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Cluster evolution in steady-state two-phase flow in porous media
1Department of Physics, Norwegian University of Science and Technology, N-7491 Trondheim, Norway. Thomas.Ramstad@phys.ntnu.no
Summary
Numerical simulations reveal that in porous media, nonwetting fluid clusters exhibit a power-law distribution at critical saturation. This finding is crucial for understanding two-phase flow dynamics and cluster development.
Area of Science:
- Physics
- Earth Sciences
- Chemical Engineering
Background:
- Two-phase flow in porous media is fundamental to processes like oil recovery and CO2 sequestration.
- Understanding cluster development is key to predicting fluid distribution and transport.
- Previous models often simplified the complex dynamics of initial transients and steady-state evolution.
Purpose of the Study:
- To numerically investigate the cluster development of two-phase flow in porous media under steady-state conditions.
- To analyze the influence of capillary forces on cluster formation and distribution.
- To characterize the statistical properties of nonwetting fluid clusters.
Main Methods:
- Utilized a two-dimensional flow simulator incorporating biperiodic boundary conditions.
- Simulated initial transients and their evolution towards a steady state.
- Focused on capillary-dominated flow regimes with capillary numbers around 10(-5).
Main Results:
- Observed a crossover phenomenon where initial patterns break up before reaching steady state.
- Identified a power-law distribution (ns ~ s^(-tau)) for nonwetting cluster sizes near critical saturation, with tau = 1.92 ± 0.04.
- The determined exponent is lower than that found in ordinary percolation theory.
- Presented scaling relations and time evolution data for cluster structure and global pressure.
Conclusions:
- The study provides critical insights into the statistical mechanics of two-phase flow in porous media.
- The power-law distribution suggests scale-invariant properties of nonwetting clusters at critical saturation.
- Findings contribute to a more accurate modeling of fluid dynamics in geological formations and engineered systems.