Abstract
The effect of admixture diffusion on the process of precipitation during solution evaporation in high-temperature low-permeability rocks is investigated. It is found that at permeabilities lower than 0.01 mD the two-valued solution is restructured becoming single-valued. As a result, during salt precipitation in low-permeability rocks where admixture diffusion is important, a solution exists for any flow regime and the channels in the porous medium are not blocked by solid-phase salt.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.