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高压诱导水铝石的堆积无序化。

Pressure-induced stacking disorder in boehmite.

机构信息

Geochemical Research Center, Graduate School of Science, The University of Tokyo, Hongo 7-3-1, Bunkyo-ku, Tokyo 113-0033, Japan.

出版信息

Phys Chem Chem Phys. 2018 Jun 20;20(24):16650-16656. doi: 10.1039/c8cp02565g.

Abstract

The structure of an aluminum layered hydroxide, boehmite (γ-AlOOH), as a function of pressure was studied by using in situ synchrotron X-ray and neutron diffraction. Peak broadening, which is only found for hkl (h ≠ 0) peaks in the X-ray diffraction patterns, is explained by stacking disorder accompanying a continuously increasing displacement of the AlO6 octahedral layer along the a-axis. This finding could be the first experimental result for pressure-induced stacking disorder driven by continuous layer displacement. The magnitude of the layer displacement was estimated from the X-ray scattering profile calculation based on the stacking disordered structure model. Hydrogen bond geometries of boehmite, obtained by structure refinements of the observed neutron diffraction patterns for the deuterated sample up to 10 GPa, show linearly approaching O-D covalent and DO hydrogen bond distances and they merge below 26 GPa. Pressure-induced stacking disorder makes the electrostatic potential of hydrogen bonds asymmetric, yielding less chance for proton-tunnelling.

摘要

采用同步加速器 X 射线和中子衍射原位研究了铝层状氢氧化物,即勃姆石(γ-AlOOH)的结构随压力的变化。X 射线衍射图谱中仅发现 hkl(h ≠ 0)峰的峰宽展宽,这可以用沿 a 轴方向 AlO6 八面体层不断增大的位移引起的堆叠无序来解释。这一发现可能是首次实验证明由连续层位移驱动的压力诱导堆叠无序。根据基于堆叠无序结构模型的 X 射线散射谱计算,估算了层位移的大小。通过对氘化样品在 10 GPa 以下的观察到的中子衍射图谱的结构精修,得到了勃姆石的氢键几何形状,结果表明 O-D 共价和 DO 氢键距离呈线性接近,并且在低于 26 GPa 时合并。压力诱导的堆叠无序使氢键的静电势不对称,质子隧穿的机会减少。

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