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首页> 外文期刊>Materials Chemistry and Physics >Structure, elasticity and stability of reidite (ZrSiO_4) under hydrostatic pressure: A density functional study
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Structure, elasticity and stability of reidite (ZrSiO_4) under hydrostatic pressure: A density functional study

机译:静水压力下Reidite(ZrSiO_4)的结构,弹性和稳定性:密度泛函研究

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摘要

We investigate the lattice parameters, elastic constants and the stability of ZrSiO_4 phases using plane wave implementation of the density functional theory within the framework of local density approximation (LDA). ZrSiO_4 occurs as a stable tetragonal phase (zircon, 141/amd) in the ambient condition, which undergoes a transition to reidite phase (I41/a) at a pressure of 7.3 GPa. Our study predicts that the silicate phase can experience another transformation (reconstructive phase transition) to a phase with wolframite structure (P2/c) at 75.8 GPa. Electronic band gaps of zircon and reidite widen with pressure, whereas that of wolframite declines at a threshold pressure (72 GPa). The bulk modulus of reidite steadily increases with pressure, but its shear modulus follows a quadratic variation, showing drops at pressures >75 GPa. Finally, we interpret that the reidite to wolframite transition results from increasing cation-cation repulsive forces and negative pressure derivatives of shear modulus.
机译:我们在局部密度近似(LDA)框架内,使用密度泛函理论的平面波实现方法,研究了ZrSiO_4相的晶格参数,弹性常数和稳定性。 ZrSiO_4在环境条件下以稳定的四方相形式存在(锆石,141 / amd),并在7.3 GPa的压力下转变为堇青石相(I41 / a)。我们的研究预测,在75.8 GPa时,硅酸盐相会经历另一种转变(重构相变),转变为具有钨铁矿结构(P2 / c)的相。锆石和黑云母的电子带隙随着压力而增大,而黑钨矿的电子带隙在阈值压力(72 GPa)下下降。随压力的变化,堇青石的体积模量稳定增加,但其剪切模量呈二次方变化,在压力> 75 GPa时下降。最后,我们解释说,由增加的阳离子-阳离子排斥力和剪切模量的负压导数导致了从辉石到黑钨矿的转变。

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