首页> 美国卫生研究院文献>Materials >Numerical Study on Crack Propagation in Brittle Jointed Rock Mass Influenced by Fracture Water Pressure
【2h】

Numerical Study on Crack Propagation in Brittle Jointed Rock Mass Influenced by Fracture Water Pressure

机译:断裂水压对脆性节理岩体裂纹扩展影响的数值研究

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

The initiation, propagation, coalescence and failure mode of brittle jointed rock mass influenced by fissure water pressure have always been studied as a hot issue in the society of rock mechanics and engineering. In order to analyze the damage evolution process of jointed rock mass under fracture water pressure, a novel numerical model on the basis of secondary development in fast Lagrangian analysis of continua (FLAC3D) is proposed to simulate the fracture development of jointed rock mass under fracture water pressure. To validate the feasibility of this numerical model, the failure process of a numerical specimen under uniaxial compression containing pre-existing fissures is simulated and compared with the results obtained from the lab experiments, and they are found to be in good agreement. Meanwhile, the propagation of cracks, variations of stress and strain, peak strength and crack initiation principles are further analyzed. It is concluded that the fissure water has a significant reducing effect on the strength and stability of the jointed rock mass.
机译:裂隙水压力影响下的脆性节理岩体的萌生,传播,聚结和破坏模式一直是岩石力学与工程社会研究的热点问题。为了分析裂隙水压力下节理岩体的破坏演化过程,提出了基于快速拉格朗日连续性分析二次发展的新数值模型(FLAC3D),以模拟裂隙水下节理岩体的裂缝发展。压力。为了验证该数值模型的可行性,模拟了包含预先存在的裂缝的单轴压缩数值试样的破坏过程,并将其与实验室实验的结果进行了比较,发现它们具有良好的一致性。同时,进一步分析了裂纹的扩展,应力和应变的变化,峰值强度和裂纹萌生原理。结论是,裂隙水对节理岩体的强度和稳定性具有显着的降低作用。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号