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Science 2 June 1972:
Vol. 176. no. 4038, pp. 1011 - 1012
DOI: 10.1126/science.176.4038.1011

Articles

Partial Pressure of Gases Dissolved at Great Depth

Wallace O. Fenn 1

1 Department of Physiology, University of Rochester School of Medicine and Dentistry, Rochester, New York 14620

Thermodynamic considerations have been applied to data showing that the solubilities of oxygen, carbon dioxide, and helium in water decrease with increasing pressure and depth. When water is saturated with a given gas at 1 atmosphere absolute, the equilibrium partial pressure of the gas at any depth is equal to the partial pressure of that gas if it were contained in a gas column extending from the surface to that particular depth.


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Hemoglobin function in deep-sea and hydrothermal-vent endemic fish: Symenchelis parasitica (Anguillidae) and Thermarces cerberus (Zoarcidae).
R. E. Weber, S. Hourdez, F. Knowles, and F. Lallier (2003)
J. Exp. Biol. 206, 2693-2702
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The Thermodynamics of Gases Dissolved at Great Depths.
C. A. Eckert (1973)
Science 180, 426-427
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Gravitational Effects on Concentrations and Partial Pressures in Solutions: A Thermodynamic Analysis.
F. C. Andrews (1972)
Science 178, 1199-1201
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