Crack evolution and strength deterioration of fine-grained tailings under dry and wet cycle

IF 4.2 2区 工程技术 Q3 ENGINEERING, ENVIRONMENTAL
Qinglin Chen, Lilin Bao, Chao Zhang, Zugui Li, Xiaojun Wang, Guangjin Wang
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Abstract

Affected by repeated tailings discharge and rainfall, tailings materials are constantly in a state of moisture absorption and desorption, which degrades mechanical properties of tailings. To investigate the evolution of cracks and the deterioration of strength in fine-grained tailings under dry-wet cycling conditions, direct shear tests and nuclear magnetic resonance (NMR) tests were conducted. The strength deterioration and pore structure characteristics of fine-grained tailings were analyzed. Using image processing technology, surface crack parameters of fine-grained tailings were extracted, and the crack evolution characteristics under dry-wet cycles were explored. The evolution of surface cracks can be divided into two stages: rapid crack development and steady crack development. In the rapid crack development stage, both the area and average width of the cracks decrease significantly, while the total length decreases slowly. In the steady crack development stage, the crack area and average crack width gradually decline, and the total crack length undergoes a pronounced reduction. The porosity of the tailings consistently increases due to the cycles. Cohesion and the internal friction angle of the tailings decrease exponentially with increasing porosity, and both also decrease as the number of dry-wet cycles increases. Consequently, the safety factor of the tailings dam gradually declines with increased cycling, leading to reduced dam stability and increased risk for safe operation. The research results provide certain guiding significance for the stability and long-term safe operation of tailings dams.

Abstract Image

干湿循环下细粒尾砂裂纹演化与强度劣化
受反复尾矿排放和降雨的影响,尾矿物料不断处于吸湿解吸状态,使尾矿的力学性能下降。为研究干湿循环条件下细粒尾矿的裂纹演化和强度劣化,开展了直剪试验和核磁共振试验。分析了细粒尾砂的强度劣化及孔隙结构特征。利用图像处理技术提取细粒尾砂表面裂纹参数,探索干湿循环作用下的裂纹演化特征。表面裂纹的演化可分为快速裂纹发展和稳定裂纹发展两个阶段。在裂纹快速发展阶段,裂纹面积和平均宽度均显著减小,而总长度减小缓慢。在裂纹稳定发展阶段,裂纹面积和平均裂纹宽度逐渐减小,裂纹总长度明显减小。随着循环的进行,尾矿的孔隙率不断增大。尾矿的黏聚力和内摩擦角随孔隙率的增加呈指数减小,随干湿循环次数的增加而减小。因此,随着循环次数的增加,尾矿坝的安全系数逐渐降低,导致尾矿坝稳定性降低,安全运行风险增大。研究结果对尾矿坝的稳定和长期安全运行具有一定的指导意义。
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来源期刊
Bulletin of Engineering Geology and the Environment
Bulletin of Engineering Geology and the Environment 工程技术-地球科学综合
CiteScore
7.10
自引率
11.90%
发文量
445
审稿时长
4.1 months
期刊介绍: Engineering geology is defined in the statutes of the IAEG as the science devoted to the investigation, study and solution of engineering and environmental problems which may arise as the result of the interaction between geology and the works or activities of man, as well as of the prediction of and development of measures for the prevention or remediation of geological hazards. Engineering geology embraces: • the applications/implications of the geomorphology, structural geology, and hydrogeological conditions of geological formations; • the characterisation of the mineralogical, physico-geomechanical, chemical and hydraulic properties of all earth materials involved in construction, resource recovery and environmental change; • the assessment of the mechanical and hydrological behaviour of soil and rock masses; • the prediction of changes to the above properties with time; • the determination of the parameters to be considered in the stability analysis of engineering works and earth masses.
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