1887
Volume 39 Number 2
  • E-ISSN: 1365-2478

Abstract

A

Permeability is a second rank tensor relating flow rate to pressure gradient in a porous medium. If the permeability is a constant times the identity tensor the permeable medium is isotropic; otherwise it is anisotropic. A formalism is presented for the simple calculation of the permeability tensor of a heterogeneous layered system composed of interleaved thin layers of several permeable constituent porous media in the static limit. Corresponding to any cumulative thickness of a constituent is an element consisting of scalar and a matrix which is times a hybrid matrix function of permeability. The calculation of the properties of a medium equivalent to the combination of permeable constituents may then be accomplished by simple addition of the corresponding scalar/matrix elements. Subtraction of an element removes a permeable constituent, providing the means to decompose a permeable medium into many possible sets of permeable constituents, all of which have the same flow properties. A set of layers of a constituent medium in the heterogeneous layered system with permeability of the order of as → 0, where is that constituent's concentration, acts as a set of infinitely thin channels and is a model for a set of parallel cracks or fractures. Conversely, a set of layers of a given constituent with permeability of the order of as → 0 acts as a set of parallel flow barriers and models a set of parallel, relatively impermeable, interfaces, such as shale stringers or some faults. Both sets of channels and sets of barriers are defined explicitly by scalar/matrix elements for which the scalar and three of the four sub‐matrices vanish. Further, non‐parallel sets of channels barriers can be ‘added’ and 'subtracted’ from a background homogeneous anisotropic medium commutatively and associatively, but not non‐parallel sets of channels barriers reflecting the physical reality that fractures that penetrate barriers will give a different flow behaviour from barriers that block channels. This analysis of layered media, and the representations of the phenomena that can occur as the thickness of a constituent is allowed to approach zero, are applicable directly to layered heat conductors, layered electrostatic conductors and layered dielectrics.

Loading

Article metrics loading...

/content/journals/10.1111/j.1365-2478.1991.tb00310.x
2006-04-27
2024-04-26
Loading full text...

Full text loading...

References

  1. Backus, G.1990. Review of a note by Hudson, J.A. and Crampin, S. submitted to Geophysics .
  2. Biot, M.A.1956. Theory of elastic waves in a fluid‐saturated porous solid. I. Low‐frequency range. Journal of the Acoustical Society of America28, 168–178.
    [Google Scholar]
  3. Crampin, S.1984. Effective anisotropic elastic constants for wave propagation through cracked solids. Geophysical Journal of the Royal Astronomical Society76, 135–145.
    [Google Scholar]
  4. Helbig, K. and Schoenberg, M.1987. Anomalous polarization of elastic waves in transversely isotropic media. Journal of the Acoustical Society of America81, 1235–1245.
    [Google Scholar]
  5. Nichols, D., Muir, F. and Schoenberg, M.1989. Elastic properties of rocks with multiple sets of fractures. 59th SEG meeting, Dallas, Expanded Abstracts, 471–474.
  6. Schoenberg, M. and Muir, F.1989. A calculus for finely layered anisotropic media. Geophysics54, 581–589.
    [Google Scholar]
  7. Schoenberg, M. and Sen, P.N.1987. Permeability and velocity in simple modes with compressible fluids. Journal of the Acoustical Society of America82, 1804–1810.
    [Google Scholar]
http://instance.metastore.ingenta.com/content/journals/10.1111/j.1365-2478.1991.tb00310.x
Loading
  • Article Type: Research Article

Most Cited This Month Most Cited RSS feed

This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error