Hard, transparent, sp3-containing 2D phase formed from few-layer graphene under compression

石墨烯 材料科学 拉曼光谱 石墨 相变 钻石 相(物质) 静水压力 基质(水族馆) 金刚石顶砧 复合材料 流体静力平衡 压缩(物理) 化学物理 纳米技术 图层(电子) 凝聚态物理 高压 热力学 光学 化学 有机化学 量子力学 物理 地质学 海洋学
作者
Luiz G. P. Martins,Diego L. Silva,Jesse S. Smith,Ang‐Yu Lu,Cong Su,Marek Hempel,Connor A. Occhialini,Xiang Ji,Ricardo Pablo,Rafael S. Alencar,Alan C. R. Souza,Alysson A. Pinto,Alan B. de Oliveira,Ronaldo J. C. Batista,Tomás Palacios,Mário S. C. Mazzoni,Matheus J. S. Matos,Riccardo Comin,Jing Kong,Luiz Gustavo Cançado
出处
期刊:Carbon [Elsevier BV]
卷期号:173: 744-757 被引量:43
标识
DOI:10.1016/j.carbon.2020.11.038
摘要

Abstract Despite several theoretically proposed two-dimensional (2D) diamond structures, experimental efforts to obtain such structures are in initial stage. Recent high-pressure experiments provided significant advancements in the field, however, expected properties of a 2D-like diamond such as sp3 content, transparency and hardness, have not been observed together in a compressed graphene system. Here, we compress few-layer graphene samples on SiO2/Si substrate in water and provide experimental evidence for the formation of a quenchable hard, transparent, sp3-containing 2D phase. Our Raman spectroscopy data indicates phase transition and a surprisingly similar critical pressure for two-, five-layer graphene and graphite in the 4–6 GPa range, as evidenced by changes in several Raman features, combined with a lack of evidence of significant pressure gradients or local non-hydrostatic stress components of the pressure medium up to ≈ 8 GPa. The new phase is transparent and hard, as evidenced from indentation marks on the SiO2 substrate, a material considerably harder than graphene systems. Furthermore, we report the lowest critical pressure ( ≈ 4 GPa) in graphite, which we attribute to the role of water in facilitating the phase transition. Theoretical calculations and experimental data indicate a novel, surface-to-bulk phase transition mechanism that gives hint of diamondene formation.
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