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For random polycrystals (see the earlier discussion of the basic
model in the second section), it is most convenient to define a new
canonical function:
| ![\begin{displaymath}
\Sigma_X(s) = \left[\frac{1}{3}\left(\frac{1}{\sigma_H+2s}
+ \frac{2}{\sigma_M+2s}\right)\right]^{-1} - 2s,
\end{displaymath}](img116.gif) |
(36) |
where the mean
and harmonic mean
of the layer constituents are the pertinent conductivities (off-axis
and on-axis of symmetry, respectively) in each layered grain. Then, the
Hashin-Shtrikman bounds for the conductivity of the random polycrystal are
| ![\begin{displaymath}
\sigma_{HSX}^\pm = \Sigma_X(\sigma_\pm),
\end{displaymath}](img119.gif) |
(37) |
where
and
.These bounds are known not to be the most general ones since they rely
on an implicit assumption that the grains are equiaxed.
A more general lower bound that is known to be optimal is due to Schulgasser
(1983) and Avellaneda et al. (1988):
| ![\begin{displaymath}
\sigma_{ACLMX}^- = \Sigma_X(\sigma_{ACLMX}^-/4).
\end{displaymath}](img122.gif) |
(38) |
Helsing and Helte (1991) have reviewed the state of the art for
conductivity bounds for polycrystals, and in particular have noted
that the self-consistent
[or CPA (i.e., coherent potential approximation)]
for the random polycrystal conductivity is given by
| ![\begin{displaymath}
\sigma_{CPAX}^* = \Sigma_X(\sigma_{CPAX}^*).
\end{displaymath}](img123.gif) |
(39) |
It is easy to show (39) always lies between the two rigorous bounds
and
, and also between
and
. Note that
and
cross when
, with
becoming the superior lower bound for mean/harmonic-mean
contrast ratios greater than 10.
Next: Comparisons of conductivity bounds
Up: CONDUCTIVITY: CANONICAL FUNCTIONS AND
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Stanford Exploration Project
5/3/2005