白钨矿
四方晶系
锆石
材料科学
结晶学
类型(生物学)
钇
十二面体
衍射
粉末衍射
晶体结构
物理
地质学
钨
光学
化学
核物理学
冶金
古生物学
氧化物
作者
X. Wang,I. Loa,K. Syassen,Michael Hanfland,B Ferrand
标识
DOI:10.1103/physrevb.70.064109
摘要
The laser host material yttrium orthovanadate ${\mathrm{YVO}}_{4}$ with a tetragonal zircon-type structure has been studied by angle-dispersive powder x-ray diffraction in a diamond anvil cell up to $26\phantom{\rule{0.3em}{0ex}}\mathrm{GPa}$ $(T=300\phantom{\rule{0.3em}{0ex}}\mathrm{K})$. In situ diffraction confirms that the compound undergoes a nonreversible transformation to a scheelite-type structure at a pressure of $8.5\phantom{\rule{0.3em}{0ex}}\mathrm{GPa}$. The equations of state of the zircon and scheelite phases and changes in internal structural parameters are reported. The effect of pressure on the distorted tetrahedral and dodecahedral coordinations of the V and Y ions, respectively, is discussed.
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