Clathrate Hydrates of Air in Antarctic Ice

Measurements of the dissociation pressure of nitrogen hydrate and oxygen hydrate show that the clathrate hydrate of air with the formula (N 2 ,O 2 ) ⋅ 6H 2 O should exist below about 800 meters in the Antarctic ice sheet. This accounts for the disappearance of gas bubbles at depths greater than 1200...

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Bibliographic Details
Published in:Science
Main Author: Miller, Stanley L.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1969
Subjects:
Online Access:http://dx.doi.org/10.1126/science.165.3892.489
https://www.science.org/doi/pdf/10.1126/science.165.3892.489
Description
Summary:Measurements of the dissociation pressure of nitrogen hydrate and oxygen hydrate show that the clathrate hydrate of air with the formula (N 2 ,O 2 ) ⋅ 6H 2 O should exist below about 800 meters in the Antarctic ice sheet. This accounts for the disappearance of gas bubbles at depths greater than 1200 meters. The hydrate should exist from this depth to the bottom of the core and should comprise 0.06 percent of the ice.