新海底电缆地震和海啸观测系统的信息通信技术增强

M. Shinohara, Tomoaki Yamada, S. Sakai, H. Shiobara, T. Kanazawa
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引用次数: 5

摘要

一种新的海底电缆地震和海啸观测系统(OBCST)已经开发出来,以取代现有的海底电缆观测系统,该系统位于日本三陆附近,其登陆站在2011年东北地震的海啸中遭到破坏。直到2010年,我们已经在日本海的浅岛附近开发并安装了新的紧凑型海底电缆地震仪(OBCS)系统。安装完成后,OBCS系统连续运行,我们获得了3年多的连续地震数据。三陆外地区的OBCST系统基于Awashima系统,其特点是采用TCP/IP技术实现系统可靠性,并采用最新电子设备缩小观测节点的尺寸。与第一个系统相比,新的OBCST系统具有新的功能。系统的以太网升级为千兆比特,观测节点时钟可以通过TCP/IP协议同步,精度达到300ns (IEEE 1588)。此外,以太网供电技术使我们能够为额外的传感器配备外部端口。电缆系统安装后,可以使用遥控车辆增加/更换科学传感器。我们计划在2015年安装新的OBCST系统。该系统有两个观测节点,带有三分量加速度计和用于海啸观测的压力表,一个节点带有加速度计和用于海底附加传感器的外部端口。实际系统的总长度约为100公里,观测节点的间隔约为30公里。目前,我们正在制作新的OBCST的观测节点。本文详细介绍了一种新型OBCST系统,并给出了安装方案。
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New ocean bottom cabled seismic and tsunami observation system enhanced by ICT
A new Ocean Bottom Cabled Seismic and Tsunami observation system (OBCST) has been developed for replacement of the existing cabled observation system off Sanriku, Japan, whose landing station was damaged by tsunamis of the 2011 Tohoku earthquake. Until 2010, we had already developed and installed the new compact Ocean Bottom Cabled Seismometer (OBCS) system near Awashima-island in the Japan Sea. After the installation, the OBCS system is being operated continuously and we have continuous seismic data for more than 3 years. The new OBCST system for off-Sanriku area is based on the Awashima system, and is characterized by system reliability using TCP/IP technology and down-sizing of an observation node using up-to-date electronics. The new OBCST system has new functions compared to the first system. An Ethernet of the system is upgraded to Giga-bit and clocks in observation nodes can be synchronized through TCP/IP protocol with an accuracy of 300 ns (IEEE 1588). In addition, power over Ethernet technology enables us to equip an external port for additional sensors. After installation of the cabled system, a scientific sensor can be added/replaced by using remotely operated vehicle. We have a plan to install the new OBCST system in 2015. The system has two observation nodes with three-component accelerometers and pressure gauge for tsunami observation and one node with accelerometers and an external port for additional sensors on seafloor. Total length of the practical system is approximately 100 km and an interval of the observation node is about 30 km. At the present, we are producing the observation nodes of the new OBCST. In this paper, we present a system of the new OBCST in detail, and installation plan.
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