落石碰撞破碎概率及碎片分布特征研究
批准号:
42107175
项目类别:
青年科学基金项目(C类)
资助金额:
30.0 万元
负责人:
叶阳
依托单位:
学科分类:
工程地质环境与灾害
结题年份:
2024
批准年份:
2021
项目状态:
已结题
项目参与者:
叶阳
中文摘要
我国西南地区,尤其是川藏铁路沿线,存在大量高陡层状碎裂岩质边坡,致使落石灾害频发。由于高位落石与坡面碰撞速度大,崩塌后常发生剧烈破碎。破碎显著改变了落石运动轨迹,使得轨迹预测变得更加困难,导致难以设计合理的落石防护措施。因此,本项目以落石碰撞破碎为核心,考虑落石外形及内在节理两个关键因素,围绕落石碰撞破碎概率及碎片分布两个科学问题开展研究。本课题通过高陡层状碎裂岩质边坡原位地质调查,对落石外形及内在节理进行量化;通过落石碰撞破碎室内试验,揭示外形及内在节理对破碎概率及碎片分布的影响;基于碰撞破碎三维离散元精细模拟方法,开展落石碰撞破碎模拟,阐明破碎细观机理,并开展更复杂条件下落石碰撞破碎模拟。基于试验及模拟结果,建立碰撞破碎概率和碎片分布理论模型;基于提出的理论模型,开发考虑破碎的落石运动轨迹三维离散元快速分析方法,实现破碎条件下落石轨迹的准确预测,为防护措施设计提供合理依据。
英文摘要
Many high rock slopes with layered cataclastic structure exist in Southwest China, especially along the constructing Chuanzhang railway, which result in frequent occurrence of rockfall. The rockfall at high and steep rock slope has high impact velocity and thus the rockfall fragmentation is common. Rockfall fragmentation significantly changes rockfall trajectory, and the precise trajectory prediction and reasonable rockfall protection measures are more difficult. Hence, the study focuses on rockfall fragmentation, which refers to two questions-breakage probability and fragment distribution. The crucial factors of complex shape and internal discontinuities are considered. In this study, the in-situ geological surveys of rock slope and rockfall are conducted to analyze the complex shape of rockfall blocks and the discontinuities comprehensively and quantitatively; the laboratory tests are performed to indicate the effect of block shape and discontinuities on breakage probability and fragment distribution; through the proposed precise rock block fragmentation modelling method, the three-dimensional discrete element method simulations of rockfall impact are performed to reveals the fragmentation mechanisms, and simulations with more complex shape and internal discontinuities are conducted to supplements the laboratory tests; based on the laboratory and simulated results, the breakage probability and fragment size and velocity models are proposed; based on the proposed models, the fast three-dimensional discrete element method of rockfall trajectory considering fragmentation is developed. The accurate rockfall trajectory can be predicted through the proposed method, which provides a reasonable basis for the design of protective measures.
落石灾害常发生在我国西南地区广泛分布的高陡碎裂岩质边坡。高陡碎裂岩质边坡落石启动位置高,与坡面碰撞速度大,碰撞破碎现象频繁发生。落石碰撞破碎不仅大量增加飞溅的块石,同时显著改变落石运动轨迹。本项目以落石碰撞破碎现象为研究对象,针对落石破碎概率及碎片分布特征开展研究。首先,针对典型碎裂岩质边坡开展了精细野外调查,基于三维激光扫描技术研究了边坡结构和落石形状特征,得到落石形态及结构特征统计规律;针对落石碰撞破碎理论问题,开展了室内块石接触力学试验,揭示了块石破碎模式和接触力位移曲线规律,阐明了多次加载条件下块石损伤破碎演化规律,提出弹塑性接触力学模型用于模拟落石碰撞耗能过程;为模拟研究落石碰撞破碎机理,本项目提出岩石非线性压密特性三维离散元模拟方法和岩石力学参数离散性模拟方法;岩石非线性压密特性模拟方法能够准确模拟落石碰撞损伤破碎能耗过程;基于提出的初始微裂隙分布模型,实现了岩石弹性模量、泊松比、抗压强度和抗拉强度平均值及标准差的准确模拟,为模拟研究落石碰撞破碎概率及其演化规律提供可靠方法;本项目研发了一套落石碰撞破碎室内模型试验平台,实现了落石碰撞破碎过程观测及破碎表面积精确测量;基于该平台,开展了大量落石碰撞破碎模型试验研究,揭示了落石外形、内在结构面、接触类型等对落石碰撞破碎概率、破碎模式、碎片分布及形状演化的影响;采用提出的落石碰撞破碎三维离散元精细数值模拟方法,针对落石碰撞破碎机理及碎片运动进行模拟研究,揭示了三种典型破碎模式(局部粉碎、膨胀劈裂、弹性波拉伸劈裂),阐明了多次碰撞的累计效应及相互作用机理;基于破碎功指标,提出了落石多次碰撞破碎概率模型,理论结果与室内试验及数值模拟结果保持一致;最后提出了一种落石碰撞运动轨迹三维离散元数值模拟方法,并应用在青海哇让抽水蓄能电站典型岩质边坡崩塌落石运动轨迹评估中,为该工程的落石防护设计提供重要支撑。
国内基金
海外基金