Abstract
The complexity of pore geometry results in local variations of fluid velocity that affect the interplay between advective and diffusive transport. Dissolution rates are a function of the solute concentrations that are in direct contact with the mineral surfaces.
Chapter PDF
Similar content being viewed by others
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2023 The Author(s), under exclusive license to Springer Nature Switzerland AG
About this chapter
Cite this chapter
Molins, S., Trebotich, D. (2023). Pore-Scale Controls on Calcite Dissolution using Direct Numerical Simulations. In: Médici, E.F., Otero, A.D. (eds) Album of Porous Media. Springer, Cham. https://doi.org/10.1007/978-3-031-23800-0_112
Download citation
DOI: https://doi.org/10.1007/978-3-031-23800-0_112
Published:
Publisher Name: Springer, Cham
Print ISBN: 978-3-031-23799-7
Online ISBN: 978-3-031-23800-0
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)