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