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| Schoenberg's angle on fractures and anisotropy: A study in orthotropy | |
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Another model in a very similar context that has been discussed frequently
by Schoenberg and Helbig (1997), Bakulin et al. (2000), and others is
the model of a VTI earth system (where the background elastic medium is
transversely isotropic with vertical axis of system, as it would be in a
layered earth model having isotropic layers [Backus (1962)]) with superposed vertical fractures.
A result that is often quoted in this context concerns a condition
that is necessarily satisfied by the elastic stiffness matrix elements
for such a system:
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(10) |
Using the same ideas applied here already, we can reduce this
equation to a simple statement about the system compliances. The
resulting statement is the formula:
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(11) |
by which we mean to say that the only requirement imposed
on the compliances after the introduction of the vertical
fractures to the VTI earth background is that the new overall
system compliance must satisfy the conditions
in (11) after the changes due to the fractures are
included in the values of these two compliance components.
No other special constraints appear.
To see that (11) is the correct condition, note
that
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(12) |
where is the determinant of the upper left
sub-matrix of the orthotropic stiffness matrix .
Equating these two expressions from (12) and
rearranging the final result gives a
formula that is precisely the same condition (10) given by Schoenberg and Helbig (1997).
What this condition implies for the physical system -- since
the background earth medium is assumed to be VTI with vertical axis
of symmetry and also since
for the background medium
itself (before the fractures are added to it) --
is that our final result must be the condition:
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(13) |
This very simple equality means the changes (i.e., increases)
in these off-diagonal compliances -- when due to the addition of the vertical fractures
to this model -- have just one constraint, and that single constraint is
that changes in these two off-diagonal compliances and
must occur in unison. This result is also seen as a limiting case found
in Table 1, when , which occurs only when .
Since means that all the vertical fractures are parallel,
and therefore being all aligned fractures, I therefore then have exactly the case
studied explicitly by Schoenberg and Helbig (1997).
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| Schoenberg's angle on fractures and anisotropy: A study in orthotropy | |
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Next: DISCUSSION OF VARIOUS FRACTURE
Up: Berryman: Fractures and anisotropy
Previous: VANISHING OF THE ANELLIPTICITY
2009-10-19