首页> 外文期刊>Granular matter >Calibration of micro-scaled mechanical parameters of granite based on a bonded-particle model with 2D particle flow code
【24h】

Calibration of micro-scaled mechanical parameters of granite based on a bonded-particle model with 2D particle flow code

机译:基于带有二维颗粒流代码的键合颗粒模型的花岗岩微尺度力学参数校准

获取原文
获取原文并翻译 | 示例
           

摘要

From a microscopic perspective, the mechanical behavior of rocks can be well simulated by particle discrete element method. However, the ideal mechanical properties under macroscopic compression and tension conditions of the granular system require not only reasonable micro-parameters but also consider the mineral distribution in rock microstructure. In this study, the internal microstructure of granite was characterized based on digital images. The cellular automata method was used to construct a discrete element model of clustered particles, and a rapid and effective calibration method for rock microscopic parameters was established. Numerical results significantly relate with laboratory test results, and the microscopic mechanical parameters of the rock were rapidly predicted. Clustered discrete element model simulated the macroscopic mechanical behavior of the investigated rock by considering microscopic rock structure while ignoring particle shape. Results showed that bond strength ratio of the filler-matrix in the numerical sample can significantly affect the compressive-tensile strength ratio. Further, the internal mineral proportion and degree of mineral contact damage strongly influenced the macroscopic mechanical behavior of the investigated rock. Results of this study can provide basis for the construction of micro-scaled model and calibration of microscopic parameters for investigation of rock mechanical behavior.
机译:从微观角度看,岩石的力学行为可以通过粒子离散元法很好地模拟。然而,在颗粒系统的宏观压缩和拉伸条件下,理想的机械性能不仅需要合理的微观参数,而且还需要考虑岩石微观结构中的矿物分布。在这项研究中,基于数字图像表征了花岗岩的内部微观结构。利用元胞自动机方法建立了簇状颗粒的离散元模型,建立了一种快速有效的岩石微观参数标定方法。数值结果与实验室测试结果显着相关,并且可以快速预测岩石的微观力学参数。聚集离散元模型通过在不考虑颗粒形状的情况下考虑微观岩石结构来模拟被研究岩石的宏观力学行为。结果表明,数值样品中填料基体的结合强度比可以显着影响抗压强度比。此外,内部矿物比例和矿物接触破坏程度强烈影响了被调查岩石的宏观力学行为。这项研究的结果可以为微观模型的建立和微观参数的标定提供基础,以研究岩石的力学行为。

著录项

  • 来源
    《Granular matter》 |2019年第2期|38.1-38.13|共13页
  • 作者单位

    Hohai Univ, Key Lab, Minist Educ Geomech & Embankment Engn, Nanjing 210098, Jiangsu, Peoples R China|Hohai Univ, Inst Geotech Res, Nanjing 210098, Jiangsu, Peoples R China;

    Hohai Univ, Key Lab, Minist Educ Geomech & Embankment Engn, Nanjing 210098, Jiangsu, Peoples R China|Hohai Univ, Inst Geotech Res, Nanjing 210098, Jiangsu, Peoples R China;

    Hohai Univ, Key Lab, Minist Educ Geomech & Embankment Engn, Nanjing 210098, Jiangsu, Peoples R China|Hohai Univ, Inst Geotech Res, Nanjing 210098, Jiangsu, Peoples R China;

    Hohai Univ, Key Lab, Minist Educ Geomech & Embankment Engn, Nanjing 210098, Jiangsu, Peoples R China|Hohai Univ, Inst Geotech Res, Nanjing 210098, Jiangsu, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Microscopic structure; Particle flow code; Discrete element method; Compressive-tensile strength ratio;

    机译:微观结构;颗粒流代码;离散元法;抗压强度比;

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

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