地球のマントルからのヘリウム流は,ハワイのフーマロリック脱ガスから推定されています
まとめ
研究者は,ハワイのキラウエアでヘリウムと二酸化炭素の比率を測定しました. このデータは,1×10^5原子/cm^2/秒のヘリウム流動を示唆し,潜在的に上層マントルから発生している.
科学分野:
- 地質化学 地質化学
- 火山学 火山学とは
- 地球科学 地球科学 地球科学
背景:
- 火山ガスは,地表の過程についての洞察を提供します.
- ガス組成を理解することは,火山活動と地球のマントルの動態を監視するために不可欠です.
研究 の 目的:
- ハワイのキラウエアにある硫黄バンクの煙突からのヘリウム流量を定量化するために.
- ヘリウム排出の起源とマントルプロセスとの関連を調査する.
主な方法:
- 硫黄銀行煙突からの火山ガス (ヘリウムと二酸化炭素) の体系的な収集と分析.
- 地球の地殻における炭素含有量の推定.
主要な成果:
- ヘリウムと二酸化炭素の平均比率を決定した.
- 平方センチメートル/秒あたり1×10^5原子のヘリウム流が計算されました.
- この流動は,以前に推定された値の低い範囲に該当します.
結論:
- 測定されたヘリウム流は,上層マントルの深層にある源からの貢献を示している可能性があります.
- 硫黄バンクの煙突ガス組成は,マントルの脱ガス化の指標として役立つ.
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