Ageing deformation of tailings dams in seasonally frozen soil areas under freeze-thaw cycles

Abstract The freeze-thaw cycle is one of the important factors in inducing a dam-break in the permafrost region, so it is of great practical significance to study the mechanism of the failure deformation of tailings dams under freeze-thaw cycles. In this paper, the water-heat-force coupling model of...

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Bibliographic Details
Published in:Scientific Reports
Main Authors: Jin, Jiaxu, Li, Shiwang, Song, Chenguang, Zhang, Xinlei, Lv, Xiangfeng
Other Authors: National Natural Science Foundation of China
Format: Article in Journal/Newspaper
Language:English
Published: Springer Science and Business Media LLC 2019
Subjects:
Online Access:http://dx.doi.org/10.1038/s41598-019-51449-6
http://www.nature.com/articles/s41598-019-51449-6.pdf
http://www.nature.com/articles/s41598-019-51449-6
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Summary:Abstract The freeze-thaw cycle is one of the important factors in inducing a dam-break in the permafrost region, so it is of great practical significance to study the mechanism of the failure deformation of tailings dams under freeze-thaw cycles. In this paper, the water-heat-force coupling model of a tailings dam considering frost-thaw damage is established, and the freeze-thaw cyclic ageing deformation of a tailings dam in a seasonally frozen soil area is studied. The correctness of the model is validated by numerical calculation. The research shows under the same water content, the compressive strength and modulus of deformation decrease with an increase in the number of freeze-thaw cycles, the cohesion and internal friction angle decrease, and the amplitude gradually decreases before becoming stable. In the process of cooling, the pore water pressure first increases and then decreases, and the pore water pressure first decreases and then increases during the heating process. The research results can provide a theoretical basis and reference values for the stability analysis of tailings dams in seasonally frozen soil areas.