Mechanisms controlling the distribution of helium and neon in the Arctic seas: the case of the Knipovich Ridge

Helium concentration and isotopic ratio in the ocean are influenced by four sources: the mantle, atmosphere, crust and tritium decay. In addition, the concentration of dissolved gases can be altered by air injection and ice-related mechanisms such as brine rejection, sea-ice melting and glacial melt...

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Veröffentlicht in:	Earth and planetary science letters 2004-12, Vol.229 (1), p.125-139
Hauptverfasser:	Hahm, Doshik, Postlethwaite, Clare F., Tamaki, Kensaku, Kim, Kyung-Ryul
Format:	Artikel
Sprache:	eng
Schlagworte:	Arctic Glacier Helium Marine Neon Sea-ice The Knipovich Ridge
Online-Zugang:	Volltext
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