1995
DOI: 10.1016/0013-4686(94)00329-y
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Transport of intercalated anions in graphite according to Walden's rule

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Cited by 6 publications
(2 citation statements)
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“…The slopes and two sets of potential data for 10 and 1 5~ H2SO4 are summarized in Table 5. Charge-transfer kinetics at the phase boundary electrode (GIC)/electrolyte is due to ions [16], and exchange current densities were measured of io = 0.6 Ncm2 in 18 M H2SO4 but 0.014.1 Ncm2 in 1 M LiC104 in aprotic solvents [149,151]. The strong concentration effect represented by Fig.…”
Section: Acceptor (A)-type Gicsmentioning
confidence: 99%
“…The slopes and two sets of potential data for 10 and 1 5~ H2SO4 are summarized in Table 5. Charge-transfer kinetics at the phase boundary electrode (GIC)/electrolyte is due to ions [16], and exchange current densities were measured of io = 0.6 Ncm2 in 18 M H2SO4 but 0.014.1 Ncm2 in 1 M LiC104 in aprotic solvents [149,151]. The strong concentration effect represented by Fig.…”
Section: Acceptor (A)-type Gicsmentioning
confidence: 99%
“…These defects are localized; indeed, they cannot move from the lattice positions where they originate. Differently, H 2 SO 4 molecules are free to move by diffusion in the space between the adjacent graphite crystallographic planes and segregate mostly at the crystal edges to maximize all physical interactions, allowing the formation of a network of linear defects in the graphite matrix structure [4,14].…”
Section: Introductionmentioning
confidence: 99%