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Centre National de la Recherche Scientifique, Laboratoire de Physico-Chimie des Materiaux, Meudon, France
A new polymorph of phosphorus oxynitride (PON) a silica analog has been recovered at ambient pressure by quenching after a treatment at 850 degrees C under a pressure of 2.5 GPa using cristobalite- or quartz-type phases as starting materials. This PON polymorph is a thermodynamically stable phase with its own stability field in a P-T diagram. The structure of this PON phase was refined by the Rietveld method from an X-ray powder diffractogram. It is isostructural with "moganite" (SiO 2 ). The discovery of this PON polymorph should stimulate a renewed interest in the occurrence of this phase in the silica system, because "moganite" may have a small but defined P-T stability field. These results confirm the structure of "moganite" as a new structure-type in AX 2 compounds.
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P. J. Heaney and J. E. Post Evidence for an I2/a to Imab phase transition in the silica polymorph moganite at ~570 K American Mineralogist, November 1, 2001; 86(11-12): 1358 - 1366. [Abstract] [Full Text] [PDF] |
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J.-M. LEGER, J. HAINES, and C. CHATEAU The high-pressure behaviour of the "moganite" polymorph of SiO2 European Journal of Mineralogy, April 1, 2001; 13(2): 351 - 359. [Abstract] [Full Text] [PDF] |
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