Abstract
The large variety and complexity of the exotic phases of ice is in clear contrast to the simplicity of the water molecule. The properties of these phases are crucially dependent on the nature of the hydrogen bond. Our observation of the existence of two H-bonds in ices [1] indicates that the true reason for the formation of the large number of ice structures is the existence of a mixture of the strong and weak H-bonds, resulting in a large internal stress in the system. Hence relaxation of the stress, reducing the stress energy, could result in different distorted ice structures, in metastable states. In a similar way, the two types of H-bond can stabilise the two phases which are often proposed in the various mixture models of water. The details of our model are discussed.
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© 1994 Springer Science+Business Media Dordrecht
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Li, J., Ross, D.K. (1994). The Role of H-Bond in the Formation of Ices. In: Bellissent-Funel, MC., Dore, J.C. (eds) Hydrogen Bond Networks. NATO ASI Series, vol 435. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-8332-9_5
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DOI: https://doi.org/10.1007/978-94-015-8332-9_5
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