动静荷载作用下岩石裂纹扩展应力阈值识别  

Identification of stress thresholds for crack propagation of rock under quasi-static and dynamic loadings

作　　者：李地元[1] 周奥辉 陈昱达 马金银 LI Diyuan;ZHOU Aohui;CHEN Yuda;MA Jinyin(School of Resources and Safety Engineering,Central South University,Changsha 410083,Hunan,China)

机构地区：[1]中南大学资源与安全工程学院,湖南长沙410083

出　　处：《爆炸与冲击》2023年第10期57-70,共14页Explosion and Shock Waves

基　　金：国家自然科学基金面上项目(52074349)。

摘　　要：压缩荷载作用下岩石裂纹扩展应力阈值的识别是理解岩石渐进破坏过程和分析岩石宏观破坏机制的重要基础。对大理岩、粗花岗岩和细花岗岩开展了单轴压缩和动态冲击试验,引入岩石裂纹轴向应变和裂纹径向面积应变两个参数,根据岩石单轴压缩破坏时裂纹径向面积应变曲线斜率的不同,把以上三种岩石分成类型Ⅰ(大理岩)和类型Ⅱ(粗花岗岩和细花岗岩)岩石。研究表明,对于类型Ⅰ和类型Ⅱ岩石,分别利用其裂纹轴向应变和裂纹轴向应变刚度曲线特征点能准确识别出岩石在静态压缩荷载下裂纹稳定扩展应力σ_(sd)、裂纹不稳定扩展应力σusd以及裂纹相互贯通应力σct,证明了仅利用轴向应变数据就可对类型Ⅰ和类型Ⅱ岩石静荷载下应力阈值进行识别。而后将裂纹轴向应变法推广至动态冲击荷载下岩石的应力阈值识别,解决了动态冲击压缩载荷作用下试样难以进行裂纹扩展应力阈值识别的问题。与静态荷载下岩石的裂纹扩展应力阈值不同,在动态冲击荷载下,岩石裂纹稳定扩展应力与峰值强度的比值有所减小,裂纹不稳定扩展应力和裂纹相互贯通应力阈值相等,且与峰值强度的比值也有所减小,岩石产生更多的贯通裂纹,试样破坏时破碎程度更高。The identification of stress threshold for crack propagation of rock under compressive loading is an important issue for understanding the progressive damage process and analyzing the macroscopic damage mechanism of rocks.In order to accurately identify the stress threshold of brittle hard rock under quasi-static and dynamic compressive loads,uniaxial and dynamic compression tests were carried out for three kinds of rock specimens(including marble,coarse granite and fine granite)by using an INSTRON 1346 and a split Hopkinson pressure bar(SHPB)system.Two deformation parameters were introduced in the paper,including crack axial strain and crack radial area strain.According to the slope difference of the crack radial area strain curves at the failure point,the three kinds of rocks were classified into typeⅠ(marble)and typeⅡ(coarse granite and fine granite)rocks.The testing results indicate that the crack axial strain curves and crack axial strain stiffness curves can be used to accurately identify the crack stability propagation stressσ_(sd),crack instability propagation stressσusd and the crack connectivity stressσct under quasi-static compressive loading for typeⅠand typeⅡrocks respectively.It is proved that the stress thresholds of typeⅠand typeⅡrocks can be identified only by using the axial strain data.The method based on crack axial strain is extended to identify the stress threshold of rock under dynamic impact loading.It solves the problem to identify the stress threshold of rock specimens under dynamic compressive loading.Different from the stress threshold of rock under quasi static loading,it is found that the ratio of the crack stability propagation stress to the peak strength of the rock decreases under dynamic loading.The crack instability propagation stress and the crack connectivity stress coincide with each other,and the ratio to the peak strength also decreases.When the specimen is failed under dynamic loading,it usually generates more penetrating cracks and more fragments than that

关 键 词：裂纹扩展 应力阈值识别 裂纹轴向应变 动态冲击荷载 裂纹径向面积应变 

分 类 号：O347.3[理学—固体力学]