1887

Abstract

The hydrodynamical theory of the miscible displacement in fractured-porous media (FPM) that describes convective, gravitational, diffusive mechanisms of the recovery from blocks and hydraulic interaction between blocks and cracks is developed. The solution of the inverse problem is obtained to determine FPM properties from data from laboratory displacement.

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/content/papers/10.3997/2214-4609.201411212
1991-05-21
2020-08-12
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201411212
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