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Abstract

Movement of the fluids, saturating porous media of the real reservoirs,can be, in many cases, especially by miscible displacement, considered as a dispersion process.This process may be caused not only by molecular and convective diffusion, but as weIl by strata heterogeneity. As examples, solutions of the dispersion equation for layered and fractured-porous reservoirs are given. On the base of this solutions inverse method is developed, which permits to evaluate heterogeneous strata properties.

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/content/papers/10.3997/2214-4609.201406907
1996-09-03
2021-06-22
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201406907
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