Evidence for re-crystallization process in the irradiated graphite with heavy ions obtained by Raman spectroscopy
Evidence for re-crystallization process in the irradiated graphite with heavy ions obtained by Raman spectroscopy
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通过拉曼光谱获得重离子辐照石墨中重结晶过程的证据
DOI:
10.1016/j.carbon.2016.01.076
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发表时间:
2016-05
期刊:
影响因子:
10.9
通讯作者:
Youmei Sun
中科院分区:
文献类型:
--
作者:
Pengfei Zhai;Jie Liu;Jian Zeng;Jinglai Duan;Lijun Xu;Huijun Yao;Hang Guo;Shengxia Zhang;Mingdong Hou;Youmei Sun
Highly oriented pyrolytic graphite (HOPG) was irradiated with 40.5 MeV112Sn ions at a range of fluence: 1 × 1012–1 × 1014ions/cm2. A new Raman band was observed at ∼864 cm−1which grows with increasing the irradiation fluence. This band has been observed in Raman spectra of HOPG and natural graphite crystal edge planes, only when the incident light is polarized perpendicular to the basal planes and it has been assigned to the out-of-plane Raman-inactiveB2gmode which becomes Raman active due to a slight rearrangement of lattice structure at the edge. However, we first obtained this band in Raman spectra of basal planes of irradiated HOPG with the polarization of the incident light parallel to the basal planes. Then, a half-wave plate was used to change the polarization direction of the incident light in the HOPG basal planes. The intensity of the band at 864 cm−1is almost independent of the incident light polarization direction. We suggest that re-crystallized graphite with random lattice orientations are formed during ion irradiation, which gives rise to theB2gband. The conclusion is confirmed by transmission electron microscopy images, showing that there are some randomly orientated nanoscale graphite crystals surrounded by amorphous carbon.
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