The first study of free vaporization kinetics of ice at temperatures near its melting point is reported. The experimental approach employed is based on a unique combination of thermal desorption spectroscopy, microcalorimetry, and time-of-flight mass spectrometry, making it possible to overcome challenges associated with the introduction of volatile solids into a high vacuum environment. Measurements of the vaporization rate of polycrystalline ice demonstrate that the vaporization kinetics deviate dramatically from those predicted by a simple mobile precursor mechanism. The vaporization rate follows Arrhenius behavior from -40 to 0°C with an effective activation energy of 50±4 kJ/mol, which is significantly higher than the value predicted by the simple mobile precursor mechanism. Extrapolation of earlier measurements conducted below -40°C yields a value of approximately 0.02 at 0°C for the vaporization coefficient α v. In contrast, experimentally determined vaporization coefficient is found to be 0.7±0.3 and shows a weak dependence on temperature up to the bulk melting point. The role of possible surface phase transitions in the mechanisms of release and uptake of H 2O and other chemical species by ice surfaces is discussed. © 2004 American Institute of Physics.
CITATION STYLE
Sadtchenko, V., Brindza, M., Chonde, M., Palmore, B., & Eom, R. (2004). The vaporization rate of ice at temperatures near its melting point. Journal of Chemical Physics, 121(23), 11980–11992. https://doi.org/10.1063/1.1817820
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