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Pore-Scale Lattice Boltzmann Modeling and 4D X-ray Computed Microtomography Imaging of Fracture-Matrix Fluid Transfer
Authors:C J Landry  Z T Karpyn  O Ayala
Institution:1. Bureau of Economic Geology, University of Texas at Austin, Austin, TX, USA
2. John and Willie Leone Family Department of Energy and Mineral Engineering, EMS Energy Institute, The Pennsylvania State University, University Park, PA, USA
3. Department of Engineering Technology, Old Dominion University, Norfolk, VA, USA
4. Centro de Métodos Numéricos en Ingeniería, Escuela de Ingeniería y Ciencias Aplicadas, Universidad de Oriente, Puerto La Cruz, Venezuela
Abstract:We present sequential X-ray computed microtomography (CMT) images of matrix drainage in a fractured, sintered glass-granule-pack. Sequential (4D) CMT imaging captured the capillary-dominated displacement of the oil-occupied matrix by the surfactant-brine-occupied fracture at the pore scale. The sintered glass-granule-pack was designed to have minimal pore space beyond the resolution of CMT imaging, ensuring that the pore space of the matrix connected to the fracture could be captured in its entirety. This provided an opportunity to validate the increasingly common lattice Boltzmann modeling technique against experimental images at the pore scale. Although the surfactant was found to alter the wettability of the originally weakly oil-wet glass to water-wet, the fracture-matrix fluid transfer is found to be a drainage process, showing minimal counter-current migration of the initial wetting phase (decane). The LB simulations were found to closely match experimental rates of fracture-matrix fluid transfer, and trends in the saturation profiles, but not the irreducible wetting-phase saturation behind the flooding front. The underestimation of the irreducible wetting phase saturation suggests that finer image and lattice resolutions than those reported here may be required for accurate prediction of some macroscale multiphase flow properties, at a sizable computational cost.
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