Toward the Understanding of Stress-Induced Mineral Dissolution via Molecular Scale Simulations

Abstract

Stress-induced mineral dissolution at contacts is a critical geophysical process in a broad spectrum of phenomena such as earthquake slip weakening, petroleum migration, and rock deformation. However, there is limited understanding of how this geophysical process originates from the grain-to-grain contacts on a nanoscale. In this study, we simulated the contact process of two quartz asperities in water and present a specially designed molecular dynamics (MD)-based scheme to quantify the dissolution tendency at contacts. Our results suggest that a water layer between the two asperities persists even when the quartz crystals are highly deformed. The MD simulation allowed us to evaluate the the..