Disasters such as water inrush induced by blasting and excavation frequently occur in deep rock engineering. These are closely associated with microcrack formation and expansion in rock. Their prevention requires a thorough understanding of the dynamic fracture behavior of rocks under coupled static stress and water pressure conditions. To address this issue, a testing method for determining the mode-I dynamic fracture toughness of rocks under such coupled conditions was developed using a self-designed rock dynamics system capable of applying static stress and water pressure. Dynamic fracture experiments were conducted on granite specimens to investigate the effects of dynamic loading rate and water pressure on mode-I dynamic fracture toughness. An evolution model was then established. The evolution mechanism was further elucidated through combined macroscopic and microscopic fracture analyses. Results indicate that, under a constant water pressure, the mode-I dynamic fracture toughness follows a power-function increase with increasing loading rate, although the enhancement becomes less pronounced at high loading rates. Under a fixed loading rate, the toughness rises linearly with water pressure. Macroscopically, higher water pressure and loading rate reduce both fracture expansion contour roughness and fractal dimension. Microscopically, the fracture mechanism transitions from intergranular to transgranular failure. These findings provide theoretical guidance for preventing water inrush disasters induced by blasting and excavation.
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