Tailings Heterogeneity and Multi-Scenario Response of an Upstream Tailings Dam
- Proceedings
- EUROCK 2026
- Pages
- 1081-1087
- Submitted
- 22 April 2026
- Accepted
- 15 June 2026
- Published
- 12 August 2026
Summary
Abstract
Upstream tailings dams are highly vulnerable to instability under extreme rainfall and seismic loading, yet the mechanism by which depositional spatial heterogeneity governs dam responses and failure evolution under multiple scenarios remains insufficiently constrained. This study investigates a high-altitude canyon-type upstream tailings storage facility in western China using representative profiles, borehole sampling, laboratory testing, and GeoStudio-based numerical simulations. The results show that the deposited tailings become progressively finer from the dam front to the reservoir tail, while vertically they display a coarse-fine-coarse cyclic pattern, jointly forming a pronounced three-dimensional heterogeneous structure. This depositional heterogeneity is further translated into layered hydro-mechanical parameter zonation, characterized by relatively loose, more permeable, and lower-stiffness tailings in the shallow part, a compaction-transition zone in the middle part, and denser tailings with lower permeability, higher shear strength, and higher stiffness at depth. Under heavy rainfall, infiltration is preferentially concentrated in the shallow tailings, whereas the relatively low-permeability middle layers impede downward seepage, resulting in perched water, pore-pressure accumulation near the dam toe, and progressive reduction in effective stress and local shear resistance; consequently, the factor of safety decreases from 1.35 to 0.98. Under seismic loading, the combined influence of low stiffness in the shallow tailings, structural transitions in the middle-upper zone, and free-surface amplification promotes deformation localization in the crest and middle-upper deposited-tailings zone, leading to the development of potential sliding zones and a reduction in the factor of safety to 0.962. These findings demonstrate that tailings spatial heterogeneity is not merely a depositional feature, but the key internal factor governing seepage redistribution, deformation localization, and failure evolution of upstream tailings dams under different external disturbances.
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References
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