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激光驱动冲击波压缩多晶氧化铝中的高压相转变和强度估计。

High pressure phase transition and strength estimate in polycrystalline alumina during laser-driven shock compression.

机构信息

Department of Earth and Planetary Sciences, Johns Hopkins University, Baltimore, MD 21218, United States of America.

Department of Physics, Clarendon Laboratory, University of Oxford, Parks Road, Oxford OX1 3PU, United Kingdom.

出版信息

J Phys Condens Matter. 2022 Dec 28;35(9). doi: 10.1088/1361-648X/aca860.

Abstract

Alumina (AlO) is an important ceramic material notable for its compressive strength and hardness. It represents one of the major oxide components of the Earth's mantle. Static compression experiments have reported evidence for phase transformations from the trigonal-corundum phase to the orthorhombic RhO(II)-type structure at ∼90 GPa, and then to the post-perovskite structure at ∼130 GPa, but these phases have yet to be directly observed under shock compression. In this work, we describe laser-driven shock compression experiments on polycrystalline alumina conducted at the Matter in Extreme Conditions endstation of the Linac Coherent Light Source. Ultrafast x-ray pulses (50 fs, 10photons/pulse) were used to probe the atomic-level response at different times during shock propagation and subsequent pressure release. At 107 ± 8 GPa on the Hugoniot, we observe diffraction peaks that match the orthorhombic RhO(II) phase with a density of 5.16 ± 0.03 g cm. Upon unloading, the material transforms back to the-corundum structure. Upon release to ambient pressure, densities are lower than predicted assuming isentropic release, indicating additional lattice expansion due to plastic work heating. Using temperature values calculated from density measurements, we provide an estimate of alumina's strength on release from shock compression.

摘要

氧化铝(AlO)是一种重要的陶瓷材料,以其抗压强度和硬度而闻名。它是地球地幔主要氧化物成分之一。静态压缩实验已经证明,在约 90 GPa 时,从三方刚玉相转变为正交 RhO(II)-型结构,然后在约 130 GPa 时转变为后钙钛矿结构,但这些相尚未在冲击压缩下直接观察到。在这项工作中,我们描述了在 Linac Coherent Light Source 的 Matter in Extreme Conditions 终端进行的多晶氧化铝的激光驱动冲击压缩实验。超快 X 射线脉冲(50 fs,10 个光子/脉冲)用于在冲击传播和随后的压力释放过程中的不同时间探测原子级响应。在 107 ± 8 GPa 的冲击压缩状态下,我们观察到与正交 RhO(II)相匹配的衍射峰,其密度为 5.16 ± 0.03 g cm。卸载时,材料会恢复到刚玉结构。在释放到环境压力时,密度低于等熵释放的预测值,表明由于塑性功加热导致晶格进一步膨胀。我们使用密度测量计算的温度值,对冲击压缩释放后氧化铝的强度进行了估计。

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