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Using infrared spectroscopy, transitions among ice, solution, and clathrate phases are compared with the predictions of the SO 2 −H 2 O phase diagram in the temperature range −20 to 10 °C and SO 2 pressures from 50 to 900 mbar. The infrared signatures of clathrate and ice, as well as SO 2 in a variety of phases are recorded and interpreted in terms of their environments. The consequences of SO 2 in confined geometries within ice are explored.
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Zhang et al. (2004) studied this question.
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