温度与荷载对砂岩动态力学性能及裂纹的影响Effect of temperature and load on dynamic mechanical properties and cracks of sandstone
徐颖;王崑;邵彬彬;
XU Ying;WANG Kun;SHAO Bin-bin;School of Civil Engineering Architecture, Anhui University of Science and Technology;
摘要(Abstract):
为研究在不同温度与荷载下砂岩的动态力学性能,运用了SHPB实验仪器及配套高温环境箱分别在25(常温)、100、200、300、400、500、600、700℃下对砂岩进行3种不同荷载(0.3、0.5、0.7 MPa)动态压缩实验,并结合SEM设备对高温应力作用下砂岩内部裂纹进行分析。结果表明:当冲击荷载增大时,砂岩所能承受的动态压缩强度显著提高;当所处温度一定时,其破裂情况也随荷载的增大而加剧;当冲击气压一定时,随着温度升高,砂岩的峰值应力表现出平缓、上升、下降的变化趋势,最终在700℃时达到最小值。在应力与常温作用下,试件会先以应力作用影响为主,出现单条裂纹,当温度升高至300℃以上,单条裂纹会有所延伸并形成多条裂纹,出现二次开裂。
To study the dynamic mechanical properties of sandstone under different temperatures and loads, three different load(0.3,0.5,0.7 MPa)dynamic compression experiments were carried out on sandstone at 25(normal temperature),100,200,300,400,500,600,700 ℃ by using SHPB experimental instruments and supporting high temperature environmental boxes, respectively, and the internal cracks of sandstone under high temperature stress were analyzed in combination with the SEM equipment. The results show that when the impact load increases, the dynamic compressive strength of sandstone increases significantly, and when the temperature is fixed, the rupture condition increases with the load. When the impact air pressur is fixed with the temperature rises, the peak stress of sandstone should be force shows a gentle, rising, decreasing trend of change, and finally reaches the minimum at 700 ℃. Under the action of stress and normal temperature, the main effect of stress is the single crack. As the temperature rises to more than 300 ℃, a single crack will extend and form multiple cracks, and secondary cracking will occur.
关键词(KeyWords):
砂岩;高温;SHPB;峰值应力;裂纹
sandstone;high temperature;Separated Hopkinson Pressure Bar;peak stress;cracks
基金项目(Foundation):
作者(Authors):
徐颖;王崑;邵彬彬;
XU Ying;WANG Kun;SHAO Bin-bin;School of Civil Engineering Architecture, Anhui University of Science and Technology;
参考文献(References):
- [1] 李倩琪.中国经济增长的煤炭依赖与解耦路径研究[D].徐州:中国矿业大学,2019.LI Q Q.Coal dependence and decoupling path of China's economic growth[D].Xuzhou:China University of Mining and Technology,2019.
- [2] 何满潮,谢和平,彭苏萍,等.深部开采岩体力学研究[J].岩石力学与工程学报,2004,24(16):2 803-2 814.HE M C,XIE H P,PENG S P,et al.Study on rock mass mechanics in deep mining [J].Journal of Rock Mechanics and Engineering.2004,24(16):2 803-2 814.
- [3] 谢和平,彭苏萍,何满潮.深部开采基础理论研究与工程实践[M].北京:科学出版社,2006:3-14.XIE H P,PENG S P,HE M C.Basic theory research and engineering practice of deep mining[M].Beijing:Science Publishing House.2006:3-14.
- [4] ALM O,JAKTLUND L L,SHAO Q K.The influence of microcrack density on the elastic and fracture mechanical properties of stripa granite[J].Physics of the Earth & Planetary Interiors,1985,40(3):161-179.
- [5] ATKINSON B K.Mieroselsmic Activity in Geologic Structures and Materials[C]//Proc.3rd Int:Conf on AE Leighton,1984.
- [6] 寇绍全.热开裂损伤对花岗岩变形及破坏特性的影响[J].力学学报,1987,19(6):550-555.KOU S Q.Effect of thermal cracking damage on deformation and failure characteristics of granite [J].Journal of Mechanics.1987,19(6):550-555.
- [7] 罗生银,窦斌,田红,等.自然冷却后与实时高温下花岗岩物理力学性质对比试验研究[J].地学前缘,2020,27(1):178-184.LUO S Y,DOU B,TIAN H,et al.Experimental study on physical and mechanical properties of granite after natural cooling and real-time high temperature [J].Geoscience Frontiers ,2020,27(1):178-184.
- [8] 许锡昌,刘泉声.高温下花岗岩基本力学性质初步研究[J].岩土工程学报,2000,20(3):332-335.XU X C,LIU Q S.A preliminary study on the basic mechanical properties of granite at high temperature [J].Journal of Geotechnical Engineering.2000,20(3):332-335.
- [9] 王德荣,刘昭言,刘家贵,等.砂岩和花岗岩的动态性能与能量耗散分析[J].北京理工大学学报,2017,37(12):1 217-1 223.WANG D R,LIU Z Y,LIU J G,et al.Dynamic properties and energy dissipation analysis of sandstone and granite[J].Journal of Beijing Institute of Technology ,2017,37(12):1 217-1 223.
- [10] 基姆弗兰克林,张受天.国际岩石力学学会试验方法委员会确定岩石应力的建议方法[J].岩石力学与工程学报,1988(4):357-388.FRANKLIN K,ZHANG S T.Recommended method for determination of rock stress by the commission on test methods of the international society of rock mechanics [J].Journal of Rock Mechanics and Engineering ,1988(4):357-388.