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Effect of iron on delithiation in LixCo1-yFeyO2.: Part 2:: in-situ XANES and EXAFS upon electrochemical cycling
被引:14
作者:
Holzapfel, M
Proux, O
Strobel, P
Darie, C
Borowski, M
Morcrette, M
机构:
[1] UJF, INPG, CNRS, Lab Electrochim & Physicochim Mat & Interfaces, F-38402 St Martin Dheres, France
[2] CNRS, Lab Champs Magnet Intenses, F-38042 Grenoble 9, France
[3] Max Planck Inst Festkorperforsch, F-38042 Grenoble 9, France
[4] UJF, Lab Geophys Interne & Tectonophys, CNRS, UMR, F-38400 St Martin Dheres, France
[5] CNRS, Cristallog Lab, F-38042 Grenoble 9, France
[6] European Synchrotron Radiat Facil, F-38043 Grenoble, France
[7] UPJV, CNRS, Lab React & Chim Solides, F-80039 Amiens, France
关键词:
D O I:
10.1039/b307672e
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:
LixCo1-yFeyO2 solid solutions were examined in an in-situ electrochemical X-ray absorption spectroscopy study using a plastic battery configuration. XANES and EXAFS were applied to elucidate the evolution of local symmetry and oxidation states of iron and cobalt upon electrochemical cycling of three particular stoichiometries: LixCo0.9Fe0.1O2, LixCo0.8Fe0.2O2 and LixCo0.6Fe0.4O2. While the cobalt environment shows little variation, a distortion of the FeO6 octahedra occurs quite rapidly for all three samples with a decrease in the next neighbour numbers from six to four. This is ascribed to the Jahn-Teller effect which affects Fe4+ (a d(4) system), that is formed upon delithiation. No distortion is observed for cobalt. Along the delithiation process a simultaneous increase in the edge energy occurs for cobalt and iron in the case of y=0.1 and to a lesser extent for iron than for cobalt for y=0.4. This means that the oxidation of Fe3+ occurs together with the oxidation of the cobalt matrix in the cobalt-rich samples but becomes more difficult for iron-rich samples. In the case of the cobalt-rich samples, the edge-energy for both elements shifts back down at the end of charge, in spite of the continuing oxidation of the cations. This effect is probably related to the appearance of a new lithium-poor phase, that is not formed for y=0.4, and confirms the in-situ X-ray diffraction results published in the first part of this series.
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页码:102 / 110
页数:9
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