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

IUCr IT WDC

home archive editors for authors for readers submit subscribe open access

view article

Figure 8
Depiction of the compressibility representation surface at 0 MPa superimposed on the unit cell of meridianiite where only the central water hexadecamer is shown. This emphasizes that the stiffest direction is along the long axis of the cluster and the most compressible direction is parallel to the two bifurcated hydrogen bonds.

STRUCTURAL SCIENCE
CRYSTAL ENGINEERING
MATERIALS

ISSN: 2052-5206

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

https://doi.org/10.1107/S2052520616018254

Open

access

Follow Acta Cryst. B

Search IUCr Journals		doi		Advanced search
Author		volume	page