
doi: 10.2118/80391-ms , 10.2523/80391-ms
Abstract As water migrates through porous rock, any changes in pressure or temperature, as well as changes in fluid composition, may lead to changes in the solubility of dissolved minerals. We examine the reactions which may develop in such a system, following the injection of water of one temperature and composition into a reservoir with different temperature and equilibrium composition. We examine the structure of pressure, temperature and compositionally induced reactions.
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