Rock and Soil Mechanics ›› 2026, Vol. 47 ›› Issue (11): 3908-3920.doi: 10.16285/j.rsm.2025.1303

• Geotechnical Engineering • Previous Articles     Next Articles

Evolution of static stability of upstream tailings dams

ZHANG Chao1, LI Xue-ting1, 2, YANG Chun-he1, LIU Yong-feng3, 4, MA Chang-kun1, MA Lei1   

  1. 1. State Key Laboratory of Geomechanics and Geotechnical Engineering Safety, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, Hubei 430071, China; 2. University of Chinese Academy of Sciences, Beijing 100049, China; 3. School of Resources and Safety Engineering, Chongqing University, Chongqing 400044, China; 4. Shenzhen Zhongjin Lingnan Nonferrous Metal Company Limited, Shenzhen, Guangdong 518024, China
  • Received:2025-12-04 Accepted:2026-03-12 Online:2026-11-09 Published:2026-11-07
  • Supported by:
    The work was supported by the National Natural Science Foundation of China (52574170, 52304155), the National Key Research & Development Program of China (2023YFC3012200) and the Key Project of China Coal Technology & Engineering Group Corp (2022-ZD002).

Abstract: To reveal the evolution of static stability of upstream tailings dams under the combined effects of construction rate, fine-grained interlayers, and drainage facilities, this paper employs FLAC3D, integrating the Duncan-Chang constitutive model with the Van Genuchten-Mualem seepage model, to simulate the stability response of the dam during incremental construction. The results indicate that the landslide mode of the dam evolves through three stages: the unsaturated zone stage, the partially saturated zone stage, and the saturated zone stage. The shape of the most dangerous sliding surface is governed by the internal structure: it remains circular in homogeneous dams, whereas in dams containing fine-grained interlayers, it gradually transitions from circular to a non-circular shape controlled by the interlayers. The horizontal displacement at the crest of the starter dam exhibits three stages: initial deformation, uniform deformation, and accelerated deformation. The accelerated deformation stage is triggered by fine-grained interlayers and can be effectively suppressed by improving drainage. The safety factor evolution follows a two-stage pattern: the unsaturated-partially saturated zone landslide stage and the saturated zone landslide stage. The controlling effect of fine-grained interlayers on the sliding surface morphology only becomes apparent during the saturated zone landslide stage. The findings of this paper can provide a reference for the safety management of upstream tailings dams and help reduce the risk of static instability.

Key words: upstream tailings dams, static stability, dam construction rate, fine-grained interlayer, drainage facilities

CLC Number: 

  • TU 433
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