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基于PFC3D-GBM的晶体–单元体尺寸比对花岗岩动态拉伸特性影响分析 被引量:12
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作者 张涛 蔚立元 +3 位作者 鞠明和 李明 苏海健 季浩奇 《岩石力学与工程学报》 EI CAS CSCD 北大核心 2022年第3期468-478,共11页
为从矿物颗粒尺度上探究花岗岩的动态拉伸力学行为,提出一种新型的基于颗粒流方法(particle flow code,PFC)的三维等效晶质模型(grain-basedmodel,GBM),并利用FDM-DEM耦合建模技术构建三维分离式霍普金森压杆(splitHopkinsonpressurebar... 为从矿物颗粒尺度上探究花岗岩的动态拉伸力学行为,提出一种新型的基于颗粒流方法(particle flow code,PFC)的三维等效晶质模型(grain-basedmodel,GBM),并利用FDM-DEM耦合建模技术构建三维分离式霍普金森压杆(splitHopkinsonpressurebar,SHPB)模拟系统。利用该系统对模拟岩样进行动态半圆弯拉(semi-circular bending,SCB)试验,探究试样破裂过程,并讨论晶体-单元体尺寸比对花岗岩动态拉伸力学行为的影响。研究结果表明:动载作用下的试样内部裂纹数目演化过程可分为萌生、缓慢增长、急速增长、趋于稳定4个阶段,且拉伸破坏是引起试样整体破裂的主要力学机制。随着晶体-单元体尺寸比的增加,试样晶内接触数量占总接触数量的比值逐渐上升并趋于稳定,而晶间接触占比则相应减小。试样破坏后产生的晶内裂纹数量占总裂纹数量的比值逐渐增大,导致试样发生宏观断裂时所需的外部荷载值上升,因此其动态抗拉强度上升且逐渐趋于稳定。PFC3D-GBM在研究晶质性岩石动力学方面具有可行性,是从矿物颗粒尺度上进行岩石力学探究的有力工具。 展开更多
关键词 岩石力学 三维矿物晶体模型 晶体–单元体尺寸比 动态拉伸 微裂纹特征
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Influence of grain size on strength of polymineralic crystalline rock: New insights from DEM grain-based modeling 被引量:7
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作者 Jun Peng Louis Ngai Yuen Wong Cee Ing Teh 《Journal of Rock Mechanics and Geotechnical Engineering》 SCIE CSCD 2021年第4期755-766,共12页
Grain size effect on rock strength is a topic of great interest in geotechnical engineering.A consensus obtained from earlier laboratory tests is that rock strength generally decreases with the increase of grain size ... Grain size effect on rock strength is a topic of great interest in geotechnical engineering.A consensus obtained from earlier laboratory tests is that rock strength generally decreases with the increase of grain size for both silicate and carbonate rocks;however,some recent numerical results conflict with such laboratory test results.To address this intriguing issue,the effect of grain size on strength of polymineralic crystalline rock with low porosity is investigated numerically using the grain-based modeling(GBM)approach in discrete element method(DEM)by interpreting micro-cracking process in response to loading.In agreement with some previous DEM simulation results,the simulated rock strength is found to increase with increasing grain size for both homogeneous and heterogeneous models,even when the number of assembled disks in one mineral grain changes.The mechanism of strength increase with increasing grain size is mainly associated with the number of assembled smooth-joint contacts along grain interfaces and the generation of grain boundary cracks in response to loading.The grain interfaces significantly weaken the integrity of the rock model,which is similar to effects of inherent defects in real rock.As the grain size increases,fewer grain interfaces are built in the model and the rock strength becomes much higher.Hence,by solely changing the mineral grain size in a model,the mechanism of grain size effect as observed in laboratory tests cannot be replicated.To address this issue,a method of degradation of grain boundary strength parameters is used to mimic the possible mechanism of grain size effect.The simulated strength using the method becomes comparable with those obtained from laboratory tests when the heterogeneity in the rock is considered.Degradation of grain boundary parameters with increasing grain size provides a plausible explanation for the grain size effect on rock strength. 展开更多
关键词 Grain size Rock strength Grain-based modeling(GBM)approach Grain boundary micro-cracking behavior
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循环加载强化作用对花岗岩细观破坏影响的离散元研究
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作者 张霄 于昊 +4 位作者 李壮 刘衍顺 张紫东 籍鑫雨 李相辉 《浙江大学学报(工学版)》 EI CAS CSCD 北大核心 2022年第11期2303-2312,共10页
基于室内单轴压缩试验结果,采用离散元方法建立等效晶质模型(GBM).根据室内循环加卸载试验结果改进GBM模型晶内、晶间接触模型,建立能够准确表征循环加载强化作用的GBM强化模型,借此GBM强化模型揭示循环加载强化作用对花岗岩单轴压缩过... 基于室内单轴压缩试验结果,采用离散元方法建立等效晶质模型(GBM).根据室内循环加卸载试验结果改进GBM模型晶内、晶间接触模型,建立能够准确表征循环加载强化作用的GBM强化模型,借此GBM强化模型揭示循环加载强化作用对花岗岩单轴压缩过程细观破坏的影响机制.结果表明,在峰前应力阶段,自锁效应造成的应力分布不同,导致晶内/晶间接触出现以张拉为主的裂纹,石英、长石依次成为承载主体;在峰后应力阶段,前期强化作用所积蓄的剪切能量得到释放,导致长石出现密集的晶内裂纹,是试块失稳的主要标志;长石周边矿物差异性失效引起长石矿物破坏路径改变,造成试块峰值应力随强化系数增大呈现波动性增长.构建的GBM强化模型为研究循环加载强化作用对脆性岩石不同加载路径细观破坏机制提供新方法. 展开更多
关键词 花岗岩 循环加载强化作用 离散元 GBM强化模型 微裂纹特征 细观破坏机理
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