Next: 9.3.5 Trace-free frictional stress
Up: 9.3 The stress tensor
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The presence of gravity provides a symmetry breaking from
three-dimensional isotropy down to transverse isotropy about the local
vertical direction .
It is important that the stress tensor
also respect this symmetry, which in turn provides constraints on the
form of the viscosity tensor.
In order to understand what transverse, or axial, isotropy imposes on
the viscosity tensor, it is necessary to recall that a fourth order
tensor transforms under a change of coordinates in the following
manner
|
= |
|
(9.29) |
Transverse isotropy means two things. First, the physical system
remains invariant under arbitrary rotations about the
direction, where
is the vertical direction.
Second, the physical system remains invariant under the
transformation
,
and
,
which is a transformation between two right handed
coordinate systems, with the vertical pointing up and down,
respectively. The transformation matrix for the rotational symmetry
takes the form of a rotation about the vertical
|
= |
|
(9.30) |
and the transformation matrix between right handed systems takes the
form
|
= |
|
(9.31) |
Imposing the constraint that
where
is one of the given
transformation matrices, provides for relations between the 21
remaining elements of Cabcd.
To determine the relations between the elements of Cabcd requires no more than careful enumeration of the possibilities. For
example, with a rotation angle of
about ,
rotational
symmetry implies
|
(9.33) |
However, the transformation between the two right handed coordinate
systems implies
These two results are satisfied only if
C1222 = C2111 = 0.
|
(9.35) |
For a rotation of ,
isotropy implies
|
(9.36) |
or
C1212 = (C1111 - C1122)/2.
|
(9.37) |
Continuing in this manner implies that the only nonzero elements of
Cijmn are Cijij, where ,
and Ciijj. The
relation between these nonzero elements can be written
|
= |
|
(9.38) |
and
C1212 |
= |
(c11 - c12)/2 |
(9.39) |
C2323 |
= |
C1313 = c44/2, |
(9.40) |
which brings to five the total number of independent degrees of
freedom.
Next: 9.3.5 Trace-free frictional stress
Up: 9.3 The stress tensor
Previous: 9.3.3 Dissipation of total
RC Pacanowski and SM Griffies, GFDL, Jan 2000