1887

Abstract

Matrix pore water in the connected inter-and intragranular pore space of low-permeable crystalline bedrock interacts with flowing fracture groundwater predominately by diffusion. The amount of pore water in the rock matrix and the volume of gas dissolved

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/content/papers/10.3997/2214-4609.20144139
2011-11-08
2024-04-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20144139
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