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Abstract

Tube waves propagating in the boreholes are used for the investigation of permeable zones and of fluid transport in porous rocks (Aidinov, 1994). It is known that in a permeable interfal a clay coating and colmatage zone are often formed. We study effects of these factors on the velocity and attenuation of a tube wave by means of an experimental and theoretical treatment.

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/content/papers/10.3997/2214-4609.201409523
1995-05-29
2022-06-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409523
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