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Using borehole electroseismic measurements to detect and describe permeable zones

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Author(s)
Imomnazarov Kholmatzhon,
Imomnazarov Bakhodirzhon
Abstract

Formulas for the modified Darcy and Ohm laws are obtained. The diffusion coefficient is shown to be a function of the conductivity of the liquid, elastic porous body, and electrokinetic coefficient. A formula for the determination of porosity is obtained.

File
imomnazarov.pdf4.9 MB
Issue
Mathematical Modeling in Geophysics, № 8, 2003
Pages
47-57
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    • About
      • Journal
      • Editorial
      • ISSN
    • Series
      • Computer Science
      • Mathematical Modeling in Geophysics
      • Numerical Analysis
      • Numerical Modeling in Atmosphere, Ocean, and Environment Studies
    • Search
    • Authors
    • Submission
    • Contacts
    • Search