岩土力学 ›› 2023, Vol. 44 ›› Issue (2): 531-540.doi: 10.16285/j.rsm.2022.0362

• 基础理论与实验研究 • 上一篇    下一篇

物质组成特征对碎石土斜坡变形破坏影响研究

周翔1,蔡静森1, 2,马伟成1,肖皓文1   

  1. 1. 中国地质大学(武汉)工程学院,湖北 武汉 430074; 2. 中国地质大学(武汉)岩土钻掘与防护教育部工程研究中心,湖北 武汉 430074
  • 收稿日期:2022-03-24 接受日期:2022-06-20 出版日期:2023-02-10 发布日期:2023-02-17
  • 通讯作者: 蔡静森,男,1988年生,博士,副教授,主要从事重大工程区地质灾害风险评估与防控方面的研究。E-mail: jingsencai@cug.edu.cn E-mail:475292944@qq.com
  • 作者简介:周翔,男,1998年生,硕士研究生,主要从事岩土体性质及稳定性方面的研究。
  • 基金资助:
    国家自然科学基金青年项目(No. 41807264);教育部重点实验室开放基金课题(No. 2020KDZ01);岩土钻掘与防护教育部工程研究中心开放课题基金(No. 202102)

Influence of material composition characteristics on the deformation and failure of gravel soil slopes

ZHOU Xiang1, CAI Jing-sen1, 2, MA Wei-cheng1, XIAO Hao-wen1   

  1. 1. Faculty of Engineering, China University of Geosciences, Wuhan, Hubei 430074, China; 2. Engineering Research Center of Rock-Soil Drilling & Excavation and Protection of Ministry of Education, China University of Geosciences, Wuhan, Hubei 430074, China
  • Received:2022-03-24 Accepted:2022-06-20 Online:2023-02-10 Published:2023-02-17
  • Supported by:
    This work was supported by the National Natural Science Foundation of China Youth Program (41807264), the Open Fund Project of the Key Laboratory of the Ministry of Education (2020KDZ01) and the Open Project Fund of Geotechnical Drilling and Protection Engineering Research Center, Ministry of Education (202102).

摘要: 为研究物质组成空间分布特征对降雨下碎石土斜坡变形破坏的影响,以不同成因碎石土斜坡的特点为依照,进行了4种物质组成空间分布的碎石土斜坡模型及1种均质斜坡模型试验。结果表明,物质组成空间分布特征对降雨下碎石土斜坡变形破坏所发挥的作用与降雨入渗方向和应力调整方向有重要关系。当土料变化方向与入渗方向大角度相交且与应力调整方向相同时,斜坡渗透性为土料各自的渗透性,斜坡力学性质偏向于组成土料力学性质的最大值。当土料变化方向与入渗方向相同且与应力调整方向大角度相交时,斜坡渗透性接近组成土料渗透性的最小值,斜坡变形破坏受控于其中的软弱土料。降雨下斜坡各处均发生变形,且变形向周围调整并产生影响。破裂面更易发于软弱土料中。该研究有助于斜坡灾害勘察、预测评价及防治向精细化方向发展。

关键词: 碎石土斜坡, 室内模型试验, 物质组成空间分布, 应力调整, 降雨入渗, 变形破坏规律

Abstract: To study the influence of the spatial distribution characteristics of material composition on the deformation and failure of gravel soil slope under rainfall, four types of material composition spatial distribution gravel soil slopes and homogeneous slope model tests were conducted according to the characteristics of gravel soil slopes of different geneses. Results show that the role of spatial distribution of material composition played in the deformation and failure of gravel soil slope under rainfall depends on the directions of rainfall infiltration and stress adjustment. When the change direction of soil material intersects the rainfall infiltration direction at a large angle and is the same as the stress adjustment direction, the permeability of slope is actually the permeability of the constituent materials themselves, and the mechanical properties of slope approach the maximum value of the mechanical properties of soil materials that form the slope. When the change direction of soil material is the same as the rainfall infiltration direction and intersects the stress adjustment direction at a large angle, the slope permeability approaches the minimum value of the permeability of the constituent soil material, and the slope deformation and failure are controlled by the weak soil material. The deformation occurs in all parts of the slope under rainfall, and it adjusts to surroundings and thus affecting the surroundings. The fractured surface is more likely to occur in weak soil. Research contributes to the development of the slope disaster investigation, prediction, evaluation and prevention towards refinement.

Key words: gravel soil slope, laboratory model test, spatial distribution of material composition, stress adjustment, rainfall infiltration, pattern of deformation and failure

中图分类号: TU 43
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