The mechanism governing the transition from creep to rapid movement is a central challenge in understanding the instability of reservoir landslides. This study focuses on the Muyubao landslide, a giant bedding landslide in the Three Gorges Reservoir Area that exhibits persistent creep. This study focuses on the Muy...
During the initial stage of water injection into deep, low-permeability gas-bearing coal seams, a significant threshold pressure gradient causes the seepage behavior to deviate from Darcy's linear flow law. Consequently, the pressure gradient of pressure-driven water increases during transport through the porous medium...
Due to their complex pore-throat networks, low permeability, and high water saturation, water-bearing tight sandstone reservoirs exhibit pronounced heterogeneity in formation pressure distribution and unclear reserve mobilization patterns. These factors hinder accurate estimation of remaining gas and the design of ba...
Rainfall and fluctuations in reservoir water levels are critical external factors influencing the stability of landslides along reservoir banks. This study investigates the Yetan Primary School landslide, which serves as a representative example of a metamorphic rock landslide influenced by reservoir conditions in Shiy...
Researching the deformation mechanisms and early warning of landslides holds significant engineering importance. A typical accumulation-structured landslide in southern China was selected as the case study to investigate the intrinsic failure mechanisms of slopes, with adjacent tunnel construction and rainfall consider...
Long-term groundwater exploitation causes water-level fluctuations, which are a major driver of land subsidence and infrastructure deformation in sedimentary basins. To investigate the stress-history-dependent compression–rebound behavior of deep cohesive soils, soil samples along the Beijing–Tianjin High-Speed Railway...
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