2006年のマウント・セント・アウグスティヌス火山の噴火中の電気活動
R J Thomas1, P R Krehbiel, W Rison
1Langmuir Laboratory, New Mexico Tech, Socorro, NM 87801, USA. thomas@nmt.edu
まとめ
火山の噴火は,2つの異なる電気的相を通して雷を発生させることができます: 充電された物質の爆発的な放出と,その後の噴火中の放電. これらの発見は,火山の電気現象に光を当てています.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 大気科学 大気科学
- 火山学 火山学とは
背景:
- 火山噴火は複雑な現象で,電気的な側面はよくわかっていない.
- 火山の噴火の中で雷の発生が観察されているが,完全に特徴づけられていない.
研究 の 目的:
- 火山噴火に関連した電気活動を調査するために.
- 噴火中の雷のモードと特徴を区別するために.
主な方法:
- 利用した無線周波数到着時間 (RF TOA) 測定.
- 電気放電を分析するためにインターフェローメーターの測定を用いた.
- セント・アウグスティヌス山の噴火中に観測された電気的活動.
主要な成果:
- 噴火中の2つの異なる電気活動の相を特定した.
- 第1段階:正電荷の火山噴出物の爆発的噴出,無秩序な放電と単純な雷.
- 第2段階:火山の羽根の中の従来の稲妻,発射が遅れて,下風で拡散し,インサイト充電が示唆される.
結論:
- 火山の噴火は,少なくとも2つの異なるモードで複雑な電気的行動を示します.
- 電気活動は雷雨の電化プロセスと類似点を共有しています.
- 火山の噴出物における in situ 充電メカニズムを完全に理解するためには,さらなる研究が必要である.
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