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Visualizing the stress tensor: Stress ellipse and Mohr circle
Adopting the principal stress axes as our reference system we know from
Equation 16 that the traction vector on any plane with normal
is
Since all normals
are assumed to have unit length, i.e.
, it follows
that the components of the traction vector lie on an ellipsoid with semi-axes
,
and
 |
(37) |
The stress ellipsoid, see Figure 5 left column, is a
convenient tool to easily visualize the orientations and magnitudes of the
principal stresses and hence the
prevalent faulting regime and the magnitude of the shearing stresses.
Figure:
Stress ellipsoids and Mohr circles for two stress tensors with
equal value of
. The upper tensor has
= 1.3,
= 1 and
= 0.8 and the lower tensor has
= 1.9,
= 1 and
= 0.4. Observe the difference in the shapes of the
stress ellipsoids but the identical shapes (except for a scale
factor) of the Mohr circle diagrams.
 |
The stress ellipsoid is, however, less convenient for showing the relationship
between the orientation of a plane in the stress field and the resulting
magnitudes of the normal and shear stresses upon it. To this respect we use
the Mohr circle diagram which, as we shall see, is very useful also in
the discussion of rock failure. I will not derive the angular relations for
the Mohr circle here, see e.g. Jaeger and Cook [1979], instead the relationship
between the normal to a fault plane and the normal, shear and principal
stresses are illustrated in Figure 6.
Figure:
Figure modified after Jaeger and Cook [1979].
A) One octant of the stress ellipsoid showing the definitions of the
angles
and
and the traces of two ellipses for
fixed values of
(GEH) and
(DEF).
B) The Mohr diagram corresponding to the stress ellipsoid in A.
 |
The angle between the
axis and the normal is denoted
and the angle between the
axis
and the normal is
. Using the equations for the magnitudes of the
normal and shear stresses, Equations 17 and 20, we
find that if one angle is kept fixed, varying the other angle traces out a
circle in
,
space. If we fix one angle in the plane of two
principal stresses, the three main circles in Figure 6B will be
traced out, e.g. for a fault normal in the
-
plane (
), Figure 6A, we have a circle centered on A
(normal stress
) in Figure 6B, with radius
. We see from Figure 6B that normal stress
for the circle varies from
to
and shear stress from 0 to
, as we expect. Setting
to any other angle will
trace out other circles centered on A, such as the DEF circle segment.
The largest of the three main circles traces out the stress magnitudes on
normals in the
-
plane. If desired, the Mohr circles can be
mirrored in the
axis to allow for negative shear stress magnitudes.
The space enclosed between the two smaller circles and the larger circle shows
the possible shear and normal stresses on any plane in the stress field.
Using the Mohr diagram we can
hence read off the normal and shear stress magnitudes for any value of
and
, i.e. any direction of the fault plane normal.
Comparing the stress ellipsoids and the Mohr diagrams in
Figure 5 we see that although the ratio
is often referred
to as the shape factor it does not describe the shape of the stress ellipsoid
but instead the position of the
point in the Mohr diagram.
reflects
how close
is to
or
, but it does not give any information
on the magnitude of (
-
), i.e. the size of the Mohr diagram. An
unscaled Mohr diagram can be constructed using only the directions of
the principal stresses and
. Although without information on the absolute
magnitude of the shear stress, such a diagram is valuable for the analysis of
the relative stability of fault planes, since the location of the fault plane
normal in the Mohr diagram only depends on the relative orientation of the
fault plane normal with respect to the principal stress axes.
Next: Rock fracture, friction and
Up: The Stress Tensor
Previous: Direction of horizontal stress
  Contents
Bjorn Lund
2000-06-14