The direction of \(\sigma_2\) is usually along the fault plane
\( \sigma_1 \) is vertical (as stated in the problem)
\( \sigma_3 \) is horizontal (as stated in the problem)
\(\theta \) is the angle from the horizontal (same as the dip) for *this* problem. See figure P10.1 for help.
\(\sigma_n = \dfrac{\sigma_1 + \sigma_3}{2} + \dfrac{\sigma_1 - \sigma_3}{2} \cos (2\theta)\)
\(\sigma_s = \dfrac{\sigma_1 - \sigma_3}{2} \sin (2\theta)\)
Plot the normal and shear stress on the graph provided in P10.1
Plot the Mohr Circle with \( \sigma_1 = 100 MPa\) and \( \sigma_3 = 20 MPa\)
Oh that is a lot of text
Plot the Mohr Circle for the regional stress state \( \sigma_1 = 10 Mpa \) and \( \sigma_3 = 6 MPa \)
Draw a Failure envelope with \( \mu = 0.4 \) (the slope) and a Cohesion \( C = 0 \)
\( \sigma_s = \mu \sigma_1 + C \) (form of \( y= mx + b \) )
Shift the Mohr circle until it intersects with the Failure envelope. This is the same as increasing the pore fluid pressure or subtracting some pressure from the normal stresses
How far you moved the circle is the Pore fluid pressure
Problem 10.2
Problem 10.3
This is similar to Problem 10.1 with different normal stress values and fault dip
Problem 10.5
Problem 10.9