Rock fractures are ubiquitous in the crust of the Earth. Because of their high permeability, fractures usually provide the main pathways for fluid flow and control fluid migration in geological systems (Igonin et al., 2021). When the flowing fluid is reactive, the dissolution of minerals within fracture walls would expand the fracture aperture and form distinct dissolution patterns. These dissolution patterns determine how the dissolved region develops and how the permeability increases (Roded et al., 2018;Wang & Cardenas, 2017). Understanding and quantifying the dissolution patterns in rough fractures is fundamental to many natural settings and engineering applications, including the evolution of karst hydrology (