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应力-干湿循环联合作用下泥岩剪切特性试验研究

张景昱 王文豪 邓华锋 李建林 宛良朋 李佳成 刘盼 钱信之

岩土力学2026,Vol.47Issue(6):1961-1972,12.
岩土力学2026,Vol.47Issue(6):1961-1972,12.DOI:10.16285/j.rsm.2025.0557

应力-干湿循环联合作用下泥岩剪切特性试验研究

Experimental study on shear characteristics of mudstone under combined action of stress-dry-wet cycles

张景昱 1王文豪 1邓华锋 2李建林 2宛良朋 3李佳成 1刘盼 1钱信之1

作者信息

  • 1. 三峡大学三峡库区地质灾害教育部重点实验室,湖北宜昌 443002||三峡大学水利与环境学院,湖北宜昌 443002
  • 2. 三峡大学三峡库区地质灾害教育部重点实验室,湖北宜昌 443002
  • 3. 中国三峡建设管理有限公司,四川成都 610041
  • 折叠

摘要

Abstract

In practical engineering,the rock mass in the hydro-fluctuation zone of the bank slope is not only subjected to wet-dry cycles,but also influenced by overlying stress,especially clastic rocks represented by mudstone.To study the shear mechanical deterioration characteristics of mudstone in the hydro-fluctuation zone under the combined action of stress and dry-wet cycles,typical mudstone from the bank fluctuation zone of the Three Gorges Reservoir Area was selected as the focal point of this study,and water-rock interaction tests considering the combined action of overlying stress and dry-wet cycles were carried out.The findings revealed:(1)During the combined action of stress and dry-wet cycles,the overlying stress accelerated the deterioration of the shear mechanical properties of mudstone.The greater the overlying stress,the more obvious the decline of the shear stress-shear displacement curve and the steeper the decrease in its slope,and the lower the shear strength and residual strength.(2)The shear strength of mudstone demonstrated a degradation pattern characterized by an initial rapid decline,followed by a gradual slowdown,and ultimately stabilization.The degradation observed in the first five cycles accounted for over 70%of the total degradation,and within the same cycle period,higher overlying stress levels corresponded to greater degradation amplitudes.(3)The increase in overlying stress significantly deteriorated the mesoscopic structure of mudstone,promoting fracture expansion,increasing the contact area of water-rock interaction,and accelerating processes such as the dissolution of calcareous cement and the expansion and contraction of illite and montmorillonite,leading to increased porosity and loose structure of mudstone.The research outcomes offer valuable insights for assessing the stability of clastic rock bank slopes in the Three Gorges Reservoir area.

关键词

消落带泥岩/干湿循环/上覆应力/剪切力学特性/劣化效应

Key words

mudstone in the hydro-fluctuation zone/dry-wet cycles/overlying stress/shear mechanical properties/deterioration effect

分类

建筑与水利

引用本文复制引用

张景昱,王文豪,邓华锋,李建林,宛良朋,李佳成,刘盼,钱信之..应力-干湿循环联合作用下泥岩剪切特性试验研究[J].岩土力学,2026,47(6):1961-1972,12.

基金项目

国家自然科学基金(No.U22A20600,No.52327811,No.52009067) (No.U22A20600,No.52327811,No.52009067)

三峡库区地质灾害教育部重点实验室开放基金项目(No.2022KDZ23).This work was supported by the National Natural Science Foundation of China(U22A20600,52327811,52009067)and the Open Fund Project of Key Laboratory of Geological Hazards on Three Gorges Reservoir Area(2022KDZ23). (No.2022KDZ23)

岩土力学

1000-7598

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