Pore-scale synchrotron imaging of scCO2-brine intermittent flow: Experimental insights into multiphase dynamics for geological carbon storage

Underground carbon dioxide (CO 2 ) storage is a critical approach for mitigating climate change by sequestering CO 2 in deep geological formations. The interaction between injected super critical (sc) CO 2 and resident brine within pores results in complex two-phase flow dynamics that influence the efficiency and security of storage. While previous studies have mainly focused on capillary-dominated regimes, where fluid phases flow at low velocities, the transitional intermittent flow regime—characterised by higher flow rates and complex displacement dynamics—remains less understood. This study investigates the onset and development of intermittent flow pathways in CO 2 -brine systems through high-resolution synchrotron X-ray micro-computed tomography imaging of a carbonate rock sample. The core-flooding experiments were conducted under 8 MPa and 50 °C to examine pore-scale fluid configuration changes as a function of capillary number ( Ca ). The results indicate that intermittent flow emerges at lower Ca values than previously observed in oil-brine systems, with a distinct transition from Darcy flow to intermittent flow. Moreover, the saturation of the intermittent phase stabilises beyond a threshold Ca , suggesting another phase transition within the intermittent flow regime. These findings provide new insights into the fundamental mechanisms of two-phase flow dynamics at the pore scale, revealing a stable intermittent flow regime at higher flow rates, with potential implications for improved injectivity under non-equilibrium conditions. • First experimental visualisation of scCO 2 –brine intermittency using synchrotron X-ray micro-CT imaging in carbonate rock. • Intermittency saturation rises and levels off near 39% once Ca exceeds ∼1.77×10⁻⁷, marking a distinct flow-regime shift. • Intermittency thresholds match theory, supporting models for CO₂ injection planning and storage efficiency.

Authors

Institutions

Publication Details

Journal
Gas Science and Engineering
Published
2025-11-20
DOI
https://doi.org/10.1016/j.jgsce.2025.205806
Primary Topic
CO2 Sequestration and Geologic Interactions
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Pore-scale synchrotron imaging of scCO2-brine intermittent flow: Experimental insights into multiphase dynamics for geological carbon storage

Gioia Falcone, Amin Taghavinejad, Yihuai Zhang, Rukuan Chai et al.
Gas Science and Engineering
CO2 Sequestration and Geologic Interactions
article

Pore-scale synchrotron imaging of scCO2-brine intermittent flow: Experimental insights into multiphase dynamics for geological carbon storage

Gioia Falcone, Amin Taghavinejad, Yihuai Zhang, Rukuan Chai, Azibayam Josiah Amabogha
article en

Abstract

Underground carbon dioxide (CO 2 ) storage is a critical approach for mitigating climate change by sequestering CO 2 in deep geological formations. The interaction between injected super critical (sc) CO 2 and resident brine within pores results in complex two-phase flow dynamics that influence the efficiency and security of storage. While previous studies have mainly focused on capillary-dominated regimes, where fluid phases flow at low velocities, the transitional intermittent flow regime—characterised by higher flow rates and complex displacement dynamics—remains less understood. This study investigates the onset and development of intermittent flow pathways in CO 2 -brine systems through high-resolution synchrotron X-ray micro-computed tomography imaging of a carbonate rock sample. The core-flooding experiments were conducted under 8 MPa and 50 °C to examine pore-scale fluid configuration changes as a function of capillary number ( Ca ). The results indicate that intermittent flow emerges at lower Ca values than previously observed in oil-brine systems, with a distinct transition from Darcy flow to intermittent flow. Moreover, the saturation of the intermittent phase stabilises beyond a threshold Ca , suggesting another phase transition within the intermittent flow regime. These findings provide new insights into the fundamental mechanisms of two-phase flow dynamics at the pore scale, revealing a stable intermittent flow regime at higher flow rates, with potential implications for improved injectivity under non-equilibrium conditions. • First experimental visualisation of scCO 2 –brine intermittency using synchrotron X-ray micro-CT imaging in carbonate rock. • Intermittency saturation rises and levels off near 39% once Ca exceeds ∼1.77×10⁻⁷, marking a distinct flow-regime shift. • Intermittency thresholds match theory, supporting models for CO₂ injection planning and storage efficiency.

Gas Science and EngineeringVol. 145
Imperial College London (GB), University of Glasgow (GB)
Openalex Percentile: Top 67%
CO2 Sequestration and Geologic Interactions
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.