日本地球惑星科学連合2016年大会

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ポスター発表

セッション記号 S (固体地球科学) » S-VC 火山学

[S-VC47] 活動的火山

2016年5月24日(火) 17:15 〜 18:30 ポスター会場 (国際展示場 6ホール)

コンビーナ:*青木 陽介(東京大学地震研究所)、前田 裕太(名古屋大学)

17:15 〜 18:30

[SVC47-P36] 桜島火山におけるACROSSで取得した伝達関数の時間変化(2015年1月〜8月)

*山岡 耕春1宮町 宏樹2八木原 寛2前田 裕太1渡辺 俊樹1國友 孝洋1生田 領野3為栗 健4清水 洋5渡邊 将史1井口 正人4 (1.名古屋大学環境学研究科附属地震火山研究センター、2.鹿児島大学大学院理工学研究科、3.静岡大学理学部、4.京都大学防災研究所、5.九州大学大学院理学研究院)

キーワード:構造、時間変化、マグマ

Quantitative monitoring of magma transport process is essentially important for understanding the volcanic process and prediction of volcanic eruptions. To realize this monitoring, an active monitoring system using a vibration source called ACROSS has been operated in Sakurajima Volcano since September 2012 (Yamaoka et al., 2014; Miyamachi et al., 2013; 2014).
From our previous observational studies, we obviously found that the amplitude and travel times of the daily transfer functions (the ACROSS signal) vary temporally. In particular Maeda et al. (2015) revealed that the amplitude of the ACROSS signals in the later phases became small in several hours before and after explosive eruptions. In this report, we show a long-term temporal change for the ACROSS signals observed with the remarkable volcanic activity that occurred in Sakurajima volcano on August 15, 2015.
DATA
Our ACROSS system is composed of two vibrators: one vibrator (SKR1) with a signal frequency range of 7.510Hz +/- 2.50Hz and the other (SKR2) with the range of 12.505Hz +/- 2.50Hz. The seismic signals from the ACROSS sources are routinely monitored with more than 20 permanent and 5 temporal seismic stations in and around Sakurajima volcano. The signals recorded at the seismic stations are deconvoluted with the ACROSS source function to obtain the transfer function between the source and the receivers.
The ACROSS system was continuously operated until 18 August, 2015 after five month failure of inverter system. We successfully replace the broken inverter with a normal one by managing transferring inverters from one source to another. The fixed ACROSS system started operation at the beginning of January 2015, but the operation was suspended on 18 August, 2015 because of the signal contamination to a monitoring seismic station for the volcano. We use the data in 2015 to check the temporal change of transfer functions between the ACROSS source and the seismic stations in Sakurajima island.
RESULTS
We calculated the daily transfer functions for each station by every 1 day stacked data during a period of January to August 2015. Transfer functions in Sakurajima volcano indicate large temporal variation especially in later phase part comparing to the other site such as Awaji or Tokai area where ACROSS system is being operated. In many of the transfer function connecting between the ACROSS source and the stations remarkable change can be seen at the end of July, 2015, though causal relationship to the volcanic event on 15 August is not clear. We also need to make a quantitative investigation on the meteorological effect to the transfer functions.
Reference
Yamaoka et al. (2014) Earth Planets, Space, Doi:10.1186/1880-5981-66-32
Maeda et al. (2015) Geophys. Res. Lett., Doi: 10.1002/2015GL064351