Multiphase flow and reactive transport are two essential physicochemical processes that
govern the effectiveness of geological carbon sequestration (GCS). The interaction and …

Due to the complexity of sedimentary rocks, especially the fine-grained and highly-
heterogeneous nature of some argillaceous caprocks in the subsurface, it is challenging to …

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

Considering the importance of carbon neutrality, UCCUS which is underground carbon
capture, utilization, and storage has been widely adopted to mitigate climate change …

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 …

Fluid‐rock dissolution occurs ubiquitously in geological systems. Surface‐volume scaling is
central to predicting overall dissolution rate R involved in modeling dissolution processes …

Understanding geochemical dissolution in porous materials is crucial, especially in
applications such as geological CO2 storage. Accurate estimation of reaction rates …

Reactive transport processes in porous media with dissolution of solid structures are widely
encountered in scientific and engineering problems. In the present work, the reactive …

In multi‐mineral fractured rocks, the altered porous layer on the fracture surface resulting
from preferential dissolution of the fast‐reacting minerals can have profound impacts on …

The dissolution dynamics of rough channels is a fundamental issue involved in widening
fracture channels (cavity evolution), solution mining, and upscaling of dissolution rate …