グリーンランドの南部の氷芯から得られた硫酸塩と窒素酸塩の濃度
まとめ
グリーンランドの氷芯は,20世紀初頭以来,硫酸塩と窒素酸塩の汚染が著しく増加したことを明らかにしています. これらの大気堆積の変化は,北米とユーラシアからの産業排出量に関連しています.
科学分野:
- 環境科学 環境科学
- 氷河学 氷河学とは
- 大気化学 大気化学
背景:
- 氷の芯は,大気組成の歴史的な記録を提供します.
- 過去の汚染レベルは,氷層内の化学物質を分析することによって再構築できます.
研究 の 目的:
- 1869年から1984年にかけてのグリーンランド南部の氷芯の化学濃度を分析するために.
- 硫酸塩と窒酸塩の堆積の傾向を時間とともに特定する.
- 観察された化学変化の潜在的な原因を調査する.
主な方法:
- 氷核における酸素同位体,塩化物,窒素酸,硫酸塩濃度の分析.
- 氷のコア層の年代測定は,1869年から1984年までのタイムラインを確立するためのものです.
主要な成果:
- 海塩以外の硫酸塩の濃度は,1900年から1910年までの約3倍になりました.
- 窒素濃度は約1955年以来2倍になった.
- 観測された増加は,産業成長期と相関しています.
結論:
- グリーンランドでは,大気中の硫酸塩と窒素酸塩の堆積が著しく増加しています.
- 北米とユーラシアからの人類による排出は,これらの傾向に寄与している可能性が高い.
- 氷芯のデータは,長期的な環境汚染パターンに関する貴重な洞察を提供します.
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