地球の深層マントルの初期に留まった水量
Wenhua Lu1,2, Ya-Nan Yang1,2, Tao Long3
1State Key Laboratory of Deep Earth Processes and Resources, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences (CAS), Guangzhou, China.
まとめ
初期の地球
科学分野:
- 地化学
- 鉱物物理学
- 惑星科学
背景:
- 地球の水吸収は 衝突によって 初期の溶けた段階で起こりました
- 結晶化マントルの水保持と分布のメカニズムは不明である.
研究 の 目的:
- ブリッジマニットと高圧溶液の間の水分分割を調査する.
- 主要なマントルの鉱物への水の組み込みに温度がどのように影響するかを決定します.
主な方法:
- 体系的な高圧実験
- 水分分割係数の分析
主要な成果:
- 水分をブリッジマニットに分けるのは 温度によって大きく増加します
- 結晶化後の下層マントルの水分保持を 示唆している.
結論:
- 下層マントルの早期に蓄積された水は,マントルのコンベクションに影響を与えます.
- 地球の居住可能惑星への移行に 潜在的に役割を果たした
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