The intercalation rate of Li+-ions in flake natural graphite with particle
size that ranged from 2 to 40 mum was investigated. The amount of Li+-ions
that intercalate at different rates was determined from measurement of the
reversible capacity during deintercalation in 1 M LiClO4/1:1 (volume ratio)
ethylene carbonate-dimethyl carbonate. The key issues in this study are th
e role of particle size and fraction of edge sites on the rate of intercala
tion and deintercalation of Li+-ions. At low specific current (15.5 mA/g ca
rbon), the composition of lithiated graphite approaches the theoretical val
ue, x = 1 in LixC6, except for the natural graphite with the largest partic
le size. However, x decreases with an increase in specific current for all
particle sizes. This trend suggests that slow solid-state diffusion of Li+-
ions limits the intercalation capacity in graphite. The flake natural graph
ite with a particle size of 12 mum may provide the optimum combination of r
eversible capacity and irreversible capacity loss in the electrolyte and di
scharge rates used in this study. (C) 2001 Elsevier Science B.V. All rights
reserved.