1. 石家庄铁道大学 省部共建交通工程结构力学行为与系统安全国家重点实验室,河北,石家庄,050043
2. 石家庄铁道大学 道路与铁道工程安全保障教育部重点实验室,河北,石家庄,050043
3. 石家庄铁道大学 河北省金属矿山安全高效开采技术创新中心,河北,石家庄,050043
4. 河北科技大学 建筑工程学院,河北,石家庄,050018
网络首发:2021-10-18,
纸质出版:2021
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王伟, 梁渲钰, 张明涛, 等. 动静组合加载下砂岩破坏机制及裂纹密度试验研究[J]. 岩土力学, 2021,42(10):2647-2658.
WANG Wei, LIANG Xuan-yu, ZHANG Ming-tao, et al. Experimental study on failure mechanism and crack density of sandstone under combined dynamic and static loading[J]. 2021, 42(10): 2647-2658.
王伟, 梁渲钰, 张明涛, 等. 动静组合加载下砂岩破坏机制及裂纹密度试验研究[J]. 岩土力学, 2021,42(10):2647-2658. DOI: 10.16285/j.rsm.2021.0095.
WANG Wei, LIANG Xuan-yu, ZHANG Ming-tao, et al. Experimental study on failure mechanism and crack density of sandstone under combined dynamic and static loading[J]. 2021, 42(10): 2647-2658. DOI: 10.16285/j.rsm.2021.0095.
为探讨砂岩在动静组合加载条件下的破坏特征及损伤规律,采用三维动静组合分离式Hopkinson压杆测试系统对砂岩试样进行了多组动静组合、不同加载速率条件下的冲击试验,利用CT扫描与数字岩芯技术得到了砂岩试样内部不同截面的破坏图和损伤后试样内部的三维重构图及裂纹密度,研究了砂岩在不同受力情况下的破坏形式和破坏机制,并对轴压、围压及应变率对砂岩裂纹密度的影响规律进行了探究。试验结果表明:常规动态冲击作用下,砂岩的动态破坏形式为典型的拉伸劈裂破坏;一维动静组合加载下,砂岩的动态破坏形式为典型的压剪破坏,内部呈现出共轭双曲线形的压剪面;三维动静组合加载下,砂岩的动态破坏形式同样表现为压剪破坏,但内部破坏面为圆台(锥)形,并对不同加载条件下砂岩的动态破坏机制进行了分析。在不同加载状态下砂岩的裂纹密度随应变率的增加均呈递增趋势,轴压、围压的施加限制了裂纹的产生和增长速率,围压相对于轴压对裂纹产生和扩展的限制程度更大,并从砂岩的抗压强度和裂纹产生的补偿空间角度对其进行了解释;利用轴压、围压模拟地应力,分析了地下0、200、400、600 m处应变率对砂岩裂纹密度的影响规律,并对其进行了定量分析,若要产生同样效果的裂纹密度,地下600 m处的砂岩所需应变率大约是无地应力状态下的3.4倍。从裂纹密度角度构建了不同加载状态下损伤变量和应变率之间的量化关系式,该研究结果可为无临空面爆破开采过程中不同爆炸应力波与岩石内部裂纹开展程度的量化问题提供了参考。
In order to investigate the failure characteristics and damage law of sandstone under the combined dynamic and static loading conditions
three-dimensional movement combination loading test system with separate Hopkinson compressive bar is applied to perform impact tests on sandstone samples under the condition of multiple combinations of dynamic and static state and different loading rates. CT scan and digital core technology are also used to observe the failure diagrams of different sections in the sandstone sample
and the three-dimensional reconstruction diagram and crack density in the damaged sample are obtained. The failure forms and failure mechanism of sandstone under different stress conditions are studied
and the effects of axial pressure
confining pressure and strain rate on the crack density of sandstone are explored. The test results show that the dynamic failure of sandstone is typical tensile splitting failure under the action of conventional dynamic impact. Under one-dimensional combined dynamic and static loading
the dynamic failure mode of sandstone is typical compression and shear failure
and the interior presents a conjugated double curved compression and shear surface. Under three-dimensional dynamic and static loading
the dynamic failure mode of sandstone is also compression and shear failure
but the internal failure surface is circular (cone) shape. The dynamic failure mechanism of sandstone under different loading conditions is analyzed. Under different loading conditions
the crack density of sandstone increases with the increase of strain rate. The application axial compression and confining pressure restrict the crack generation and growth rate
and the confining pressure has a greater limitation on the crack generation than the axial pressure. It is explained from the perspective of compressive strength and compensation space for crack generation of sandstone. The influence of strain rate on the crack density of sandstone at 0
200
400 m and 600 m underground is analyzed quantitatively by using axial compression and confining pressure to simulate the in-situ stress. To produce the same crack density
the strain rate of sandstone at 600 m underground is about 3.4 times that of sandstone without in-situ stress. The quantitative relationship between damage variables and strain rates under different loading conditions is established from the perspective of crack density. The research results can provide a reference for quantification of different explosion stress waves and the development degree of internal crack in rock during blasting mining without facing surface.
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