Pore-scale DNS shows intermittency as a network-coupled process of drainage-imbibition cycles that enhances overall fluid mobility and produces the sub-linear macroscopic scaling regime.
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Intermittent two-phase flow in porous media: insights from pore-scale direct numerical simulation
Pore-scale DNS shows intermittency as a network-coupled process of drainage-imbibition cycles that enhances overall fluid mobility and produces the sub-linear macroscopic scaling regime.