zhenbo

ISSN 2096-7780 CN 10-1665/P

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

日本海洋实时监测系统DONET简介

申中寅

申中寅. 日本海洋实时监测系统DONET简介[J]. 地震科学进展, 2018, (7): 34-40. doi: 10.3969/j.issn.0253-4975.2018.07.007
引用本文: 申中寅. 日本海洋实时监测系统DONET简介[J]. 地震科学进展, 2018, (7): 34-40. doi: 10.3969/j.issn.0253-4975.2018.07.007
Zhongyin Shen. A brief introduction to DONET in Japan[J]. Progress in Earthquake Sciences, 2018, (7): 34-40. doi: 10.3969/j.issn.0253-4975.2018.07.007
Citation: Zhongyin Shen. A brief introduction to DONET in Japan[J]. Progress in Earthquake Sciences, 2018, (7): 34-40. doi: 10.3969/j.issn.0253-4975.2018.07.007

日本海洋实时监测系统DONET简介

doi: 10.3969/j.issn.0253-4975.2018.07.007
基金项目: 地震行业科研专项: 中国全球地震台网建设预研(201508007)资助。
详细信息
    通讯作者:

    申中寅,e-mail: shen_zhongyin@163.com

  • 中图分类号: P315

A brief introduction to DONET in Japan

  • 摘要: 近年来,我国地震观测取得了长足进展,同时海底观测系统的建设也方兴未艾。而欧美及日本等发达国家在海底有线实时监测的成功先例,为我国相应工作的开展提供了良好的参考及借鉴。其中日本海底有线实时监测系统DONET始建于2011年,专注于海底地动—水压信号的高效采集,旨在监视日本南海海槽的地震和海啸事件。本文主要介绍DONET的硬件布局、搭建流程以及科研产出情况,并简要介绍我国国家海底科学观测网的基本信息。

     

  • 图  1  DONET分布示意图(原图引自JAMSTEC)

  • [1] 川口 勝義. 深海底リアルタイム観測ネットワークの構築. 日本マリンエンジニアリング学会誌, 2009, 44: 58-63.
    [2] 岡 英太郎 , 磯辺 篤彦 , 市川 香 , et al 海洋学の10年展望(I): 日本海洋学会将来構想委員会物理サブグループの議論から(海洋学の10年展望-「海の研究」特集号-). 海の研究, 2013, 22: 191-218.
    [3] Tonegawa T, Araki E, Kimura T, et al. S-wave velocity structure in the Nankai accretionary prism derived from Rayleigh admittance[C]. EGU General Assembly Conference. EGU General Assembly Conference Abstracts, 2017: 19
    [4] Takaesu M, Horikawa H, Sueki K, et al. Development of an event search and download system for analyzing waveform data observed at seafloor seismic network, DONET[C]. AGU Fall Meeting. AGU Fall Meeting Abstracts, 2014
    [5] Kitada K, Araki E, Kimura T, et al. Long-term monitoring at C0002 seafloor borehole in Nankai Trough seismogenic zone[C]. Underwater Technology Symposium. IEEE, 2013, 20(3): 1-3
    [6] 廖又明. 解读日本ARENA(新型实时海底监测电缆网络)计划. 船舶, 2005(4): 20-25.
    [7] Araki E, Yokobiki T, Kawaguchi K, et al. Background seismic noise level in DONET seafloor cabled observation network[C]. Underwater Technology Symposium. IEEE, 2013, 20(3): 1-4
    [8] Nakano M, Tonegawa T, Kaneda Y. Orientations of DONET seismometers estimated from seismic waveforms. Jamstec Report of Research & Development, 2012, 15: 77-89.
    [9] Matsumoto H, Araki E, Machida Y, et al. Utilization of temperature and pressure simulator for ocean-bottom and bore-hole observatories for quantitative crustal deformation[C]. AGU Fall Meeting. AGU Fall Meeting Abstracts, 2015
    [10] Nishida S, Kawaguchi K, Imaizumi T, et al. An evaluation of the performance of a hydrophone on sea floor[C]. Oceans. IEEE, 2014, 39(6): 1-4
    [11] Fujimoto H, Kido M, Osada Y. Improvement in the observation system for the GPS/A seafloor positioning[C]. AGU Fall Meeting. AGU Fall Meeting Abstracts, 2010, 50(7): 565-568
    [12] Kawaguchi K, Araki E, Kogure Y, et al. Development of DONET2-off Kii chanel observatory network[C]. Underwater Technology Symposium. IEEE, 2013, 20(3): 1-5
    [13] Yokobiki T, Choi J K, Nishida S, et al. Construction of DONET2[C]. Techno-Ocean. IEEE, 2017: 435-438
    [14] To A, Becker J, Weber B, et al. Development of a SeisComP3 module for detecting micro earthquakes and its application to ocean bottom network data[J]. Jamstec Rep. Res. dev., 2014, 18: 1-15
    [15] Nakamura T, Nakano M, Hayashimoto N, et al. Anomalously large seismic amplifications in the seafloor area off the Kii peninsula[J]. Mar. Geophys. Res., 2014, 35(3): 255-270.
    [16] Baba T, Takahashi N, Kaneda Y. A numerical study for relationship between coastal tsunami and bottom pressure fluctuation in the ocean generated from near-field earthquake[C]. Underwater Technology Symposium. IEEE, 2013, 20(3): 1-3
    [17] Nakano M, Nakamura T, Kamiya S I, et al. Seismic activity beneath the Nankai trough revealed by DONET ocean-bottom observations. Mar. Geophys. Res., 2014, 35(3): 271-284.
    [18] Ariyoshi K, Nakata R, Matsuzawa T, et al. The detectability of shallow slow earthquakes by the Dense Oceanfloor Network system for Earthquakes and Tsunamis (DONET) in Tonankai district, Japan. Mar. Geophys. Res., 2014, 35(3): 295-310.
    [19] Kimura T, Mikada H, Araki E, et al. S-wave anisotropy estimated by seismic interferometry using ambient noise record in the Nankai Trough subduction zone, Japan[C]. AGU Fall Meeting. AGU Fall Meeting Abstracts, 2013
    [20] Kimura T, Mikada H, Araki E. Seismic velocity monitoring using ambient noise observed by DONET seismometers in the Nankai Trough, Japan[C]. The 20th International Symposium on Recent Advances in Exploration Geophysics (RAEG 2016), 2016
    [21] Kimura T, Araki E, Mikada H, et al. Estimation of S-wave anisotropy in the Nankai Trough using active and passive seismic dataset observed by DONET[C]. The International Symposium on Recent Advances in Exploration Geophysics, 2015
    [22] Araki E, Kawaguchi K, Kaneda Y. Discriminating different type waves from pressure and ground motion observation in the seafloor by DONET cabled observation network[C]. American Geophysical Union, 2011
    [23] Nakamura T, Takenaka H, Okamoto T, et al. Seismic wavefields in the deep seafloor area from a submarine landslide source. Pure Appl. Geophys., 2014, 171(7): 1153-1167
    [24] To A, Obana K, Sugioka H, et al. Small size very low frequency earthquakes in the Nankai accretionary prism, following the 2011 Tohoku-oki earthquake. Phys. Earth Planet. In., 2015, 245: 40-51
    [25] Suzuki K, Nakano M, Takahashi N, et al. Synchronous changes in the seismicity rate and ocean-bottom hydrostatic pressures along the Nankai trough: A possible slow slip event detected by the Dense Oceanfloor Network system for Earthquakes and Tsunamis (DONET). Tectonophysics, 2016, 680: 90-98.
    [26] Nakano M, Nakamura T, Kamiya S, et al. Intensive seismic activity around the Nankai trough revealed by DONET ocean-floor seismic observations. Earth Planets Space, 2013, 65: 5-15. doi: 10.5047/eps. 2012.05.013.
    [27] Matsumoto H, Nosov M A, Kaneda Y, et al. Ocean-bottom pressure and seismic signals at tsunamigenic earthquake[C]. Underwater Technology. IEEE, 2015: 1-5
    [28] Takahashi N, Kamiya S, Nakano M, et al. Direct observation of a plate boundary earthquake by a seafloor network in the Nankai Trough seismogenic zone (DONET): An example of the M=6.5 earthquake on 1st April, 2016[C]. AGU Fall Meeting. AGU Fall Meeting Abstracts, 2016
    [29] 郑红霞, 张训华, 赵铁虎, 等. 海底监测技术之海底观测网络. 海洋地质前沿, 2015, 31(5): 51-56.
    [30] 央视新闻客户端. 我国将建国家海底科学观测网总投资超20亿元. 科技传播, 2017, 9(11).
  • 加载中
图(1)
计量
  • 文章访问数:  818
  • HTML全文浏览量:  202
  • PDF下载量:  25
出版历程
  • 收稿日期:  2017-10-17
  • 修回日期:  2017-10-30
  • 刊出日期:  2018-07-01

目录

    /

    返回文章
    返回
    本系统由北京仁和汇智信息技术有限公司设计开发 百度统计