Nonlinear interactions of phase separation and viscous fingering in radial Hele–Shaw flow

We investigate the coupled dynamics of viscous fingering (VF) and phase separation (PS) in a radial Hele–Shaw flow. Using a combination of linear stability analysis (LSA) and nonlinear simulations (NLS), we analyze how the initial concentration of injected fluid (ci) and viscosity contrast (R) determine the dominant instability mechanism. VF arises when a less viscous fluid displaces a more viscous one, i.e., R>0. In comparison, PS is quantified by parameter Θ, which is defined as the negative of the second derivative of free energy and depends on both miscibility and ci. A positive Θ indicates thermodynamic instability within the spinodal region, driving PS; otherwise, it is a metastable region. For R>0, PS dominates at low R, producing droplet or ring-like morphologies with limited influence from viscosity contrast. However, at higher R, ci determines the dominant mechanism: VF dominates for ci>0.5, while PS remains dominant for ci≤0.5. We construct a pattern diagram between effective viscosity contrast and Θ that classifies the different regimes and identifies regions where both mechanisms interact. These nonlinear patterns are consistent with the LSA predictions. The LSA reveal that viscosity contrast controls the onset and nature of instability: for R<0, the onset is delayed, whereas R>0 accelerates onset through the combined action of PS and VF. The strong agreement among NLS, LSA, and experimental observations confirms the robustness of our framework. This also validates the novel LSA approach developed here for partially miscible displacements, with direct relevance to transport in porous media.

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Publication Details

Journal
Physics of Fluids
Published
2025-12-01
DOI
https://doi.org/10.1063/5.0305215
Citations
1
Primary Topic
CO2 Sequestration and Geologic Interactions
Type
article
Field-Weighted Citation Impact
0.80
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article

Nonlinear interactions of phase separation and viscous fingering in radial Hele–Shaw flow

Priya Verma, Ching-Yao Chen, Chun-Pei Liao
1 citations
Physics of Fluids
CO2 Sequestration and Geologic Interactions
0.80
article

Nonlinear interactions of phase separation and viscous fingering in radial Hele–Shaw flow

Priya Verma, Ching-Yao Chen, Chun-Pei Liao
article en
1 citations

Abstract

We investigate the coupled dynamics of viscous fingering (VF) and phase separation (PS) in a radial Hele–Shaw flow. Using a combination of linear stability analysis (LSA) and nonlinear simulations (NLS), we analyze how the initial concentration of injected fluid (ci) and viscosity contrast (R) determine the dominant instability mechanism. VF arises when a less viscous fluid displaces a more viscous one, i.e., R>0. In comparison, PS is quantified by parameter Θ, which is defined as the negative of the second derivative of free energy and depends on both miscibility and ci. A positive Θ indicates thermodynamic instability within the spinodal region, driving PS; otherwise, it is a metastable region. For R>0, PS dominates at low R, producing droplet or ring-like morphologies with limited influence from viscosity contrast. However, at higher R, ci determines the dominant mechanism: VF dominates for ci>0.5, while PS remains dominant for ci≤0.5. We construct a pattern diagram between effective viscosity contrast and Θ that classifies the different regimes and identifies regions where both mechanisms interact. These nonlinear patterns are consistent with the LSA predictions. The LSA reveal that viscosity contrast controls the onset and nature of instability: for R<0, the onset is delayed, whereas R>0 accelerates onset through the combined action of PS and VF. The strong agreement among NLS, LSA, and experimental observations confirms the robustness of our framework. This also validates the novel LSA approach developed here for partially miscible displacements, with direct relevance to transport in porous media.

Physics of FluidsVol. 37(12)
National Yang Ming Chiao Tung University (TW)
Openalex Percentile: Top 22%
CO2 Sequestration and Geologic Interactions
0.80
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