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http://www.repositorio.ufop.br/jspui/handle/123456789/14645
Título: | Hard, transparent, sp3 -containing 2D phase formed from few-layer graphene under compression. |
Autor(es): | Martins, Luiz Gustavo Pimenta Silva, Diego L. Smith, Jesse S. Lu, Ang-Yu Su, Cong Hempel, Marek Occhialini, Connor Ji, Xiang Pablo, Ricardo Alencar, Rafael Silva Souza, Alan Custodio dos Reis Pinto, Alysson Alves Oliveira, Alan Barros de Batista, Ronaldo Junio Campos Palacios, Tomas Mazzoni, Mário Sérgio de Carvalho Matos, Matheus Josué de Souza Comin, Riccardo Kong, Jing Cançado, Luiz Gustavo de Oliveira Lopes |
Data do documento: | 2021 |
Referência: | MARTINS, L. G. P. et al. Hard, transparent, sp3 -containing 2D phase formed from few-layer graphene under compression. Carbon, v. 173, p. 744-757, 2021. Disponível em: <https://www.sciencedirect.com/science/article/abs/pii/S0008622320311179>. Acesso em: 25 ago. 2021. |
Resumo: | 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 4e6 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 z 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 (z 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, surfaceto-bulk phase transition mechanism that gives hint of diamondene formation. |
URI: | http://www.repositorio.ufop.br/jspui/handle/123456789/14645 |
Link para o artigo: | https://www.sciencedirect.com/science/article/abs/pii/S0008622320311179 |
DOI: | https://doi.org/10.1016/j.carbon.2020.11.038 |
ISSN: | 0008-6223 |
Aparece nas coleções: | DEFIS - Artigos publicados em periódicos |
Arquivos associados a este item:
Arquivo | Descrição | Tamanho | Formato | |
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ARTIGO_HardTransparentSp.pdf Restricted Access | 3,01 MB | Adobe PDF | Visualizar/Abrir |
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