Fines migration and clogging in porous media have significant implications for engineering applications. For example, during the extraction of marine gas hydrates, fines migration can lead to pore clogging and reduced permeability. This study combines micromodel experiments with DEM-CFD simulations to investigate the effects of fine type (latex/mica), fine shape (spherical/flake), pore size (50 to 700 μm), and pore fluid composition (DW/brine) on fines migration, fine clogging behavior, and the evolution of host sediment porosity. Experiments demonstrate that clogging is geometrically influenced by the relationship between pore size and fines dimensions. Even when the size of fines (mica) is smaller than the pore throat size, their aggregates can still lead to clogging at very low concentrations (0.1–0.2%). The aggregate size of irregular mica is affected by changes in pore fluid properties, which may occur due to the freshening of pore water during hydrate dissociation. Furthermore, a moving gas/liquid interface concentrates fines, thereby increasing the risk of pore clogging. Simulations further reveal that fines migration causes dynamic changes in porosity, which requires a comprehensive consideration of the coupled effects of fine type, fluid velocity, pore size, and fluid chemistry. This study elucidates the microscopic mechanisms and quantifies the macroscopic effects of fines migration behavior in porous media, providing a theoretical foundation for further research.

Particle migration is a pore-scale process that fundamentally controls pore-structure evolution and seepage behavior in granular porous media. This study investigates fine particles migration in coarse-grained sediments and its effects on pore structure and permeability by combining low-field nuclear magnetic resonance (LF-NMR) experiments with coupled CFD–DEM simulations. The evolution of fine particles migration rate, porosity variation, and permeability was analyzed under different fluid injection velocities and fines concentrations. Higher injection velocities accelerate fines initiation and early-stage migration by increasing hydrodynamic drag forces, whereas their influence diminishes at later stages due to pore-structure confinement and localized particle retention. At a constant injection velocity, increasing fines concentration suppresses early fines mobilization owing to enhanced interparticle interactions and pore throat blockage. As seepage continues, progressive fines release and export enlarge pore space and enhance permeability. Spatial analyses reveal that fines migration is governed by localized retention and rearrangement within pore throats. Within the investigated parameter ranges and timescales, system evolution is dominated by internal erosion and pore unclogging rather than sustained macroscopic clogging. These results provide mechanistic experimental–numerical insight into fines migration and seepage stability in granular porous media, with direct relevance to hydrate-bearing sediments and other fine-sensitive geological systems.