Clathrate Hydrates of Air in Antarctic Ice
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- Stanley L. Miller
- Department of Chemistry, University of California, San Diego, La Jolla 92037
Abstract
<jats:p> Measurements of the dissociation pressure of nitrogen hydrate and oxygen hydrate show that the clathrate hydrate of air with the formula (N <jats:sub>2</jats:sub> ,O <jats:sub>2</jats:sub> ) ⋅ 6H <jats:sub>2</jats:sub> 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. </jats:p>
Journal
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- Science
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Science 165 (3892), 489-490, 1969-08
American Association for the Advancement of Science (AAAS)
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Keywords
Details 詳細情報について
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- CRID
- 1360011143654987648
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- NII Article ID
- 30020495868
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- ISSN
- 10959203
- 00368075
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- Data Source
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- Crossref
- CiNii Articles