FINAL Flashcards
Mohr Circle
Normal Stress on x axis
Shear Stress on y axis
Principle Stress
Points at which there is zero shear stress
Sign convention for mohrs circle
Compression = Positive Counterclockwise = Positive
Stresses acting on a vertical plane
Draw a vertical line through the origin of planes
Orientation of Principle Planes
Draw line from Op to the major and minor points
Draw element on same line
Factors that affect strength of soils
Effective Stress
Density
Rate of Shearing
Nature of Stress Change
Mohr-Coulomb Failure Criterion
Failure occurs because of a critical combination of normal stress and shearing stress
On or under the failure envelope
If the circle is tangent to fail envelope then it has reach full strength
Failure does not have to fail at max shear stress (its a combo with normal)
๐ = ๐โ tan (ษธ) + c
Direct Shear Test
Soil in box split across middle
Confining force and constant rate of displacement
Shear force and change in height recorded
Non-uniform failure surface
Direct shear on loose sand
Shear increases with shear displacement until a failure shear stress is reached
After fail, shear resistance is constant
Loose sand shows a gradual decrease in volume
Larger confining stress, the larger the max shear stress
Direct Shear on dense sand
Shear increases with shear displacement until a failure shear stress is reached and then decreases to the critical state
Volume decreases at first and starts to increase after max shear
Dense soil provides additional resistance to sliding so its โstrongerโ
Larger confining stress, the larger the max shear stress
Friction angle is larger in dense soils
Very dense tends to act like loose
Confining State Friction Angle
tan ษธโcs = ฯr / ๐ โ
once the peak strength is hit and the displacement grows
Loose = 28-38
Dense = 35-45
Dilation
Change in volume
The lower the normal stress the more dilation
The higher the confining stress, the less diliant
Critical State
The same soil and confining stress, the same final residual shear stress no matter if loose or dense
Angle of Repose
Friction angle of sand at its loosest state