日本地球惑星科学連合2023年大会

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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-TT40] 空中からの地球計測とモニタリング

2023年5月24日(水) 13:45 〜 15:00 202 (幕張メッセ国際会議場)

コンビーナ:小山 崇夫(東京大学地震研究所)、楠本 成寿(京都大学大学院理学研究科附属地球熱学研究施設)、光畑 裕司(独立行政法人 産業技術総合研究所)、大熊 茂雄(産業技術総合研究所地質情報研究部門)、座長:小山 崇夫(東京大学地震研究所)、楠本 成寿(京都大学大学院理学研究科附属地球熱学研究施設)、光畑 裕司(独立行政法人 産業技術総合研究所)、大熊 茂雄(産業技術総合研究所地質情報研究部門)

14:00 〜 14:15

[STT40-02] 人工衛星経由の遠隔飛行制御による霧島新燃岳全方位無人ヘリ空中磁気測量

*小山 崇夫1、金子 隆之1大湊 隆雄1渡邉 篤志1行竹 洋平1本多 嘉明2 (1.東京大学地震研究所、2.千葉大学環境リモートセンシング研究センター)

キーワード:空中磁気測量、新燃岳、無人ヘリコプター

We repeatedly conducted aeromagnetic surveys at Shinmoe-dake volcano, Japan by using an uncrewed helicopter, and elucidate magnetization structure and its temporal change. At the beginning of 2011, Shinmoe-dake volcano had magmatic eruptions. After ceasing activities of volcanic eruptions, we conducted repeated surveys, and notable temporal changes are detected just around the crater of Shinmoe-dake volcano by gaining magnetization due to cooling of lava which has accumulated in the crater at the 2011 eruptions. The cooling rate just follows the square root of elapsed time from the eruption, and thus the cooling is being simply done by thermal diffusion.
Our previous surveys, however, have been done only on the western side of Shinmoe-dake volcano, because we cannot access to the eastern side of the volcano nor telecommunicate with the helicopter from the home point at a common western side if it flies in the opposite side. Recently, the remotely control system of the helicopter via a satellite was developed and it overcame the difficulties. By using this system, we conducted a comprehensive aeromagnetic survey on both the eastern and western side in 2021, as the helicopter was controlled from Hamamatsu, Shizuoka: 700 km away from the volcano.
In this paper, we show the control system and the result of the aeromagnetic survey in Shinmoedake volcano.