エンケラドスの内部で進行中の熱水活動
Hsiang-Wen Hsu1, Frank Postberg2, Yasuhito Sekine3
1Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, Colorado 80303, USA.
Nature
|March 13, 2015
まとめ
エンケラドスの分析
科学分野:
- 惑星科学は惑星科学である.
- 天体生物学 アストロバイオロジー
- 地質化学 地質化学
背景:
- 土星の衛星であるエンケラドスは,氷の粒を含んだ羽根を現しています.
- 地下海洋が検出され,水熱活動の可能性を示唆しています.
- 以前の,ナトリウム塩が豊富な粒子の検出は,岩と水の相互作用を示しています.
研究 の 目的:
- エンケラドスの羽根から,シリコン豊富なナノダスト粒子 (ストリーム粒子) を分析する.
- これらのユニークな粒子の起源と影響を調査します.
- エンケラドスの地下海洋の条件を決定する.
主な方法:
- ナノメートルのサイズのSiO2 (シリカ) 粒子の分析.
- 粒子の組成と大きさの分布の解釈.
- 羽根の組成の宇宙船の測定値との相関.
主要な成果:
- ストリーム粒子はナノメートルのサイズのシリカ (SiO2) として識別されました.
- 粒子の大きさの範囲を決定する (2-8 nm 半径).
- 指示された高温 (>90°C) 水熱反応.
結論:
- エンケラドスの海底では,熱水活動が続いている.
- 世界的な地熱活動により,熱水産物が噴出します.
- これらの発見は,エンケラドスの地下海洋の潜在的居住可能性を支持する.
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