Experimental Study on the Shear Behavior and Acoustic Emissions of Rock Joints Containing Ice-Rich Debris Infill
摘要
Increasing global warming has amplified high-altitude geohazards associated with rock joints containing ice-rich debris infill (RJID), threatening high-altitude infrastructure. Through cryogenic direct shear tests with acoustic emission (AE) monitoring, this study investigates how the filling ratio (t/a: infill thickness to asperity height), ice content (Vice), and temperature (T) govern RJID shear behavior. Three distinct failure modes are identified: elastic–fluctuating–plastic (EFP) in unfilled joints transitions to elastic–brittle–plastic (EBP) or elastic–softening–plastic (ESP) in ice-rich conditions, with EBP dominating at high Vice (≥ 65%) or low T (≤ − 3 °C). A critical t/a threshold (0.5–1.0) exists where shear strength drops by > 50% as failure shifts from rock-infill composite to pure infill-dominated behavior. This study quantifies unprecedented thermal sensitivity (τp decreases by 138.8 kPa/°C) and ice content effects (47% strength reduction at t/a = 3 when Vice increases from 40 to 90%). AE signals correlate with damage mechanisms, exhibiting delayed maxima and reduced amplitudes at high t/a. An enhanced Mohr–Coulomb criterion, incorporating T- and Vice—dependent cohesion/friction angles, was developed via bivariate regression. A refined disturbed state concept (DSC) constitutive model was developed to capture the deformation process.