Isothermal equation of state and high-pressure phase transitions of synthetic meridianiite (MgSO4·11D2O) determined by neutron powder diffraction and quasielastic neutron spectroscopy

Fortes, A.D.; Fernandez-Alonso, F.; Tucker, M.; Wood, I.G.

doi:10.1107/S2052520616018254

Acta Crystallographica Section B
Acta Crystallographica
Section B STRUCTURAL SCIENCE, CRYSTAL ENGINEERING AND MATERIALS

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Figure 11
Comparison of powder diffraction data obtained in Experiment 1 (a), directly after the pressure-induced breakdown of meridianiite at 0.91 GPa, 240 K, and a linear sum (b) of the neutron powder diffraction patterns of MgSO₄·9D₂O (c), with a small shift in d-spacing to account for the pressure difference (see text) and D₂O ice VI (d).

STRUCTURAL SCIENCE
CRYSTAL ENGINEERING
MATERIALS

ISSN: 2052-5206

Volume 73| Part 1| February 2017| Pages 33-46

https://doi.org/10.1107/S2052520616018254

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