The thermal expansion and crystal structure of mirabilite (Na2SO4·10D2O) from 4.2 to 300 K, determined by time-of-flight neutron powder diffraction-Reference-Cited by-同舟云学术

The thermal expansion and crystal structure of mirabilite (Na2SO4·10D2O) from 4.2 to 300 K, determined by time-of-flight neutron powder diffraction

Published:2008-08-20 Issue:1 Volume:36 Page:29-46
ISSN:0342-1791
Container-title:Physics and Chemistry of Minerals
language:en
Short-container-title:Phys Chem Minerals

Author:

Brand H. E. A.,Fortes A. D.,Wood I. G.,Knight K. S.,Vočadlo L.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,General Materials Science

Link

http://link.springer.com/content/pdf/10.1007/s00269-008-0256-0.pdf

Reference73 articles.

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2. Balarew C (2002) Calculation of the free Gibbs energy of phase transitions using solubility data. 1. The system Na2SO4–Na2SeO4–H2O at 15°C: stable and metastable equilibria. Pure Appl Chem 74(10):1793–1800. doi: 10.1351/pac200274101793

3. Block EA (1913) Über die schmelzkurven einiger stoffe. Z Phys Chem Stoich Verwandt 82:403–438

4. Braitsch O (1971) Salt deposits, their origin and composition. Springer, New York

5. Brand HEA, Fortes AD, Wood IG, Alfredsson M, Vočadlo L (2006) High-pressure properties of planetary sulfate hydrates determined from interatomic potential calculations. Lunar Planet Sci Conf 37 (abstract #1310), ( http://www.lpi.usra.edu/meetings/lpsc2006/pdf/1310.pdf )

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