Pore‐Scale Transition Behavior of Digital Carbonate Rock Dissolution During CO2 Geo‐Sequestration

Abstract Carbon dioxide‐rich brine formation during geological carbon sequestration induces calcite dissolution, governed by the physicochemical coupling of fluid flow, reactive transport, and pore structure evolution. Unveiling the mechanisms that control this dissolution, particularly under varyin...

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Detalhes bibliográficos

Principais autores:	Qiuheng Xie, Senyou An, Heping Xie, Wendong Wang, Vahid Niasar
Formato:	Artigo
Idioma:	Inglês
Publicado em:	Wiley 2026-02-01
Colecção:	Water Resources Research
Assuntos:	reactive transport dissolution regime CO2 sequestration volumetric LBM
Acesso em linha:	https://doi.org/10.1029/2025WR041604
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