ArticleNature communications2024
Metastable water at several compression rates and its freezing kinetics into ice VII.
Article in Nature communications, 2024. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 8 papers.
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Who cites it
8 citing papers in PubMed.
- Probing electron transport and thermodynamic properties in expanded warm dense matter.Nature communications · 2026Article
- Using X-ray free electron lasers to explore extreme states under quasi-static compression.Nature communications · 2026Review
- Extremophile survives the transient pressures associated with impact-induced ejection from Mars.PNAS nexus · 2026Article
- Multiple freezing-melting pathways of high-density ice through ice XXI phase at room temperature.Nature materials · 2026Article
- The blackjack of ice.Nature materials · 2026Article
- Achieving nanosecond time resolution with a two-dimensional X-ray detector.Journal of synchrotron radiation · 2025Article
- Interpreting dynamic-compression experiments to uncover the time dependence of freezing: Application to gallium.Proceedings of the National Academy of Sciences of the United States of America · 2025Article
- Sulfur chains glass formed by fast compression.Nature communications · 2025Article
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Authors and funding
8 authors.
Funding
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Abstract
Water can be dynamically over-compressed well into the stability field of ice VII. Whether water then transforms into ice VII, vitreous ice or a metastable novel crystalline phase remained uncertain. We report here the freezing of over-compressed water to ice VII by time-resolved X-ray diffraction. Quasi-isothermal dynamic compression paths are achieved using a dynamic-piezo-Diamond-Anvil-Cell, with programmable pressure rise time from 0.1 ms to 100 ms. By combining the present data set with those obtained on various ns-dynamical platforms, a complete evolution of the solidification pressure of metastable water versus the compression rate is rationalized within the classical nucleation theory framework. Also, when crystallization into ice VII occurs in between 1.6 GPa and 2.0 GPa, that is in the stability field of ice VI, a structural evolution over few ms is then observed into a mixture of ice VI and ice VII that seems to resolve apparent contradictions between previous results.
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Registered trials
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