LIN Zhiheng, ZHANG Guangze, YUAN Dong
Journal of Railway Engineering Society. 2025, 42(8): 67-71.
Research purposes: With the continuous advancement of tunnel engineering in complex geological conditions in western China, water and mud inrush during mountain tunnel construction has become increasingly frequent and severe. Among these disasters, time-lag inrush events characterized by suddenness and hysteresis pose significant challenges to construction safety due to their pronounced spatio-temporal uncertainties. This paper analyzes the formation environments and process mechanisms of recent time-lag water and mud inrush events in mountain tunnels, proposes their definitions, classifications, detection and prediction technologies, and establishes a set of reliable risk identification and prevention measures for field construction.
Research conclusions: (1) Time-lag water and mud inrush events can be classified into three categories based on spatio-temporal characteristics: water gushing-piping type, flow soil-collapse type, and composite type.(2) High-risk zones for time-lag inrushes typically exhibit disaster-prone environmental features such as surface negative topography, structural fracture zones, low-resistivity anomaly regions in geophysical surveys, and minor angles between maximum principal stresses and negative topography/structures.(3) A semi-quantitative evaluation method was developed to assess risk levels (Levels I,II,and III) and probabilities of time-lag inrush, considering factors including rock fragmentation, water outflow state, primary support conditions, and construction collapse impacts.(4) Prevention strategies should follow the principle of "prioritizing robustness over weakness and ensuring one-time pass-through". Key measures include extended detection range, long-distance pressure relief, graded reinforcement techniques, and hierarchical risk mitigation for hysteresis hazards.(5) The research results can provide references for predicting and controlling time-lag water/mud inrush in similar complex geological settings.