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Structural characterization of a new high-pressure phase of GaAsO4

机译:GaAsO4新型高压相的结构表征

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As in SiO2 which, at high pressures, undergoes the alpha-quartz -> stishovite transition, GaAsO4 transforms into a dirutile structure at 9 GPa and 1173 K. In 2002, a new GaAsO4 polymorph was found by quenching the compound from 6 GPa and 1273 K to ambient conditions. The powder diagram was indexed on the basis of a hexagonal cell (a = 8.2033, c = 4.3941 A, V = 256.08 A(3)), but the structure did not correspond to any known structure of other AXO(4) compounds. We report here the ab initio crystal structure determination of this hexagonal polymorph from powder data. The new phase is isostructural to beta-MnSb2O6 and it can be described as a lacunary derivative of NiAs with half the octahedral sites being vacant, but it also contains fragments of the rutile-like structure.
机译:就像在高压下经历α-石英->辉石过渡的SiO2中一样,GaAsO4在9 GPa和1173 K时转变为一种易碎的结构。2002年,通过淬灭6 GPa和1273中的化合物发现了一种新的GaAsO4多晶型物。 K到环境条件。粉末图基于六角形单元索引(a = 8.2033,c = 4.3941 A,V = 256.08 A(3)),但该结构与其他AXO(4)化合物的任何已知结构均不对应。我们从粉末数据中报告了这种六边形多晶型的从头算晶体结构的确定。该新相与β-MnSb2O6是同构的,可以描述为NiAs的腔衍生物,八面体位置的一半是空的,但它也包含金红石状结构的片段。

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