Deep underground rock masses with structural defects often experience combined dynamic and static stress conditions. This study systematically examines the multi-scale failure mechanisms of fractured red sandstone subjected to combined loading by varying the rock bridge angle ( α ). A custom dynamic-static superposition system featuring an anti-rebound mechanism was employed to provide pure, uninterrupted dynamic pulses. Synchronized multi-field characterization suites, comprising acoustic emission (AE) and digital image correlation (DIC), were utilized to monitor the real-time progression of damage evolution. A dimensionless competition factor χ and a friction-corrected effective Mode-II stress intensity factor ( K II eff ) are formulated to define the mechanical transition from crack-tip tensile-shear regimes to rock-bridge pure shear regimes. Results indicate that as α increases from 0° to 90°, the peak strength demonstrates a variable decline, while the primary damage zone consistently shifts from the tips of flaws to the connecting ligament. Furthermore, an analytical model that incorporates a dynamic participation coefficient λ ( α ) is proposed. This model effectively forecasts a non-linear "Dynamic Strengthening Effect" specifically at α = 90°, where transient kinematic adjustments reformulate the primary load-transfer paths. Complementary PFC2D discrete element modeling accurately replicates the macro-mechanical profiles, confirming the localized stress-transfer pathways. These findings establish a strong theoretical and experimental foundation for evaluating stability in deep underground engineering.
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Zhang et al. (2026) studied this question.
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