Study on Stress-Type Rockburst Mechanism Based on Continuous-Discontinuous Element Method

IF 1.8 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Lithosphere Pub Date : 2023-05-08 DOI:10.2113/2022/5668451
Kezhu Chen, Tianbin Li, Meiben Gao, Chun-chi Ma, Y. Zhang
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引用次数: 0

Abstract

Rockburst plays a serious threat to personnel and equipment during underground engineering construction. The study of the rockburst mechanism is helpful to its prediction and prevention. Based on the characteristic analysis of a large number of rockburst cases, Li et al. proposed three stress-type and three stress-structural rockbursts and obtained the geological characteristics and occurrence criteria of these rockbursts, but the evolution process of rockbursts is still unclear. Based on the continuous-discontinuous element method, the characteristics of failure process, surrounding rock stress, motion, and energy of three stress-rockburst blocks are analyzed. The results show that rockburst failure generally goes through several stages, such as a few surfaces tensile failure, shallow shear failure, deep extension of tensile failure, shear failure communication, and rockburst occurrence. The total volume of rockburst blocks and the main distribution intervals of block diameters for different types of rockbursts are quite different, which are mainly affected by stress state and geological structure. The ejection velocity of the small block is always higher than that of the large block during the same one rockburst simulation, and the ejection velocity of the small block is from the surface. In the process of rockburst, not only the elastic strain energy is released but also the elastic strain energy is accumulated. The greater the rockburst intensity, the more the elastic strain energy is released, and the steeper the prepeak curve of elastic strain energy. The research results provide a reference for further understanding the mechanism of rockburst and lay a theoretical basis for the prevention and control of rockburst in underground engineering.
基于连续-不连续单元法的应力型岩爆机理研究
在地下工程施工中,岩爆对人员和设备造成了严重的威胁。对岩爆机理的研究有助于岩爆的预测和防治。Li等在对大量岩爆案例进行特征分析的基础上,提出了三种应力型岩爆和三种应力构造岩爆,并获得了这些岩爆的地质特征和产状判据,但岩爆的演化过程尚不清楚。基于连续-不连续单元法,分析了3个应力-岩爆块体的破坏过程、围岩应力、运动和能量特征。结果表明:岩爆破坏总体上经历了少量地表拉伸破坏、浅层剪切破坏、拉伸破坏向深部延伸、剪切破坏贯通、岩爆发生等几个阶段;不同类型岩爆的岩爆块体总量和主要块体直径分布区间差异较大,主要受应力状态和地质构造的影响。在同一次岩爆模拟中,小块体的弹射速度总是高于大块体的弹射速度,并且小块体的弹射速度来自地表。在冲击地压过程中,弹性应变能不仅有释放,而且有积累。冲击地压强度越大,释放的弹性应变能越多,弹性应变能预峰曲线越陡。研究结果为进一步认识岩爆机理提供了参考,为地下工程防治岩爆奠定了理论基础。
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来源期刊
Lithosphere
Lithosphere GEOCHEMISTRY & GEOPHYSICS-GEOLOGY
CiteScore
3.80
自引率
16.70%
发文量
284
审稿时长
>12 weeks
期刊介绍: The open access journal will have an expanded scope covering research in all areas of earth, planetary, and environmental sciences, providing a unique publishing choice for authors in the geoscience community.
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