The mechanisms for pressure-induced amorphization of ice I(h).
Author(s) : TSE J. S., KLUG D. D., TULK C. A., et al.
Type of article: Article
Summary
The high-density amorphous (HDA) phase of ice I(h) forms at a pressure close to the extrapolated melting curve of ice, leading to the suggestion that it may have structure similar to that of dense water. On annealing, HDA ice transforms into a low-density amorphous (LDA) phase with a distinct phase boundary. The authors use quasi-harmonic lattice-dynamics calculations to show that the amorphization mechanism in ice I(h) changes from thermodynamic melting for T> 162 K to mechanical melting at lower temperatures. The vibrational spectra of ice I(h), LDA ice and quenched water also indicate a structure for LDA ice that differs from that of the liquid.
Details
- Original title: The mechanisms for pressure-induced amorphization of ice I(h).
- Record ID : 2000-2384
- Languages: English
- Source: Nature - vol. 400 - n. 6745
- Publication date: 1999/08/12
- Document available for consultation in the library of the IIR headquarters only.
Links
See the source
Indexing
- Themes: Thermodynamics and changes of state
- Keywords: Ice; Temperature; Physical property; Pressure; Change of phase
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