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Abstract

The aim of this paper is to discuss whether or not solubilisation of-gases in water and subsequent diffusion can be considered as a migration proces. We give first an example where geological and geochemical data may be interpreted as the result of a diffusion leakage. Second, the diffusion of gases through argilleous caprock has been studied with an experimental cell coupled with a numerical model. Lastly, the numerical model for this experiment has been extended and applied to the geological example.

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/content/papers/10.3997/2214-4609.201409640
1995-05-29
2024-10-03
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/content/papers/10.3997/2214-4609.201409640
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