JpGU-AGU Joint Meeting 2020

講演情報

[J] 口頭発表

セッション記号 S (固体地球科学) » S-GD 測地学

[S-GD02] 測地学

コンビーナ:松尾 功二(国土交通省国土地理院)、横田 裕輔(東京大学生産技術研究所)、岡 大輔(地方独立行政法人北海道立総合研究機構環境・地質研究本部地質研究所 )

[SGD02-12] レーザー歪計ネットワークによる地殻活動の広帯域観測

*新谷 昌人1高森 昭光1勝間田 明男2小林 昭夫2伊藤 武男3奥田 隆3大久保 慎人4 (1.東京大学地震研究所、2.気象庁気象研究所、3.名古屋大学大学院環境学研究科、4.高知大学教育研究部自然科学系)

キーワード:歪計、レーザー、地殻変動、神岡、犬山、船明

A laser strainmeter can measure deformation of the ground by sensing distance between two separated points based on the optical interferometer with reference to wavelength of light, enabling to detect small strain changes over wide frequency range [1]. Its advantages are high resolution with a long baseline, resonance-free response of optical reference, and low-drift detection using a stable wavelength of the laser, as compared to a conventional strainmeters using a mechanical reference.

To establish accurate and broadband observations of regional crustal activities, we constructed laser strainmeters at three underground sites in Japan, Kamioka (Gifu Pref.), Inuyama (Aichi Pref.), and Funagira (Shizuoka Pref.), and operate them as a strainmeter network. At Kamioka site, two laser strainmeters with baselines of 100m and 1500m are in operation [2, 3]. At Inuyama and Funagira sites, a 30-m strainmeter and a 400-m one are also in operation, respectively [4]. These strainmeters clearly detect earth tides, and their amplitudes are consistent with the calculations based on tidal force, the standard Earth's model, and the topographic effects around the sites. Coseismic strain steps were observed by the strainmeter network as common signals of the crustal activities and they were consistent with strain changes expected from the fault parameters.

At low frequencies, local disturbances of the site, such as changes in temperature, air pressure, and ground water level, have an effect on long-term strain changes and limit the detectability of the strainmeter network. In the presentation, we discuss the low-frequency performance of the laser strainmeters and the detectability of the strainmeter network for monitoring crustal activities.


References

[1] V. Vali, R. S. Krogstad, and R. W. Moss, Laser interferometer for earth strain measurements, Rev. Sci. Instrum., 36, 1352, 1965.

[2] A. Araya, A. Takamori, W. Morii, K. Miyo, M. Ohashi, K. Hayama, T. Uchiyama, S. Miyoki, and Y. Saito, Design and operation of a 1500-m laser strainmeter installed at an underground site in Kamioka, Japan, Earth, Planets and Space, 69:77, 2017.

[3] T. Akutsu, M. Ando, S. Araki, A. Araya, T. Arima et al., Construction of KAGRA: an underground gravitational-wave observatory, Prog. Theor. Exp. Phys., 013F01, 2018.

[4] A. Araya, T. Kunugi, Y. Fukao, I. Yamada, N. Suda, S. Maruyama, N. Mio, and S. Moriwaki, Iodine-stabilized Nd:YAG laser applied to a long-baseline interferometer for wideband earth strain observations, Rev. Sci. Instrum., 73, 6, 2434-2439, 2002.