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...
| Published in: | Earth and Planetary Science Letters |
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| Main Authors: | , , , |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
2004
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| Subjects: | |
| Online Access: | https://eprints.soton.ac.uk/24078/ |