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人工震源地下介质变化动态监测

Monitoring Subsurface Changes with Active Sources

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【作者】 王宝善王伟涛葛洪魁徐平王彬

【Author】 Wang Baoshan1,Wang Weitao1,Ge Hongkui1,Xu Ping2,Wang Bin3(1.Institute of Geophysics,China Earthquake Administration,Beijing 100081,China;2.Earthquake Administration of Beijing,Beijing 100080,China; 3.Earthquake Administration of Yunnan Province,Kunming 650024,China)

【机构】 中国地震局地球物理研究所北京市地震局云南省地震局

【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地震波,进行地下介质监测自然成为一个重要的发展方向。系统地介绍了国内外利用人工震源进行不同尺度地下介质变化监测的研究,分析了不同震源的优缺点。根据分析和对比结果,认为在进行地下介质变化研究方面,气枪震源要优于其他震源。还介绍了相关的数据处理方法,包括互相关延时估计,尾波干涉和信号叠加等。目前用于大尺度地下动态监测的震源,接收和数据处理等主要技术已经基本发展成熟,利用人工震源进行地下介质大尺度监测成为可能,相关研究在减轻自然灾害和资源探查等领域具有广阔的应用前景。

【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.

【基金】 国家自然科学基金项目“地下介质变化四维地震监测关键技术和理论的实验研究”(编号:40874095);国家自然科学基金重点项目“地震波雷达——用人工震源探测大陆地壳结构及其演化”(编号:40730318);地震行业科研专项项目“地震波走时变化的主动源监测技术研究”(编号:200808002)资助
  • 【文献出处】 地球科学进展 ,Advances in Earth Science , 编辑部邮箱 ,2011年03期
  • 【分类号】P631.4
  • 【被引频次】45
  • 【下载频次】235
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