Dry ice II, a new polymorph of CO2

Computer Science

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Carbon Dioxide, Crystal Structure, Ice, Planetary Composition, Polymorphism, Phase Diagrams, Phase Transformations, X Ray Diffraction

Scientific paper

In situ studies of high-pressure phase transformations of CO2 have been performed with both optical and X-ray observations in a standard gasketed diamond anvil pressure cell. A new polymorph of dry ice was observed in the pressure range between about 5 and 23 kbar at room temperature. No X-ray powder diffraction pattern for the solid phase crystallized from liquid CO2 was obtained because of the strong tendency to form large single crystals, except when a 'metastable' liquid CO2 suddenly transformed to the new solid phase accompanied by an explosion. The quality of the powder diffraction data thus produced is too poor to deduce a possible structural type for the new phase. On the basis of optical observations, dry ice II might have a refractive index and/or density very similar to ordinary dry ice (type I) in the vicinity of 23 kbar at room temperature.

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