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室温压缩和解压下石墨的晶体结构。

Crystal structure of graphite under room-temperature compression and decompression.

机构信息

Department of Geology and Geophysics, Yale University, New Haven, CT 06520, USA.

出版信息

Sci Rep. 2012;2:520. doi: 10.1038/srep00520. Epub 2012 Jul 19.

Abstract

Recently, sophisticated theoretical computational studies have proposed several new crystal structures of carbon (e.g., bct-C(4), H-, M-, R-, S-, W-, and Z-carbon). However, until now, there lacked experimental evidence to verify the predicted high-pressure structures for cold-compressed elemental carbon at least up to 50 GPa. Here we present direct experimental evidence that this enigmatic high-pressure structure is currently only consistent with M-carbon, one of the proposed carbon structures. Furthermore, we show that this phase transition is extremely sluggish, which led to the observed broad x-ray diffraction peaks in previous studies and hindered the proper identification of the post-graphite phase in cold-compressed carbon.

摘要

最近,复杂的理论计算研究提出了几种新的碳晶体结构(例如 bct-C(4)、H-、M-、R-、S-、W- 和 Z-碳)。然而,到目前为止,还缺乏实验证据来验证至少在 50 GPa 高压下冷压元素碳的预测高压结构。在这里,我们提供了直接的实验证据,表明这种神秘的高压结构目前仅与 M-碳一致,M-碳是提出的碳结构之一。此外,我们表明这种相变非常缓慢,这导致了先前研究中观察到的宽 X 射线衍射峰,并阻碍了冷压碳中石墨后相的正确识别。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9108/3400081/1c90389e9a16/srep00520-f1.jpg

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