Quantitative predictions of natural and induced phenomena in fractured rock is one of the
great challenges in the Earth and Energy Sciences with far‐reaching economic and …

Geological carbon storage is one of the technologies required to arrive at the ambitious yet
realistic net-zero emission target and climate change neutrality. Injected CO 2 in geological …

Limestone pore structure strongly influences dissolution and associated reactive transport.
These effects are critical in limestone diagenesis and but also in engineering operations …

This third edition offers a comprehensive overview of the latest theories on flow, transport,
and heat-exchange processes in porous media. It also details sophisticated porous media …

Fluid–mineral and fluid–rock interfaces are key parameters controlling the reactivity and fate
of fluids in reservoir rocks and aquifers. The interface dynamics through space and time …

We investigate the dissolution of artificial fractures with three‐dimensional, pore‐scale
numerical simulations. The fluid velocity in the fracture space was determined from a lattice …

The roughness of solid surfaces influences mineral dissolution rates by affecting flow and
transport in the near-surface regions and by increasing the surface area available for …

We develop a 2‐D pore scale model of coupled fluid flow, reactive transport, and calcium
carbonate (CaCO3) precipitation and dissolution. The model is used to simulate transient …

Understanding how fracture wall-roughness affects fluid flow is important when modeling
many subsurface transport problems. Computed tomography scanning provides a unique …

Geochemical reactions may alter the permeability of leakage pathways in caprocks, which
serve a critical role in confining CO2 in geologic carbon sequestration. A caprock specimen …