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 4
Representation glyphs of the unit-strain tensor surface corresponding to (a) thermal expansion at 240 K (after Fortes et al., 2008

), (b) compressibility at zero pressure and (c) compressibility at 900 MPa. Black arrows indicate the orthogonal reference frame [cf. Equation (3

) and Fig. 5

a]. Coloured arrows show the eigenvectors of the Eulerian infinitesimal unit-strain tensor. Representation surfaces created using WinTensor (Kaminski, 2004

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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