The graphite arc-discharge in the presence of CCl4:: Chlorinated carbon clusters in relation with fullerenes formation

被引:10
作者
Gao, F
Xie, SY [1 ]
Ma, ZJ
Feng, YQ
Huang, RB
Zheng, LS
机构
[1] Xiamen Univ, Dept Chem, State Key Lab Phys Chem Solid Surfaces, Xiamen 361005, Peoples R China
[2] Wuhan Univ, Dept Chem, Wuhan 430072, Peoples R China
基金
中国国家自然科学基金;
关键词
fullerene; carbon clusters; arc discharge; mass spectrometry;
D O I
10.1016/j.carbon.2004.03.028
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The graphite arc-discharge in the atmosphere consisting of CCl4 40 Torr and increasing partial pressure of He from 0 to 300 Torr produced, in addition to carbon species such as graphite and fullerenes C-60 and C-70, numerous chlorinated carbon clusters (CCCs). The yields of some CCCs, including C6Cl6 (perchlorobenzene), C10Cl8 (perchloronaphthalene), C12Cl8 (perchloroacenaphthylene) and C12Cl8 (isomer II), C14Cl8 (isomer I), C16Cl10 (perchlorofluoranthene), C18Cl10 (isomer I and II), and C20Cl10 (isomer I), correspond well with C-60 yields, which may imply these CCCs share the same growth mechanism with fullerenes. Such a yield correlation can be used to distinguish the fullerene precursors from the irrelevant by-products, thus contributes to the mechanistic study of fullerene formation. (C) 2004 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1959 / 1963
页数:5
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