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EVOLUTION IN PERMEABILITY IN SILICEOUS ROCKS INDUCED BY MINERAL DISSOLUTION AND PRECIPITATION (2009)
A conceptual model is presented to follow the evolution of permeability in siliceous rocks mediated by pressure solution comprising the serial processes of interfacial dissolution, diffusion, and free-face precipitation.
Reference:
International Journal of the JCRM vol.5 (2009) pp.83-85
International Journal of the JCRM vol.5 (2009) pp.83-85
Organization:
Member of ISRM: Dept. of Civil and Environmental Engineering, Ehime University, 3, Bunkyo-cho, Matsuyama 790-8577 Japan
Member of ISRM: Dept. of Civil and Environmental Engineering, Ehime University, 3, Bunkyo-cho, Matsuyama 790-8577 Japan
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