Numerous ice-soil-mixture landslide dams have formed in the cryosphere such as the Tibetan Plateau and resulted in disastrous consequences after these dams broke. The dam forming materials are often ice-soil mixtures that consist of graded soil particles and fragmented ice particles. The performance of such mixtures when subject to ice melting has rarely been studied; yet understanding the thermal-hydro-mechanical behavior of such ice-soil mixtures is essential for mitigating glacier hazards. In this study, the mechanical responses of ice-soil mixture to ice melting were investigated using an advanced stress- and temperature-controlled triaxial apparatus. Ice-soil mixtures with various initial ice contents were tested under different stress states. In each test, the progression of ice melting, local and global deformation, and post-melting stress-strain behavior were measured and evaluated. The test program led to the first batch of experiment data on the mechanical responses of ice-soil mixtures to ice melting. A relationship between normalized volumetric change and normalized time was established to describe the progression of ice melting. The melting of ice particles caused significant deformation, increases in the void ratio and degree of saturation, and reductions in the shear strength. These properties reached a steady state when the initial ice content exceeded 30%.
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