Structure, thermal expansion and incompressibility of MgSO4·9H2O, its relationship to meridianiite (MgSO4·11H2O) and possible natural occurrences

Fortes, A.D.; Knight, K.S.; Wood, I.G.

doi:10.1107/S2052520616018266

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

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Figure 6
Principal and volume thermal expansion coefficients of MS9 as a function of temperature. Solid lines are derived from smoothed values calculated using the Einstein-model fit parameters reported in Table 3

. Symbols are `point-by-point' derivatives of the raw cell parameter values calculated across a moving window 15 K wide. The dashed red line in (d) depicts the volume thermal expansion of MS11 for comparison with that of MS9: the dotted blue line represents the unconstrained double-Debye model fit to the data (see text in the supporting information)

STRUCTURAL SCIENCE
CRYSTAL ENGINEERING
MATERIALS

ISSN: 2052-5206

Volume 73| Part 1| February 2017| Pages 47-64

https://doi.org/10.1107/S2052520616018266

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