Transition of current of lithium intercalation from solution to graphite

被引:6
|
作者
Wang, Xiaoxia [1 ]
Aoki, Koichi [1 ]
机构
[1] Univ Fukui, Dept Appl Phys, Fukui 9108507, Japan
关键词
critical concentration; intercalation of lithium ion; chronoamperometry; diffusion coefficient; graphite;
D O I
10.1016/j.jelechem.2007.03.012
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
Intercalation current of Li+ to a graphite electrode varied sharply with [Li+] from the proportionality to a constant, exhibiting critical behavior at [Li+] = 10 mM. The voltarnmetrically cathodic peak current, which is caused by the intercalation, was proportional to the square-root of the scan rate, irrespective of the concentrations. The current for [Li+] < 10 mM is controlled both by diffusion and electric migration of Li+ in solution, whereas that for [Li+] > 10 mM is controlled by diffusion of Li in the graphite. In order to validate the critical behavior, the time-dependent mass transport theory was developed by use of the Nernst-Planck equation for the solution phase and the diffusion equation for the graphite one. Both equations were combined at the interface through a kind of the Nernst equation which contained a maximum concentration of Li in the graphite predicted from the structure of LiC6. The theory supported the critical behavior in the potential domain of the limiting current. From the critical concentration, the diffusion coefficient of Li in the graphite was estimated to be 0.79 x 10(-11) cm(2) s(-1), independent of the concentrations. (c) 2007 Elsevier B.V. All rights reserved.
引用
收藏
页码:101 / 108
页数:8
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