地质科技通报2024,Vol.43Issue(2) :175-185.DOI:10.19509/j.cnki.dzkq.tb20220513

岩崩坡面撞击碎裂特征离散元模拟

Rockfall fragmentation upon slope impact based on discrete element simu-lation

黄健 袁镜清 曾探 廖健鸿 黄祥 王豪
地质科技通报2024,Vol.43Issue(2) :175-185.DOI:10.19509/j.cnki.dzkq.tb20220513

岩崩坡面撞击碎裂特征离散元模拟

Rockfall fragmentation upon slope impact based on discrete element simu-lation

黄健 1袁镜清 2曾探 1廖健鸿 1黄祥 1王豪1
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作者信息

  • 1. 成都理工大学地质灾害防治与地质环境保护国家重点实验室,成都 610059
  • 2. 成都理工大学地质灾害防治与地质环境保护国家重点实验室,成都 610059;北京城建勘测设计研究院有限责任公司,北京 100101
  • 折叠

摘要

岩崩坡面撞击破碎是运动轨迹难以预测的重要原因,其中坡体几何特征是影响破碎块体运动变化特征的关键因素.为了研究岩崩撞击破碎过程及坡体几何特征对岩崩块体运动特征的影响,利用离散单元法(PFC2D)模拟技术,通过统计典型岩崩灾害点岩体结构与坡体几何特征,建立了岩崩 自由落体-撞击破碎-运动堆积模型,剖析了在不同坠落高度、撞击角度条件下岩崩坡面撞击碎裂过程,获得了块体运动速度、裂纹数量和冲击力变化曲线,同时采用双参数Weibull分布对碎裂块体破碎程度进行了描述.实验结果表明:破裂过程分为接触-解体、挤压-碎裂及独立运动3个阶段;岩体碎裂由撞击点开始,沿结构面先出现解体,再产生新断裂面的岩石破碎;块体速度、裂纹数量和冲击力的骤变均发生在接触-解体与挤压-碎裂阶段,块体速度骤降,呈现出"阶梯效应",冲击力骤升,表现为"双峰现象",同时随着坠落高度增加或撞击角度减小,"阶梯效应"与"双峰现象"更为明显;同一撞击角度条件下,坠落高度的增加使得撞击动能增加,进而增大了破碎程度,导致粒径分布范围与特征粒径尺寸的减小;同一坠落高度下,撞击角度的增加,意味着接触面积的减小,进而降低了破碎程度,导致粒径分布范围与特征粒径尺寸的增大.研究成果对揭示岩崩坡面撞击碎裂机理及预测块体运动轨迹提供了技术支撑.

Abstract

[Objective]The impact and fracture of rockfall are important reasons for the difficulty in predicting movement trajectories,and the geometric characteristics of slope bodies are key factors affecting the movement.[Methods]To study the crushing process of rockfalls and the influence of slope geometry characteristics on the movement of rockfall blocks,discrete element method(PFC2D)simulation technology was used to establish a rock-fall free-fall-impact model to analysethe rock mass structure and slope geometry characteristics of typical rockfall disaster points.The fragmentation process of rockfall under different fall heights and impact angles is analysed,and the block motion velocity,crack number and impact force are obtained.Moreover,the two-parameter Weibull dis-tribution is used to describe the fragmentation degree of blocks.[Results]The experimental results reveal that the fracture process can be divided into three stages:Contact-disintegration,extrusion-fragmentation and independent movement.Rock mass fragmentation starts at the impact point,disintegration occurs along the structural plane first,and fragmentation occurs on the new fracture plane.Sudden changes of the block velocity,crack quantity and im-pact force occur in the contact-disintegration and compression-fragmentation stages.The block velocity plummets,exhibiting a"step effect",and the impact force rises sharply,revealing a"double peak phenomenon".Moreover,when the fall height increases or the impact angle decreases,the"step effect"and"double peak phenomenon"be-come more obvious.Under the same impact angle,an increase of the fall height results in the increase of impact ki-netic energy,thus increasing the degree of fragmentation and decreasing the particle size distribution range and characteristic particle size.At the same fall height,an increase in the impact angle causes that the contact area is reduced,and the degree of breakage is reduced,increasing the particle size distribution range and characteristic particle size.[Conclusion]The present results provide technical support for revealing the impact fragmentation mechanism of rockfall slopes and predicting the trajectory of block motion.

关键词

岩崩/动力破碎/离散元法/Weibull分布/坡面撞击

Key words

rockfall/dynamic fragmentation/discrete element method(DEM)/Weibull distribution/slope impact

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基金项目

国家自然科学基金创新研究群体项目(41521002)

四川省自然科学基金(2023NSFSC0264)

出版年

2024
地质科技通报
中国地质大学(武汉)

地质科技通报

CSTPCDCSCD北大核心
影响因子:1.018
ISSN:2096-8523
参考文献量31
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