Red-bed mudstone is a widely distributed sedimentary fill material in western China and exhibits pronounced moisture sensitivity, making it susceptible to long-term creep deformation under unsaturated conditions. To elucidate its time-dependent mechanical behavior and underlying microstructural control mechanisms, a series of multi-stage creep tests was conducted using a GDS double-cell unsaturated triaxial apparatus under controlled matric suctions of 100, 200, and 300 kPa. The microstructural evolution before and after creep was systematically investigated through scanning electron microscopy (SEM) and mercury intrusion porosimetry (MIP). The results indicate that red-bed mudstone exhibits strongly nonlinear, time-dependent deformation characteristics under coupled matric suction-stress conditions. At high creep loading levels, increasing matric suction markedly suppresses pore collapse and compressive deformation, leading to a progressive transition in the creep mechanism from compression-dominated to shear-dominated behavior. Matric suction primarily inhibits creep deformation by enhancing structural stability, whereas higher stress levels intensify structural rearrangement and compaction. Microstructural analyses further reveal that increasing suction reduces pore connectivity and promotes face-to-face contacts between platy minerals, thereby effectively slowing the creep rate. In addition, the regulatory effect of matric suction on creep stiffness shows a pronounced dependence on stress level, and creep stiffness exhibits a characteristic time-dependent softening behavior. These findings provide new insights into the long-term creep deformation mechanisms of unsaturated red-bed mudstone and offer valuable reference information for evaluating the long-term stability of high-fill station-yard subgrades under complex geological conditions.
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