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首页> 外文期刊>The Canadian Mineralogist >CHROMATE ALUMINATE SODALITE, Ca8[Al12O24](CrO4)2: PHASE TRANSITIONS AND HIGH-TEMPERATURE STRUCTURAL EVOLUTION OF THE CUBIC PHASE
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CHROMATE ALUMINATE SODALITE, Ca8[Al12O24](CrO4)2: PHASE TRANSITIONS AND HIGH-TEMPERATURE STRUCTURAL EVOLUTION OF THE CUBIC PHASE

机译:铬酸铝方钠钙Ca8 [Al12O24](CrO4)2:立方相的相变和高温结构演化

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The structural behavior of a chromate aluminate sodalite, Ca8[Al12O24](CrO4)2, at room pressure and on heating from 463 to 982°C was determined by using in situ synchrotron X-ray powder-diffraction data [ = 0.91997(4) Å] and Rietveld refinements. The sample was heated at a rate of about 9.5°C/min., and X-ray traces were collected at intervals of about 17°C. The structure at 463°C is a modulated cubic phase, whereas above 512°C, the structure is cubic with space group I3m. The a parameter increases linearly from 512 to 982°C, and the percent change in volume is 0.9(1)%. Between 463 and 982°C, the Al–O distance is nearly constant, the angle of rotation of the AlO4 tetrahedron, Al, decreases by 0.6° and simultaneously, the Al–O–Al bridging angle increases by 0.8(2)°. Between 463 to 982°C, the Ca–O distances are nearly constant. The Ca atom is located nearly in the plane of the three O’ framework atoms, so movement of the Ca atom out of this plane will cause longer Ca–O’ bonds instead of shorter bonds that occur when the Ca atom is migrating toward this plane. The highly charged [Ca4·CrO4]6+ clusters bond strongly to the framework oxygen atoms, which limits the rotation of the framework AlO4 tetrahedra; as a result, the expansion of the structure is small. We evaluate the differences between the thermal behavior of chromate aluminate sodalite and that of other structurally related phases (e.g., sodalite and danalite).
机译:铬酸铝钙钠方石Ca 8 [Al 12 O 24 ](CrO 4 )<的结构行为sub> 2 在室温和从463加热到982°C时通过使用原位同步加速器X射线粉末衍射数据[ up> sup> = 0.91997(4)Å]和Rietveld改进。以大约9.5°C / min的速度加热样品,以大约17°C的间隔收集X射线痕迹。 463°C 的结构是调制立方相,而512°C以上, 的结构为立方,空间群为I3m。 参数从512°C线性增加到982°C, 体积变化百分比为0.9(1)%。在463至982°C之间, Al–O距离几乎恒定,即AlO 4 四面体的旋转角 Al 减小0.6°,同时 Al–O–Al桥接角度增加0.8(2)°。 在463至982°C之间, Ca–O距离几乎是 恒定的。 Ca原子几乎位于 三个O'骨架原子的平面内,因此Ca原子从该平面的 移出将导致更长的Ca–O'键当Ca原子向此平面迁移时出现的 短键。高度带电的[Ca 4 ·CrO 4 ] 6 + 与框架氧原子牢固键合限制框架AlO 4 四面体的 旋转;结果,该结构的 扩展很小。我们评估了铬酸铝酸盐方钠石 与其他结构相关相(例如,方钠石 和方钠石)的热行为之间的差异 。 >

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    《The Canadian Mineralogist》 |2004年第4期|p.00001047-00001056|共10页
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