日本地球惑星科学連合2019年大会

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[E] 口頭発表

セッション記号 S (固体地球科学) » S-TT 計測技術・研究手法

[S-TT42] Recent Advances in Exploration Geophysics 2019

2019年5月26日(日) 10:45 〜 12:15 A04 (東京ベイ幕張ホール)

コンビーナ:三ケ田 均(京都大学大学院工学研究科)、飯尾 能久(京都大学防災研究所)、島 伸和(神戸大学大学院理学研究科惑星学専攻)、武川 順一(京都大学大学院工学研究科)、座長:武川 順一(京都大学大学院工学研究科)、渡邊 勇介(京都大学大学院工学研究科)

10:45 〜 11:00

[STT42-07] The observation of active source and ambient noise signals with telecommunication fiber-optic cable in urban area

*Baoshan Wang1Xiangfang Zeng2Xiaobin Li3Weiwei Xu4Shanhui Xu4Zhenghong Song1 (1.School of Earth and Space Sciences, University of Science and Technology of China、2.State Key Laboratory of Geodesy and Earth’s Dynamics, Institute of Geodesy and Geophysics, Chinese Academy of Sciences、3.Earthquake Agency of Yunnan Province、4.Institute of Geophysics, China Earthquake Administration)

キーワード:Urban Area, Telecommunication Fiber-optic Cable, Seismic Monitoring

The Distributed Acoustic Sensing (DAS) is a rapidly developing technique, which can provide dense (~ meters) seismic observations. Recently, several experiments were performed using specifically deployed fiber-optic cables, while the seismic observation with telecommunication fiber-optic cable in urban area is still challenging. A 5.2 km long telecommunication fiber-optic cable buried at about 30-cm depth in urban area is used to record active source shots and more than 10-hours continuous ambient noise. We are able to extract seismic signals with the telecommunication fiber-optic cable 9 km from the active source (~Ml0.7). The high-frequency (~ 10 Hz) Rayleigh wave signal emerges from the noise cross-correlation functions. The dispersion information of Rayleigh wave is inverted for Vs at the top 30 m and construct a 2D profile, which helps to assess ground shaking in this area.