The mechanisms for pressure-induced amorphization of ice Ih


There has been considerable interest in the structure of liquid water at low temperatures and high pressure following the discovery of the high-density amorphous (HDA) phase of ice Ih (ref. 1). HDA ice 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 boundary2,3. Extrapolation of thermodynamic data along the HDA–LDA coexistence line into the liquid region has led to the hypothesis that there might exist a second critical point for water and the speculation that liquid water is mixture of two distinct structures with different densities4,5. Here we critically examine this hypothesis. We use quasi-harmonic lattice-dynamics calculations to show that the amorphization mechanism in ice Ih changes from thermodynamic melting for T > 162 K to mechanical melting at lower temperatures. The vibrational spectra of ice Ih, LDA ice and quenched water also indicate a structure for LDA ice that differs from that of the liquid. These results call into question the validity of there being a thermodynamic connection between the amorphous and liquid phases of water.

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Figure 1: Phase behaviour (experimental and theoretical) of ice Ih.
Figure 2: The experimental inelastic incoherent neutron scattering (IINS) function for LDA ice, hyperquenched (hg) water, and ice Ih.


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Inelastic scattering data were acquired at Argonne National Laboratory: these measurements were supported by the US DOE-BES.

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Correspondence to J. S. Tse.

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Tse, J., Klug, D., Tulk, C. et al. The mechanisms for pressure-induced amorphization of ice Ih. Nature 400, 647–649 (1999).

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