Hydrology within fractured rocks is complex, with variable Péclet conditions reflecting the relative importance of fluid advection and diffusion on the movement of solutes. In many of these systems, the fluids passing through the fractures will be out of equilibrium with the resident minerals, and, in turn, a variety of reactions, for example, dissolution and precipitation, take place (Deng & Spycher, 2019). These geochemical processes can lead to the evolution of the fracture network by changing fracture permeability (Ellis et al., 2013) and potentially driving or inhibiting fracture propagation (Shovkun & Espinoza, 2019). Because the majority of flow in fractured media passes through a small volume relative to the domain size and the reactions are therein localized, these changes can produce a