Improvement of stacking order in graphite by molten fluoride salt infiltration

被引:51
作者
He Zhoutong [1 ]
Gao Lina [1 ]
Wang Xue [1 ]
Zhang Baoliang [1 ,3 ]
Qi Wei [1 ,2 ]
Song Jinliang [1 ]
He Xiujie [1 ,3 ]
Zhang Can [1 ]
Tang Hui [1 ]
Xia Huihao [1 ]
Zhou Xingtai [1 ]
机构
[1] Chinese Acad Sci, Key Lab Nucl Radiat & Nucl Energy Technol, Shanghai 201800, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Shandong Univ, Sch Phys, Jinan 250100, Peoples R China
基金
中国国家自然科学基金;
关键词
THERMAL-EXPANSION; COMPOSITES; MICROSTRUCTURE; EVOLUTION;
D O I
10.1016/j.carbon.2014.02.010
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 structure of molten fluoride salt infiltrated graphite has been studied by X-ray diffraction and Raman spectroscopy. The full width at half maximum and asymmetry degree of the (002) diffraction peak decrease with the increase of salt weight gain in the infiltration indicates the improvement of the stacking order of the graphite by the molten salt infiltration. The shape of G' resonance of Raman spectra further indicated the enhancement of the stacking order of graphite by molten salt infiltration. The shift of the (002) diffraction peak position to the higher 2 theta angle and the increase of the coefficient of thermal expansion reveal that the improvement of the stacking order is resulted from the compression of the graphite matrix by the infiltrated salt network. The compressive stress induced by the salt network in the graphite matrix could reduce the d-spacing fluctuation between graphite basal planes and close the Mrozowski crack generated by the anisotropy of graphite crystal, thus increase the crystallite size along c-axis. (C) 2014 Elsevier Ltd. All rights reserved.
引用
收藏
页码:304 / 311
页数:8
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