Rock fracturing is widespread in the upper crust of the earth. Nearly all in-situ rocks are subject to subsurface pressures. Understanding the influence of effective pressure (difference between confining stress and pore pressure) on the elastic properties of fractured rocks is crucial for estimating in-situ seismic properties. Wave-Induced Fluid Flow (WIFF) and fracture Elastic Scattering (ES) attenuation mechanisms have been widely studied. However, the effects of effective pressure on WIFF and ES mechanisms in fractured rocks are relatively unexplored. To investigate the pressure influence on WIFF and ES in P and SV wave propagation, we developed a pressure-dependent dynamic model to incorporate Multi-shaped Microcracks' Squirt Flow (MMSF), Fracture-Background WIFF (FB-WIFF), Biot Flow, and ES mechanisms with non-linear elastic and hyper-elastic deformation stages. The results show that both the WIFF and ES mechanisms are affected by effective pressure, except for the ES mechanism of normal incident SV waves. The WIFF is more susceptible to effective pressure than the ES mechanism. In addition, the closure of microcracks (soft pores) during effective pressure loading continuously decouples the MMSF mechanism from the FB-WIFF, Biot Flow, and ES mechanisms, causing the increase in the velocity of the P- and SV- waves and the variations in the attenuation processes. These wave propagation characteristics help to understand the hydraulic properties of in-situ fractured rocks. By comparing model predictions with ultrasonic laboratory velocity data under varying effective pressure loading, we validated our model.
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