海底的地球物理观测

J. Kasahara
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引用次数: 2

摘要

根据板块构造理论,环太平洋海沟系是大洋板块的俯冲带。这些俯冲带是大地震的震源区,在日本和台湾造成了巨大的破坏。三十年来的地震学研究表明,这些地震是由俯冲的大洋板块和大陆板块之间的摩擦滑动引起的。如果我们能在大地震前监测到板块边界的前兆滑动,就有可能减少地震的破坏。前兆地震活动和/或滑动可以通过海底地震仪和/或大地测量仪器来观测。为了监测深海地震活动,我们研制了自由落体-弹出式数字海底地震仪。除了使用自由落体弹出式海底地震仪进行非实时地震观测外,还使用了能够进行实时观测的海底电缆海底地震仪。日本有许多科学的海底电缆系统。每个海底电缆系统长近100公里。有些使用光纤,有些使用同轴电缆。我们还研究了使用退役的海底电信电缆的可能性。位于Izu-Bonin海沟2800 m海底的GeO-TOC电缆OBS运行了5年,连续为日本地震台网带来了重要的地震和水听器数据。使用GOGC海底电缆的VENUS电缆系统是部署在冲绳岛附近的测试系统,运行了两个月。这是一个跨学科的海底观测站。在美国和加拿大,NEPTUNE(东北太平洋时间序列海底网络实验)项目打算在温哥华岛、蒙特利湾和卡斯卡迪亚-胡安-德富卡附近安装科学海底电缆系统。在日本,已经提出了ARENA项目。为了使这一项目经济成功,需要国际合作,因为从主要海底电缆分支需要技术突破。电源系统、海底可匹配连接器和故障安全系统的发展是关键。这些新技术的发展将对海洋工程领域作出巨大贡献。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geophysical observations at the ocean bottom
Trench systems surrounding the circum Pacific Ocean are the subduction zones of the oceanic plates according to plate tectonics. These subduction zones are the source regions generating large earthquakes which caused huge damage in Japan and Taiwan. Seismological studies during three decades suggest that these earthquakes are caused by frictional slip between the subducting oceanic plate and the continental plate. If we can monitor any precursory slips at the plate boundary prior to the large earthquakes, it may be possible to reduce the earthquake damage. The precursory seismic activities and/or slip can be observed by seismometers, and/or geodetic instruments at the ocean bottom. In order to monitor the seismic activity at deep ocean, we developed free-fall-pop-up digital ocean bottom seismometers (OBSs). In addition to non-real time seismic observation using free-fall-pop-up OBSs, submarine cable OBSs enabling real-time observation have been used. There are many scientific submarine cable systems in Japan. Each submarine cable system is nearly 100 km long. Some use optical fibers and others use coaxial cables. We also examined the possibility of using decommissioned telecommunication submarine cables. The GeO-TOC cable OBS located at the 2800 m depth of ocean bottom along the Izu-Bonin Trench was operated for 5 years and brought important seismic and hydrophone data to the Japanese seismic network continuously. The VENUS cable system using the GOGC submarine cables was the test system deployed off Okinawa Island and operated for two months. It was an interdisciplinary ocean bottom observatory. In USA and Canada, the NEPTUNE (North East Pacific Time-series Undersea Networked Experiment) project is intending to install scientific submarine cables systems near Vancouver Island, Monterey Bay and off Cascadia-Juan de Fuca. In Japan, the ARENA project has been proposed. To make such a project economical and successful, international cooperation is requested because the branching from the main submarine cable needs a technological breakthrough. The development of power supply systems, undersea mateable connectors and a fail safe system are key points. This development of new technologies may greatly contribute to the ocean engineering field.
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