摘要
以透明试件受压破裂过程模拟均匀岩体的破裂过程 ,用实时全息干涉摄影系统记录试件应力场分布及其变化 ,用瞬态波形自动记录仪记录微破裂的位置和强度 .通过两种方式所获数据来探索地震微破裂成核过程与应力场关系 .
The fracture process of transparent samples are used in this paper to simulate that of a homogeneous rock mass. In order to discover relationships between the micro_fracture nucleation and its surrounding stress field, a real_time holographic optical setup is used to record the distribution and variations of the samples' stress fields and the transient wave_form automatic recorder is used to record the location and intensity of the micro_fractures. The initial research has brought about some phenomena worthy of notice. This method has provided us with a new approach to make a seismic experimental research.
出处
《地球科学（中国地质大学学报）》
EI
CAS
CSCD
北大核心
2000年第3期319-323,共5页
Earth Science-Journal of China University of Geosciences
基金
国家自然科学基金资助项目!(No .46764 0 10 )
云南省科委应用基础研究基金资助项目!(No .97D0 2 7Q)
关键词
地震波
微破裂
应力场
地震
实验模拟
成核过程
real_time holography
seismic wave
micro_fracture
stress (strain) field.
