Although many geochemical processes, including mineral dissolution, ar
e controlled by kinetic mechanisms, quantitative descriptions of the r
eaction kinetics are mostly lacking, principally due to an incomplete
understanding of the molecular-scale processes controlling these react
ions. In this paper, a combined experimental and theoretical approach
involving atomic force microscopy, an analytical terrace-ledge-kink mo
del, and kinetic Monte Carlo computer simulations was used to study th
e aqueous dissolution kinetics of the calcite (<10(1)over bar 4>) surf
ace. The study provides a determination of the elementary rates and ac
tivation energies associated with dissolution at specific kink sites o
n the calcite surface.