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Crystal structure and high pressure behaviour of the quartz-type phase of phosphorus oxynitride PON

1999; Elsevier BV; Volume: 60; Issue: 2 Linguagem: Inglês

10.1016/s0022-3697(98)00282-0

1879-2553

Jean‐Michel Léger, Julien Haines, Lia Silva de Oliveira, C. Chateau, André Le Sauze, Roger Marchand, S. Hull,

Crystal Structures and Properties

Phosphorus oxynitride PON is isoelectronic with SiO2 and both exhibit cristobalite- and quartz-type phases. The α-quartz phase of PON was prepared by submitting the β-cristobalite phase to 4.5 GPa and 750°C in a belt type apparatus. The structure at ambient was refined using time-of-flight neutron powder diffraction data on a quenched sample. The structure (trigonal, P3221, a=4.757(4), c=5.2460(2) Å, Z=3) is essentially the same as that of α-quartz SiO2. The atomic positions and temperature factors of phosphorus, oxygen and nitrogen were obtained. Oxygen and nitrogen are completely disordered over the 6(c) sites. The behaviour of α-quartz-type PON under pressure was determined by angle dispersive X-ray powder diffraction in a diamond anvil cell up to 48 GPa. The cell parameters were measured as a function of pressure. A transition to an α-quartz II phase occurs at close to 20 GPa; the main change is a small, but distinct increase in the c/a ratio. Progressive and irreversible amorphisation of PON was observed above 30 GPa, and no diffraction lines could be detected above 42 GPa. For both PON and SiO2, the α-quartz-type phases undergo phase changes under pressure to quartz II phases followed by amorphisation. This pressure study reinforces the parallel behaviour of the two compounds.