メッセンジャー (MESSENGER) は,水星近くの惑星イオンの空間的分布に関する観測を行った
Thomas H Zurbuchen1, Jim M Raines, James A Slavin
1Department of Atmospheric, Oceanic and Space Sciences, University of Michigan, Ann Arbor, MI 48109-2143, USA. thomasz@umich.edu
まとめ
水星の極域は,イオン化されたエクソスフィアの主要な源泉であり,ナトリウムや酸素などの重イオンがそこから発生します. しかし,ヘリウムはより均一な分布を示し,異なる表面ベースの源を示唆しています.
科学分野:
- 惑星科学 惑星科学
- 宇宙物理学 宇宙物理学
- エクソスフィアのダイナミクス エクソスフィアのダイナミクス
背景:
- 水星は,様々なイオンで構成された薄いエクソスフィアを持っています.
- これらのイオンの発生源と分布を理解することは,水星の太陽風との相互作用を理解するために不可欠です.
研究 の 目的:
- 水星のエクソスフィアの重イオンの空間的分布と源を分析する.
- エクソスフィアの構成における極域と表面相互作用の役割を調査する.
主な方法:
- MESSENGER宇宙船からの地球規模測定を用いた.
- ナトリウム (Na+),酸素 (O+),ヘリウム (He+) を含む特定の重イオンの流れを分析した.
主要な成果:
- 水星の北の磁気コスプ領域で,ナトリウムと酸素イオンフローの明確な最大値が観測されました.
- 惑星全体でより均一なヘリウムイオンフローが発見されました.
- ナトリウムイオンの圧力は,夜辺赤道地域のような特定の地域では,陽子の圧力の有意な部分である可能性があることを決定しました.
結論:
- 水星の極域は,おそらく太陽風の噴射による,水星のイオン化されたエクソスフィアの重要な源として特定されています.
- ヘリウムで飽和した表面蒸発モデルは,ヘリウムイオンの均一な分布をよりよく説明します.
- この発見は,水星のエクソスフィアの形成における太陽風と表面過程の複雑な相互作用を強調しています.
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