Differential effective medium modeling of rock elastic moduli with critical porosity constraints
Rocks generally have a percolation porosity at which they lose rigidity and fall apart. Percolation behaviour is a purely geometrical property, independent of any physical properties, and is a powerful constraint on any valid velocity-porosity relation. The authors show how the conventional Differential Effective Medium (DEM) theory can be modified to incorporate percolation of elastic moduli in rocks by taking the material at the critical porosity as one of the constituents of a two-phase composite. Any desired percolation porosity can be specified as an input. In contrast, the conventional DEM model always predicts percolation at a porosity of either 0 or 100 percent. Most sedimentary rocks however have intermediate percolation porosities and are therefore not well represented by the conventional theory. The modified DEM model incorporates percolation behavior, and at the same time is always consistent with the Hashin-Shtrikman bounds. The predictions compare favorably with laboratory sandstone data. 24 refs., 3 figs.
- Stanford Univ. CA (United States) [Stanford Univ. CA (United States)
- Lawrence Livermore National Lab., CA (United States) [Lawrence Livermore National Lab., CA (United States)
- Publication Date:
- OSTI Identifier:
- Resource Type:
- Journal Article
- Resource Relation:
- Journal Name: Geophysical Research Letters; Journal Volume: 22; Journal Issue: 5; Other Information: PBD: 1 Mar 1995
- Country of Publication:
- United States
- 36 MATERIALS SCIENCE; ROCKS; ELASTICITY; POROSITY; MATHEMATICAL MODELS
Enter terms in the toolbar above to search the full text of this document for pages containing specific keywords.