Structural and Electrochemical Study of a New Crystalline Hydrated Iron(III) Phosphate FePO4•H2O Obtained from LiFePO4(OH) by Ion Exchange

被引:55
作者
Marx, Nicolas [1 ]
Croguennec, Laurence [1 ]
Carlier, Dany [1 ]
Bourgeois, Lydie [2 ]
Kubiak, Pierre [1 ]
Le Cras, Frederic [3 ]
Delmas, Claude [1 ]
机构
[1] Univ Bordeaux, ICMCB, CNRS, IPB,ENSCBP, F-33608 Pessac, France
[2] Univ Bordeaux, ISM, F-33405 Talence, France
[3] LITEN, CEA, F-38054 Grenoble, France
关键词
LITHIUM VANADIUM FLUOROPHOSPHATE; POSITIVE-ELECTRODE MATERIALS; INSERTION PROPERTIES; NEUTRON-DIFFRACTION; IRON PHOSPHATES; SOLID-SOLUTION; TEMPERATURE; LIXFEPO4; INTERCALATION; MICROSCOPY;
D O I
10.1021/cm903370z
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
A new iron(III) phosphate FePO4 center dot H2O, isostructural to already reported VPO4 center dot H2O and MnPO4 center dot H2O phases, was obtained from tavorite LiFePO4(OH) through a Li+/H+ exchange. The composition of this new phase was confirmed by different chemical analyses. The ion-exchange reaction was shown to be topotactic; indeed the structures of LiFePO4OH and FePO4 center dot H2O are very similar and both are characterized by chains of FeO6 octahedia. Interconnected through PO4 tetrahedra, such as the resulting frameworks enclose different types of tunnels. A neutron diffraction study has allowed the localization of hydrogens in the FePO4 center dot H2O structure, revealing that the two hydrogen atoms are linked to the oxygen atoms shared by two adjacent FeO6 octahedra. The presence of these "H2O-like" groups inserted along the FeO6 chains leads to a considerable distortion of the FeO6 octahedra. The nature of the -OH and -OH2 groups in the LiFePO4OH and FePO4 center dot H2O, respectively, was confirmed by vibrational spectroscopies. Lithium interacalation was shown to occur in FePO4 center dot H2O through the reduction of Fe3+ to Fe2+ at an average voltage of similar to 2.8 V (vs Li+/Li) with a good cyclability.
引用
收藏
页码:1854 / 1861
页数:8
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