Mark W. Dowley
Solid State Communications
Powder data for Ag2SO4 were obtained with a conventional diffractometer equipped with a vacuum heating chamber. The transition from the low-temperature orthorhombic phase occurs over a temperature range of about 415° to 425°C and forms a hexagonal phase plus metallic silver. The lack of a sharp transition must be taken into account in high-temperature X-ray diffraction or DSC/DTA studies. The lattice parameters of the high-temperature hexagonal phase are a = 5.531(3), c = 7.456(5)Å at 440°C, λ = 1.540562 Å. Crystal structure determination was not completed because of uncertainty in the chemical composition. © 1990, Cambridge University Press. All rights reserved.
Mark W. Dowley
Solid State Communications
E. Burstein
Ferroelectrics
Shiyi Chen, Daniel Martínez, et al.
Physics of Fluids
A. Ney, R. Rajaram, et al.
Journal of Magnetism and Magnetic Materials