@Article{fdmp.2024.056421,
AUTHOR = {Min Feng, Long Wang, Lei Sun, Bo Yang, Wei Wang, Jianning Luo, Yan Wang, Ping Liu},
TITLE = {Characterization of Pore Structure and Simulation of Pore-Scale Flow in Tight Sandstone Reservoirs},
JOURNAL = {Fluid Dynamics \& Materials Processing},
VOLUME = {21},
YEAR = {2025},
NUMBER = {3},
PAGES = {573--587},
URL = {http://www.techscience.com/fdmp/v21n3/60153},
ISSN = {1555-2578},
ABSTRACT = {This study sheds light on how pore structure characteristics and varying dynamic pressure conditions influence the permeability of tight sandstone reservoirs, with a particular focus on the Paleozoic reservoirs in the Qingshimao Gas Field. Using CT scans of natural core samples, a three-dimensional digital core was constructed. The maximum ball method was applied to extract a related pore network model, and the pore structure characteristics of the core samples, such as pore radius, throat radius, pore volume, and coordination number, were quantitatively evaluated. The analysis revealed a normally distributed pore radius, suggesting a high degree of reservoir homogeneity and favorable conditions for a connected pore system. However, it was found that the majority of throat radii measured less than 1 μm, which severely restricted fluid flow and diminished permeability. Over 50% of the pores measured under 100 μm<sup>3</sup>, further constraining fluid movement. Additionally, 30%–50% of the pore network was composed of isolated and blind-end pores, which significantly impaired formation connectivity and reduced permeability. Based on this, the lattice Boltzmann method (LBM) was used for pore-scale flow simulation to investigate the influence mechanism of pore structure characteristics and dynamic-static parameters such as displacement pressure difference on the permeability performance of the considered tight sandstone reservoirs for various pressure gradients (0.1, 1, and 10 MPa). The simulations revealed a strong relationship between pressure differential and both the number of streamlines and flow path tortuosity. When the pressure differential increased to 1 MPa, 30 streamlines were observed, with a tortuosity factor of 1.5, indicating the opening of additional seepage channels and the creation of increasingly winding flow paths.},
DOI = {10.32604/fdmp.2024.056421}
}