CLASS
4: MOHRS CIRCLE
Mohrs Circle- developed by Otto Mohr (1835-1918).
a convenient graphical means to depict states of stress;
A force applied to an area (stress) may be resolved into a
normal force (Fn) perpendicular to a plane and a
shear force (Fs) , parallel to a plane in questions.
1 Sigma
1- Maximum Compressive Stress
2
Sigma 2- Intermediae Compressive Stress
3
Sigma 3- Minimum Compressive Stress
Stress is a vector quantity that can be considered as:
n
Normal Stress-
oriented perpendicular to a plane
s
Shear Stress-
oriented parallel to a plane in question
Theta- angle formed by an inclined plane with the maximum and minimum
compressive stress directions, and measured from the minimum stress position.
Important Normal Stress and Shear Stress Equations:
sn= (s1+s3) + (s1-s3) cos 2q
2 2
ss= (s1-s3) sin 2q
2
Importance of Mohrs Diagram:
1.For
any value of maximum compressive stress value and minimum compressive stress
value,
one can determine the normal and shear stress for any planes that lie
2.Depicts the attitude of planes along which shear stress is the greatest for a given stress state
3. The
most important aspect of Mohrs diagram is that it facilitates a quick,
graphical determination of stresses on planes of any orientation.
4.Mohr diagrams are excellent for visualizing the state of stress but difficult for calculating stress. Stress tensors are used to calculate stress.
PLOTTING MOHR'S CIRCLE:
Mohr's circle is plotted on two perpendicular axes: The vertical axis
(ordinate) depicts shear stress and the horizontal axis (abscissa) depicts
normal stress.
By convention compressive stress is positive (+) and
tensile stress is negative (-).

Principle Stresses sigma 1 (maximum compressive stress) and sigma 3 (minimum compressive stress) plot as two points on the horizontal axis. These two points define the diameter of a circle. The Circle is plotted on the abscissa

These points establish a radius (R) whereby:

The
center (C) is then plotted:

We can determine the normal and shear stress on any plane
oriented at an angle theta from the abscissa , as measured
counterclockwise from the minimum compressive stress
direction. Because of the properties of a circle, the angle
between Point P, the center of the circle and the maximum
compressive stress direction = 2 theta, as measured
counterclockwise from the center of the circle.

Mohrs Circle can graphically depict stress on any plane inclined
relative to the principal plane.
Normal and shear stresses can be determined graphically using
the circle or by using equations.

Differential stress, that is the difference between the maximum
and minimum compressive stress, is the most important factor in
rock fracturing
not
cause rock fracturing.
On a Mohrs Diagram, the following sense of shear conventions
apply:
Sinistral
(counterclockwise) shear is Positive
Dextral (clockwise) shear is Negative
Angles 2 theta associated with planes experiencing
sinistral shear plot in the upper
hemisphere.
Angles 2 theta associated with planes experiencing
dextral shear plot in the lower
hemisphere
Note that the axes of Mohrs diagram do not have a
geographic orientation.
However, prior to constructing a Mohrs diagram it is useful to
sketch a block diagram of the orientations of the principal
stress axes and the plane in question to ascertain the
relative sense of shear and orientation of principal stress axes
Mohrs
Envelop of Failure:
Represented by a straight line with a slope equal to Coulombs coefficient
A
number of Mohrs circles are plotted and a line tangential to the circles is
drawn
Constructed using a series of experiments in which the principal stresses
change.
Failure
occurs when the Mohrs circle intersects the envelope of failure
COULOMB'S COEFFICIENT
=
tan
(mu)
Coulomb�s Coefficient
(coefficient of internal friction
slope
of the line (envelop of failure)
(phi)
angle of internal friction
Coulomb Failure

MOHR'S CIRCLE DEPICTION OF:
EFFECTIVE STRESS & FLUID PORE PRESSURE-
Effective Stress= normal stress minus the pore fluid pressure.

Fluid
Pore Pressure (Pf)-
hydrostatic pressure exerted by interstitial water.
Mohr
circle remains same size but is translated to the left along
the horizontal axis.

Increase in Pf results in:
a reduction in the strength of the rock
facilitates hydraulic
fracturing.
Check out the following Webpage for Stress visualization: http://www.geology.sdsu.edu/visualstructure/vss/htm_hlp/index.htm
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