Real-time kinetic measurements of the condensation and evaporation of D2O molecules on ice at 140K<T<220K

被引:42
作者
Chaix, L [1 ]
van den Bergh, H [1 ]
Rossi, MJ [1 ]
机构
[1] Ecole Polytech Fed Lausanne, Lab Pollut Atmospher & Sol, Inst Environm Engn, DRG IGE, CH-1015 Lausanne, Switzerland
关键词
D O I
10.1021/jp983050n
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The kinetics of condensation of (D2O)-O-18 water vapor on (D2O)-O-16 ice was studied in the temperature range 140-220 K. The measurements have been performed in real time using the pulsed valve technique in a low-pressure flow reactor. Ice samples were prepared by several different methods. The uptake coefficient gamma was observed to decrease with increasing surface temperature, and varied from gamma = 0.06 to 0.8. A significant dependence of gamma on the method of preparation of the ice has been found. At 180 K, gamma = 0.13 for single-crystal ice, 0.18 for ice condensed from the vapor phase, and approximately 0.25 for bulk ice obtained from freezing liquid (D2O)-O-16. The uptake coefficient attained a value of gamma = 0.8 at 140 K for cubic ice prepared by vapor condensation at 140 K. The activation energy for evaporation of D2O at low temperatures (140-190 K) has been measured as 12.2 kcal/mol, whereas it decreases to 8.3 kcal/mol at higher temperatures (190-220 K). The rate of evaporation at 200 K corresponds to the loss of approximately 70 +/- 10 formal monolayers per second. The experimental results suggest the formation of loosely bound water adsorbed to the surface of ice whose bond energy is estimated to be 4.0 +/- 0.4 kcal/mol, independent of the type of ice.
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页码:10300 / 10309
页数:10
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