Bulletin of the American Physical Society
23rd Biennial Conference of the APS Topical Group on Shock Compression of Condensed Matter
Volume 68, Number 8
Monday–Friday, June 19–23, 2023; Chicago, Illinois
Session R06: SHP-Structural Study
11:15 AM–12:45 PM,
Wednesday, June 21, 2023
Sheraton Grand Chicago Riverwalk
Room: Chicago 8
Chair: Sakun Duwal
Abstract: R06.00003 : Microsecond-timescale dynamic compression of water probed by time-resolved X-ray Diffraction and Spectroscopy
11:45 AM–12:15 PM
Presenter:
Charles Pépin
(CEA)
Authors:
Charles Pépin
(CEA)
Matteo Levantino
(ESRF)
Florent Occelli
(CEA)
Arnaud Sollier
(CEA Bruyères-le-Châtel)
Ramesh André
(CEA)
Aldo Mozzanica
(PSI)
Viktoria Hinger
(PSI)
Paul Loubeyre
(CEA de Bruyeres-le-Chatel)
H2O has been extensively studied both under static compression in the DAC and under laser-shock compression, allowing the observation of a large number of polymorphs [1, 2]. It has been one of the first system to be studied in the dDAC because of the implication for fundamental physics of diffusion-mediated properties and for the thermodynamic modeling of collision/impact events on ice-rich planetary bodies. Based on visual and Raman observation, super-compressed liquid water was first reported to crystallize into ice VII in the stability field of ice VI [3]. However, it was then reported that the metastable ice VII in the stability field of ice VI forms a high-density amorphous ice [4]. The determination of the nucleation and growth mechanisms were however unknown.
This work focuses on the use of a piezo-electrically driven dDAC to achieve a rapid pressure change on liquid water. Homogenous nucleation of ice is monitored using both time-resolved XRD at the ESRF ID09 beamline and spectroscopy. Our results reveal that at sufficiently high compression rate,water can be over-pressurized into the stability domain above the ice VII metastable melting line where the freezing into ice VII becomes more favourable as observed for the first time by XRD. Using a classical nucleation theory, we show that the nucleation time of ice VII can be directly linked to the overcompression. The deduced nucleation law unifies the results from the dDAC, the Z-machine ramp compression [5] and the laser ramp compression in the case of homogenous nucleation [6].
[1] J.A. Queyroux et al. PRL 125, 195501 (2020)
[2] M. Millot et al. Nature 569, 251 (2019)
[3] G.W. Lee et al. PRB 74, 134112 (2006).
[4] J-Y Chen et al. PNAS 108, 7685 (2011).
[5] Dolan D.Het al. Nat. Phys. 3, 339 (2007)
[6] Marshall M.C. et al. PRL 127, 135701 (2021)
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