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Updated: Feb 3, 2026

Pore-scale Imaging and Characterization of Hydrocarbon Reservoir Rock Wettability at Subsurface Conditions Using X-ray Microtomography
Published on: October 21, 2018
X-ray Microtomography of Intermittency in Multiphase Flow at Steady State Using a Differential Imaging Method
Ying Gao1,2, Qingyang Lin1, Branko Bijeljic1,2
1Department of Earth Science and Engineering Imperial College London London UK.
We studied fluid flow in sandstone using differential imaging. At higher flow rates, we observed intermittent fluid occupancy, revealing new insights into oil and brine flow dynamics and connectivity.
Area of Science:
- Geosciences
- Petroleum Engineering
- Fluid Dynamics
Background:
- Understanding multiphase flow in porous media is crucial for oil recovery and carbon sequestration.
- Pore-scale fluid distribution significantly impacts macroscopic flow properties like relative permeability.
Purpose of the Study:
- To investigate the impact of flow rate on pore-scale fluid distribution during brine and decane coinjection in Bentheimer sandstone.
- To elucidate flow regimes and dynamic connectivity of non-wetting phases at different capillary numbers (Ca).
Main Methods:
- Developed a differential imaging technique to visualize fluid distribution at the pore scale.
- Conducted experiments at two capillary numbers (3.0 × 10⁻⁷ and 7.5 × 10⁻⁶) across various fractional flows.
- Measured pressure drops using high-precision sensors and analyzed fluid occupancy using image histogram distribution.
Main Results:
- At low Ca, fluids flowed in stable, connected subnetworks, aligning with conventional theory.
- At high Ca, observed intermittent occupancy of pore space by oil and brine, crucial for explaining dynamic oil phase connectivity.
- Non-wetting phase pathways did not always span the core, indicating segmented flow at higher Ca.
Conclusions:
- The study reveals distinct flow regimes at different capillary numbers, challenging conventional assumptions at higher flow rates.
- Intermittent fluid occupancy is a key mechanism for dynamic connectivity of non-wetting phases in porous media.
- Experimental results at the mm-scale show good agreement with literature data from cm-scale samples, validating the method.
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