Direct Real-Time Monitoring of Stage Transitions in Graphite Intercalation Compounds

被引:163
作者
Dimiev, Ayrat M. [1 ]
Ceriotti, Gabriel [1 ]
Behabtu, Natnael [2 ]
Zakhidov, Dante [1 ]
Pasquali, Matteo [2 ,4 ]
Saito, Riichiro [5 ]
Tour, James M. [1 ,3 ,4 ]
机构
[1] Rice Univ, Dept Chem, Houston, TX 77005 USA
[2] Rice Univ, Dept Chem & Biomol Engn, Houston, TX 77005 USA
[3] Rice Univ, Dept Mech Engn & Mat Sci, Houston, TX 77005 USA
[4] Rice Univ, Smalley Inst Nanoscale Sci & Technol, Houston, TX 77005 USA
[5] Tohoku Univ, Dept Phys, Sendai, Miyagi 9808578, Japan
关键词
graphite intercalation compounds; graphene; stage transition mechanism; Raman spectroscopy; D band origin; RAMAN-SPECTROSCOPY; ANODIC-OXIDATION; SULFURIC-ACID; DEFECTS;
D O I
10.1021/nn400207e
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Graphite intercalation compounds (GIC) possess a broad range of unique properties that are not specific to the parent materials. While the stage transition, changing the number of graphene layers sandwiched between the two layers of intercalant, is fundamentally important and has been theoretically addressed, experimental studies revealed only macroscopic parameters. On the microscale, the phenomenon remains elusive up to the present day. Here we monitor directly in real time the stage transitions using a combination of optical microscopy and Raman spectroscopy. These direct observations yield several mechanistic conclusions. While we obtained strong experimental evidence In support of the Daumas Herold theory, we find that the conventional interpretation of stage transitions as sliding of the existing intercalant domains does not sufficiently capture the actual phenomena. The entire GIC structure transforms considerably during the stage transition. Among other observations, massive wavefront-like perturbations occur on the graphite surface, which we term the tidal wave effect.
引用
收藏
页码:2773 / 2780
页数:8
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