Integration of in situ profilometry and simulations reveals fractal dimension and capillary number control gas trapping efficiency.
Gas–water displacement in rough fractures critically influences unconventional energy recovery, yet current models fail to quantify geometry-fluid-inertia coupling mechanisms that govern trapping efficiency. To resolve this, we integrate in situ profilometry and multiphysics simulations to decipher how fractal dimension (D) and capillary number (Ca) control two-phase dynamics in Qinshui Basin coal fractures. Key discoveries reveal: (1) Residual gas fraction follows a Boltzmann distribution with Ca, exhibiting a sensitive transition zone (10−2 < Ca < 10−1) where trapping surges by 18%–28%; (2) increasing D from 1.5 to 1.72 elevates residual gas by 28.5% and prolongs breakthrough via power-law scaling (R2 > 0.98); and (3) aperture transitions reduce hydraulic apertures by 13%–28% through capillary-driven fingering. These quantified mechanisms provide a predictive framework for optimizing gas recovery in fracture-dominated reservoirs.
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Ge et al. (2025) studied this question.
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