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人工震源地下介质变化动态监测
引用本文:王宝善,王伟涛,葛洪魁,徐平,王彬.人工震源地下介质变化动态监测[J].地球科学进展,2011,26(3):249-256.
作者姓名:王宝善  王伟涛  葛洪魁  徐平  王彬
作者单位:王宝善,王伟涛,葛洪魁,Wang Baoshan,Wang Weitao,Ge Hongkui(中国地震局地球物理研究所,北京,100081);徐平,Xu Ping(北京市地震局,北京,100080);王彬,Wang Bin(云南省地震局,云南,昆明,650024)
基金项目:国家自然科学基金项目,国家自然科学基金重点项目,地震行业科研专项项目
摘    要:成像地球内部介质结构及其动态变化是地球物理学家的主要任务.相对于对地球介质静态结构的认识,对于地下介质性质随时间变化的了解明显不足.近年来随着观测资料的增加,已经开始利用重复地震和噪声等震源研究地下介质变化.受到源位置和时间等因素制约,基于地震和噪声等被动震源的观测结果的时间和空间分辨率有限.利用人工震源主动向地下发射...

关 键 词:人工震源  波速变化  气枪震源  精密可控震源

Monitoring Subsurface Changes with Active Sources
Wang Baoshan,Wang Weitao,Ge Hongkui,Xu Ping,Wang Bin.Monitoring Subsurface Changes with Active Sources[J].Advance in Earth Sciences,2011,26(3):249-256.
Authors:Wang Baoshan  Wang Weitao  Ge Hongkui  Xu Ping  Wang Bin
Institution:1.Institute of Geophysics, China Earthquake Administration, Beijing100081, China; 2. Earthquake Administration of Beijing,Beijing100080,China; 3. Earthquake Administration of Yunnan Province,Kunming650024, China
Abstract:To provide images of Earth interior and their temporal variations are main tasks for geophysicists. Comparing to our understanding of the static structure, we are still lacking in the understanding of the temporal variations of the subsurface. Recently, with the accumulation of observation data, repeated earthquakes and ambient noises are used to monitor subsurface changes. The resolutions and precisions of passive source monitoring are limited by the spatial and temporal distributions of sources. Monitoring subsurface changes with seismic wave generated by artificial sources naturally becames another goal to pursue. We systematically describe recent advances in active source monitoring at various scales. In this review, we also introduce cross-correlation based time delay estimation and its precision limitation. The precision of time delay estimation is limited by the repeatability of source, signal-to-noise ratio and bandwidth of recorded signals. And seismic sources with large capacity and high repeatability are preferred for active monitoring. Advantages and disadvantages of different sources are compared in this review. According to the comparison, we suggest that the airgun source is superior to other sources for the purpose of active monitoring. Techniques as waveform stacking, coda wave interferometry and their application in active monitoring are also introduced. Waveform stacking can be used to enhance the signal-to-noise ratio and facilitate the phase identification. Coda wave travels longer and is more sensitive to subsurface changes than direct waves. Therefore, coda wave interferometry technique can be used to detect subtle variations. With the development of techniques for signal excitation, recording and processing, it is now possible to conduct large scale active subsurface monitoring. Relevant researches have broad potential applications to such fields as natural disaster mitigation and resource exploration.
Keywords:Active source  Velocity changes  Airgun source  Accurately controlled seismic source  
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