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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Thermoelastic properties of post-perovskite phase MgSiO3 determined experimentally at core-mantle boundary P-T conditions
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Thermoelastic properties of post-perovskite phase MgSiO3 determined experimentally at core-mantle boundary P-T conditions

机译:钙钛矿后相MgSiO3在芯-幔边界P-T条件下的实验确定的热弹性性质

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摘要

We have performed in-situ X-ray diffraction measurements on MgSiO3 UP to 144.5 GPa and 2535 K to obtain a precise experimental determination of the elastic properties of the post-perovskite polymorph Of MgSiO3 at high pressure and temperature. The complete dataset is comprised of 24 data points at ambient temperature and an equal number at high temperature. Fitted physical properties are the room temperature bulk modulus, the Gruneisen parameter with its volume dependency, the thermal expansion with its temperature dependency, and the linear incompressibilities as well as thermal expansions and their temperature dependency on each axis. Elastic anisotropy is observed, the structure being much more compressible along the b axis, and less compressible along the c axis, in agreement with theoretical calculations. We also demonstrate with the present study that experiments can provide precise information on the elasticity of complex materials at extreme pressure and temperature conditions. (c) 2007 Elsevier B.V. All rights reserved.
机译:我们已经在高达144.5 GPa和2535 K的MgSiO3上进行了原位X射线衍射测量,从而获得了在高温高压下钙钛矿后多晶型物MgSiO3弹性性能的精确实验测定。完整的数据集由环境温度下的24个数据点和高温环境下的相等数量的数据组成。拟合的物理特性包括室温的体积模量,具有体积依赖性的Gruneisen参数,具有温度依赖性的热膨胀,线性不可压缩性以及热膨胀及其与各轴的温度依赖性。与理论计算一致,观察到弹性各向异性,该结构沿b轴可压缩得多,而沿c轴可压缩少。我们还通过本研究证明,实验可以提供有关复杂材料在极端压力和温度条件下的弹性的精确信息。 (c)2007 Elsevier B.V.保留所有权利。

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