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新疆浅埋地层泥岩的吸水软化特性及隧洞支护对策研究
引用本文:张勇,石富坤,王俊伟,张家瑄,卢昊,孙晓明. 新疆浅埋地层泥岩的吸水软化特性及隧洞支护对策研究[J]. 矿业科学学报, 2021, 6(1): 42-50. DOI: 10.19606/j.cnki.jmst.2021.01.005
作者姓名:张勇  石富坤  王俊伟  张家瑄  卢昊  孙晓明
作者单位:深部岩土力学与地下工程国家重点实验室,北京 100083;中国矿业大学(北京)力学与建筑工程学院,北京 100083;北京邮电大学 后勤处,北京 100083
基金项目:国家重点研发计划2016YFC0600901国家自然科学基金51874311国家自然科学基金51904306深部岩土力学与地下工程国家重点实验室(北京)开放基金SKLGDUEK1826
摘    要:新疆输水隧洞围岩为浅埋泥岩地层,吸水后强度软化,支护难度高,对工程进度影响较大.本文以新疆某输水隧洞泥岩为研究对象,在对隧洞的泥岩进行XRD测试分析的基础上,开展不同含水率状态下泥岩单轴压缩和电镜扫描分析实验研究,揭示了岩样内部裂隙、孔隙结构的变化规律及强度软化特征.结果表明:该隧洞泥岩黏土矿物含量高达50%,易吸水软...

关 键 词:软化规律  软化临界点  微观结构  含水率
收稿时间:2019-08-07

Study on softening characteristics of mudstones in shallow buried strata in Xinjiang and countermeasures for tunnel support
Affiliation:1.State Key Laboratory for GeoMechanics and Deep Underground Engineering, Beijing 100083, China2.School of Mechanics and Civil Engineering, China University of Mining & Technology-Beijing, Beijing 100083, China3.Logistics Department, Beijing University of Posts and Telecommunications, Beijing 100083, China
Abstract:The Xinjiang water conveyance tunnel is a shallow buried mudstone stratum. After the water absorption, the strength of the surrounding rock softens and large deformation occurs. The support is difficult and the risk is high, which has a great impact on the progress of the project. In this paper, the mudstone of a water conveyance tunnel in Xinjiang is taken as the research object. Based on the XRD test analysis of the mudstone in the tunnel, the uniaxial compression and SEM analysis of the mudstone under different water content conditions are carried out, and the internal fissures of the rock sample are revealed. The variation of the pore structure clarifies the strength softening characteristics. The results show that the clay mineral content of the tunnel is as high as 50 %, and the proportion of montmorillonite is close to 90 %, which is easy to absorb water and soften. As the water content increases, the interior of the rock sample will undergo the process of micro-crack development, development and penetration, accompanied by the loss of pore water and internal minerals. By analyzing its saturated water absorption curve, the water absorption process is divided into three stages: rapid water absorption, decelerating water absorption and uniform water absorption stage. The Boltzmann prediction function is used to fit the rock sample strength variation curve after water absorption, and its strength can be changed. It is divided into three states: non-destructive strength, rapid softening and softening and rest state. The critical point for obtaining the softening of water absorption strength of this type of mudstone is 6 % water content; the comprehensive analysis shows that the water softening law is: the clay minerals in mudstone, mainly montmorillonite, have strong water absorption capacity. With the increase of water absorption, the free water content in the mudstone pores is significantly increased, the skeleton strength is gradually reduced, and an unstable state is formed, which is easily deformed and destroyed when subjected to external force. Based on this, the principles of stability control of such soft rock engineering are proposed, which is to determine the soft rock type and deformation mechanics mechanism, formulate targeted stability control strategies, and adopt the support of mechanical properties such as constant resistance, large deformation and high prestress material. The research results are of great significance for understanding the strength and softening characteristics of the mudstone in the water conveyance tunnel, the deformation and failure mechanism of the tunnel surrounding rock and the support design.
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