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Investigation of high-pressure planetary ices by cryo-recovery. II. High-pressure apparatus, examples and a new high-pressure phase of MgSO₄·5H₂O

Wang, W; Fortes, AD; Dobson, DP; Howard, CM; Bowles, J; Hughes, NJ; Wood, IG; (2018) Investigation of high-pressure planetary ices by cryo-recovery. II. High-pressure apparatus, examples and a new high-pressure phase of MgSO₄·5H₂O. Journal of Applied Crystallography , 51 (3) pp. 692-705. 10.1107/S1600576718003977. Green open access

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Abstract

An apparatus is described for the compression of samples to ∼2 GPa at temperatures from 80 to 300 K, rapid chilling to 80 K whilst under load and subsequent recovery into liquid nitro­gen after the load is released. In this way, a variety of quenchable high-pressure phases of many materials may be preserved for examination outside the high-pressure sample environment, with the principal benefit being the ability to obtain high-resolution powder diffraction data for phase identification and structure solution. The use of this apparatus, in combination with a newly developed cold-loadable low-temperature stage for X-ray powder diffraction (the PheniX-FL), is illustrated using ice VI (a high-pressure polymorph of ordinary water ice that is thermodynamically stable only above ∼0.6 GPa) as an example. A second example using synthetic epsomite (MgSO₄·7H₂O) reveals that, at ∼1.6 GPa and 293 K, it undergoes incongruent melting to form MgSO₄·5H₂O plus brine, contributing to a long-standing debate on the nature of the high-pressure behaviour of this and similar highly hydrated materials. The crystal structure of this new high-pressure polymorph of MgSO₄·5H₂O has been determined at 85 K in space group Pna2₁ from the X-ray powder diffraction pattern of a sample recovered into liquid nitro­gen and is found to differ from that of the known ambient-pressure phase of MgSO₄·5H₂O (pentahydrite, space group [P {\overline 1}]), consisting of corner-sharing MgO₆—SO₄ ion pairs rather than infinite corner-sharing chains.

Type: Article
Title: Investigation of high-pressure planetary ices by cryo-recovery. II. High-pressure apparatus, examples and a new high-pressure phase of MgSO₄·5H₂O
Location: United States
Open access status: An open access version is available from UCL Discovery
DOI: 10.1107/S1600576718003977
Publisher version: https://doi.org/10.1107/S1600576718003977
Language: English
Additional information: © 2018 Wang et al. This is an open access article distributed under the terms the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0/).
Keywords: planetary ices, high pressure, cryo-recovery, epsomite, magnesium sulfate pentahydrate
UCL classification: UCL
UCL > Provost and Vice Provost Offices > UCL BEAMS
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences > Dept of Earth Sciences
URI: https://discovery.ucl.ac.uk/id/eprint/10050874
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