A survey and new measurements of ice vapor pressure at temperatures between 170 and 250K

Journal Article · Fri Mar 05 00:00:00 EST 1993 · Geophysical Research Letters (American Geophysical Union); (United States)

DOI:https://doi.org/10.1029/93GL00105· OSTI ID:6438014

Marti, J; Mauersberger, K ^[1]

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1. Univ. of Minnesota, Minneapolis (United States)

Saturated vapor pressures of ice at temperatures below 200K have become more important since the discovery of ice clouds in the polar stratosphere and upper mesosphere. Direct measurements of ice vapor pressures at such low temperatures are sparse and unreliable. This paper summarizes published vapor pressure data and presents new measurements at temperatures between 170 and 250K extending the range of measured ice vapor pressures by three orders of magnitude. A simple empirical vapor pressure equation is derived which permits prediction of vapor pressures between 170K and the triple point of water, with an accuracy of about 2%: log P = A/T + B, with A = [minus]2663.5 [+-] 0.8, B = 12.537 [+-] 0.011, P in Pa and T in kelvins. Predictions by this empirical equation agree, within experimental uncertainty, with the most reliable equation derived from thermodynamic principles. 22 refs., 2 figs., 1 tab.

• OSTI ID: 6438014
• Journal Information: Geophysical Research Letters (American Geophysical Union); (United States), Vol. 20:5; ISSN 0094-8276
• Country of Publication: United States
• Language: English

Related Subjects

54 ENVIRONMENTAL SCIENCES
37 INORGANIC
ORGANIC
PHYSICAL AND ANALYTICAL CHEMISTRY
ICE
VAPOR PRESSURE
CLOUDS
MESOSPHERE
STRATOSPHERE
TEMPERATURE RANGE 0065-0273 K
WATER
EARTH ATMOSPHERE
HYDROGEN COMPOUNDS
OXYGEN COMPOUNDS
PHYSICAL PROPERTIES
TEMPERATURE RANGE
THERMODYNAMIC PROPERTIES
540110*
400201 - Chemical & Physicochemical Properties