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Abstract

Inclusion-based models are used to describe porous rocks and soils containing<br>immiscible contaminants. The results of modelling show that the functional relationship<br>between dielectric properties and the level of fluid saturation can vary significantly as the<br>pore-scale fluid distribution changes in terms of both the geometrical configuration and the<br>choice of wetting phase. The magnitude of these variations increases with decreasing<br>measurement frequency, indicating that the location of the conductive water phase is<br>important. The low frequency electrical conductivity depends on the connectivity of the<br>water phase. An inclusion-based model is used to compute the electrical stratigraphy of an<br>immiscible contaminant pooled at the water table interface.

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/content/papers/10.3997/2214-4609-pdb.209.1993_004
1993-04-18
2024-04-20
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.209.1993_004
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