore
    fluid.
  • Initial state State can be describe by terms
    such as loose, dense, overconsolidated, normally
    consolidated, stiff, soft, etc.
  • Structure Refers to the arrangement of particles
    within the soil mass the manner in which the
    particles are packed or distributed. Features
    such as layers, voids, pockets, cementation, etc,
    are part of the structure.

9
Shear Strength of Soil
  • In reality, a complete shear strength formulation
    would account for all previously stated factors.
  • Soil behavior is quite complex due to the
    possible variables stated.
  • Laboratory tests commonly used
  • Direct Shear Test
  • Unconfined Compression Testing (TODAYS LAB)

10
  • Since so many variable do exist, the Mohr-Coulomb
    failure criterion is the most common failure
    criterion used in soil mechanics.
  • The Mohr-Coulomb criterion defines shear
    strength
  • S c sµ
  • c is strength due to cohesion (cqu/2)
  • qu is unconfined compressive strength
  • sµ strength due to friction (zero for clays).
    This term applies to sand/granular materials

11
Shear Strength of Cohesive Soils
  • S c sµ
  • cqu/2 and since we have a cohesive soil, sµ
    can be assumed zero.
  • We can determine S by the unconfined compressive
    test and yield
  • S c qu/2
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