In our studies of Tg of amorphous forms of water, it had been ascertained that the observed endotherm had the characteristics of glass softening and not those of a sub-Tg peak, but an explicit discussion was not provided. To prevent this Tg-endotherm from being mistaken as part of a sub-Tg peak, we use our earlier data to explain why the endotherm corresponds to water’s Tg of 136 K, and not to a sub-Tg peak.
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G. P. Johari (2003) studied this question.
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