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Updated: Jul 12, 2026

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Atom Probe Tomography Analysis of Exsolved Mineral Phases
Published on: October 25, 2019
アポロ16号のサンプルの揮発性元素:月面からのガス排出の可能性の証拠
まとめ
月の高地における火山の過程は,水のような揮発性物質を放出します. アポロ16号のサンプルは,ブロミン,カドミウム,亜鉛などの元素の濃縮を明らかにし,限られた元の月面水を示しています.
科学分野:
- 月面地質学 月面地質学
- 地質化学 地質化学
- 惑星科学は惑星科学である.
背景:
- アポロ16号は,ブレキアや高原の土壌など,月面から様々なサンプルを回収した.
- 以前の研究では,月面のサンプルにおける揮発性元素の濃度の変動が示された.
研究 の 目的:
- アポロ16号のブレキアと高地の土壌における揮発性元素の濃縮を調査する.
- これらの濃縮物が月の火山活動や水分量に及ぼす影響を理解する.
主な方法:
- アポロ16号のブレッチアと土壌サンプルを分析した.
- 揮発性元素の濃度 (ブロミン,カドミウム,ゲルマーニウム,アンチモニー,タリウム,亜鉛) の地化学調査.
- 月面の元素の比率と宇宙の豊かさの比較.
主要な成果:
- アポロ16号のいくつかのブレキアには,揮発性元素の濃度が著しく高まっている.
- 似たような,しかしあまり顕著ではない,濃縮は,すべての高地の土壌で観察されています.
- タリウムとウランの比率は,月面での限られた原始水分含有量を示唆しています.
結論:
- 月の高地では火山活動が起こり,水を含む揮発性物質が放出されている可能性が高い.
- データは,月の初期水分量は,深さ約22メートルの層に相当することを示唆しています.
- アポロ16号の場所にあるカタクラスティック・アノルソサイトは,ネクタリス盆地からのエジェクトかもしれない.
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