School of Civil Engineering, Liaoning Technical University, Fuxin, Liaoling, China.
Institute of Geology, China Earthquake Administration, Beijing, China.
PLoS One. 2020 Apr 24;15(4):e0231464. doi: 10.1371/journal.pone.0231464. eCollection 2020.
In deep underground engineering, in a large spatial, high-stress environment, rapid excavation is likely to affect the loading rate of the fault structure and to cause stick-slip. In this study, an experiment was conducted to explore the stick-slip characteristics at different loading rates. A double-sided shear experiment and the digital speckle correlation method were used to analyze the evolution of the displacement field, the slip displacement, and the slip rate of the fault's stick-slip activity at different loading rates as well as their correlation with the loading rate. The loading rate, moment magnitude, and stress drop of the fault's stick-slip and their corresponding relationships were studied. The results show that the occurrence of stick-slip is inversely proportional to the loading rate. The evolution of the fault-slip displacement field at different loading rates is similar. At a given loading rate, the magnitude is positively correlated with the stress drop. The magnitude and stress drop are inversely related to the loading rate.
在深部地下工程中,在大空间、高应力环境中,快速开挖可能会影响断层结构的加载速率,并导致粘滑。在这项研究中,进行了一项实验来探索不同加载速率下的粘滑特性。采用双面剪切实验和数字散斑相关方法,分析了不同加载速率下断层粘滑活动的位移场演化、滑位和滑速,以及它们与加载速率的相关性。研究了断层粘滑的加载速率、矩震级和应力降及其相应的关系。结果表明,粘滑的发生与加载速率成反比。不同加载速率下的断层滑动位移场的演化是相似的。在给定的加载速率下,矩震级与应力降呈正相关。矩震级和应力降与加载速率成反比。