Micro‐continuum models are versatile and powerful approaches for simulating coupled
processes in two‐scale porous systems. Initially oriented for modeling static single‐phase …

The traditional model of solid dissolution in porous media consists of three dissolution
regimes (uniform, compact, wormhole)—or patterns—that are established depending on the …

Traditional approaches for transport in porous media rely on empirical hydrodynamic/
transport parameters to quantify the interfacial exchange terms between fluid and solid …

Fractures are ubiquitous in geological systems. As reactive fluid flow through a fracture,
dissolution of the fracture walls may occur, thus altering the fracture aperture and increasing …

The micro-continuum method is a novel approach to simulate flow and transport in
multiscale porous materials. For such materials, the domain can be divided into three sub …

Traditional approaches to mathematically describe spontaneous imbibition are usually
based on either macro-scale models, such as Richards equation, or simplified pore-scale …

The formation of new mineral phases in confined environments, especially in porous media,
is crucial for various geological processes like mineralization and diagenesis. The …

Understanding flow and transport in multiscale porous media is challenging due to the
presence of a wide range of pore sizes. Recent imaging advances offer high-resolution …

The dissolution of minerals within rock fractures is fundamental to many geological
processes. Previous research on fracture dissolution has highlighted the significant role of …

Dissolution in porous media is widespread in natural and engineered systems,
accompanied by the evolution of geometric structure, permeability and surface area of the …