グランドバンクの南にある異常な地下水は,流動的な活動が混乱していることを示唆しています
まとめ
高濃度の粒子を運ぶ気流は,ソーム・アビサール平原で発見された異常な地下水の源として特定されました. これは,大陸の上昇から下り坂の動きを示唆しています.
科学分野:
- 海洋学 海洋学 海洋学
- 海洋地質学 海洋地質学
背景:
- 深海の環境は,通常,低粒子の濃度で特徴付けられています.
- アビッサルの平原と大陸の上昇は,深い海の独特の地形学的な特徴です.
研究 の 目的:
- ソーム・アビサール平原の縁で観測された高度に曇った地下水の起源を特定するために.
- このぼんやりした水を輸送するメカニズムを特定するために.
主な方法:
- 温度,塩分,酸素含有量を含む地下水の性質を分析する.
- 水柱の粒子濃度の測定.
主要な成果:
- ぼんやりした底水は,大陸の上昇まで斜面上を辿られた.
- 微粒子の濃度は,典型的な深海レベルよりも (大きさの1〜2度) 顕著に高かった.
結論:
- 観測された地下水の特性と高い粒子の負荷は,大陸の上昇による起源を示しています.
- トルビディティ・ストリームは,この物質の下り坂輸送の可能なメカニズムとして提案されています.
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