Abstract
It is widely accepted that ice, no matter what phase, is unable to incorporate large amounts of salt into its structure. This conclusion is based on the observation that on freezing of salt water, ice expels the salt almost entirely as brine. Here, we show that this behaviour is not an intrinsic physico-chemical property of ice phases. We demonstrate by neutron diffraction that substantial amounts of dissolved LiCl can be built homogeneously into the ice VII structure if it is produced by recrystallization of its glassy (amorphous) state under pressure. Such ‘alloyed’ ice VII has significantly different structural properties compared with pure ice VII, such as an 8% larger unit cell volume, 5 times larger displacement factors, an absence of a transition to an ordered ice VIII structure and plasticity. Our study suggests that there could be a whole new class of ‘salty’ high-pressure ice forms.
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Acknowledgements
The authors are very grateful to W.F. Kuhs for pointing out the issue of plasticity in ice VII. We thank J.-L. Laborier (ILL), G. Hamel and J. Philippe for technical assistance and advice, as well as R. Pick, F. Frey and M. Schmidbauer for helpful discussions. A.M.S. acknowledges support from the French National Supercomputing Facility IDRIS, where all of the calculations have been carried out under the projects CP9-71387 and CP9-81387. This work is partially based on experiments carried out at the Swiss spallation source SINQ, Paul Scherrer Institute, Villigen, Switzerland.
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S.K., L.E.B, T.S. and T.C.H. carried out the experiments and A.M.S. the calculations. S.K. wrote the paper.
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Klotz, S., Bove, L., Strässle, T. et al. The preparation and structure of salty ice VII under pressure. Nature Mater 8, 405–409 (2009). https://doi.org/10.1038/nmat2422
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DOI: https://doi.org/10.1038/nmat2422
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