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Decompression-induced melting of ice IV and the liquid–liquid transition in water

Abstract

Although liquid water has been the focus of intensive research for over 100 years, a coherent physical picture that unifies all of the known anomalies of this liquid1,2,3, is still lacking. Some of these anomalies occur in the supercooled region, and have been rationalized on the grounds of a possible retracing of the liquid–gas spinodal (metastability limit) line into the supercooled liquid region4,5,6,7, or alternatively the presence of a line of first-order liquid–liquid phase transitions in this region which ends in a critical point8,9,10,11,12,13,14,. But these ideas remain untested experimentally, in part because supercooled water can be probed only above the homogeneous nucleation temperature TH at which water spontaneously crystallizes. Here we report an experimental approach that is not restricted by the barrier imposed by TH, involving measurement of the decompression-induced melting curves of several high-pressure phases of ice in small emulsified droplets. We find that the melting curve for ice IV seems to undergo a discontinuity at precisely the location proposed for the line of liquid–liquid phase transitions8. This is consistent with, but does not prove, the coexistence of two different phases of (supercooled) liquid water. From the experimental data we calculate a possible Gibbs potential surface and a corresponding equation of state for water, from the forms of which we estimate the coordinates of the liquid–liquid critical point to be at pressure Pc ≈ 0.1 GPa and temperature Tc ≈ 220 K.

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Figure 1: Overall logic of the present experiment.
Figure 2: Data obtained in the present experiment.
Figure 3: Gibbs potential surface for liquid water probed in the present experiments for both its stable and metastable regions.
Figure 4: Application of data obtained in the present experiment to reconstruct the Gibbs potential surface and the thermodynamic equation of state V = V(P, T).

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Acknowledgements

We thank C. A. Angell, K. Aoki, M.-C. Bellissent-Funel, M. Canpolat, H.-D. Lüdemann, P. H. Poole, R. Sadr-Lahijany, S. Sastry, F. Sciortino, F. W. Starr and Y. Suzuki for discussions and reading of manuscript drafts. We also thank C. A. Angell for pointing out subtle ponts that we initially glossed over. This work was supported by CREST (Core Research for Evolutional Science and Technology) of Japan Science and Technology Corporation (JST), BP and the US NSF.

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Mishima, O., Stanley, H. Decompression-induced melting of ice IV and the liquid–liquid transition in water. Nature 392, 164–168 (1998). https://doi.org/10.1038/32386

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