サブダクションゾーンの液体のpHから金属と揮発性サイクルへの影響
Matthieu E Galvez1, James A D Connolly1, Craig E Manning2
1Earth Sciences Department, Swiss Federal Institute of Technology, CH-8092 Zurich, Switzerland.
Nature
|November 18, 2016
まとめ
サブドクションゾーンの液体は,岩の組成と揮発性含有量によってpHが制御される軽度のアルカリ性である. これは地質学的な時間尺度で金属と揮発性元素の地球的な循環に影響します
科学分野:
- 地球科学
- 地化学
- 地力学
背景:
- 地球の金属と揮発性元素のサイクルを制御しています
- 流体媒介による化学交換のための重要な設定です.
- サブダクションゾーンの液体種化とpHの特徴づけは,重要な科学的課題である.
研究 の 目的:
- 流体岩平衡を予測する
- 熱構造,鉱物学,および流体種のモデルをリンクする.
- 液体のpHの制御と元素の循環への影響を理解する.
主な方法:
- 流体岩平衡の熱力学的な予測
- サブダクションゾーンの熱構造と鉱物学のモデリング.
- 岩の組成が異なる状態での流体種の分析
主要な成果:
- 地殻の石質学における潜水帯液体は,軽度のアルカリ性pHを示している.
- 液体のpHは岩の揮発性および塩素含有量によって調節されます.
- 寒い潜水は酸化炭素を保存する.マントルの液のpHは岩の組成に敏感である.
結論:
- 液体のpHの変動は岩の組成,地殻内分化,地殻液体の浸透と関連しています.
- 岩の組成の微妙な変化は,マントルの液のpHに影響を及ぼします.
- 大気と海洋の化学反応と 潜水地帯の流体種の形成の間には フィードバックが存在します
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