2008
DOI: 10.1016/j.ssi.2007.10.015
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The hydrothermal synthesis and characterization of olivines and related compounds for electrochemical applications

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Cited by 283 publications
(244 citation statements)
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“…As researched by J.J. Chen's group [12], it is indicated that around 0.14 zinc was substituted for iron, giving LiFe 0.86 Zn 0.14 PO 4 when 20% zinc was in the reaction medium. A Rietveld analysis also indicated zinc on the iron site and not on the lithium site.…”
Section: Sample Preparationmentioning
confidence: 95%
See 1 more Smart Citation
“…As researched by J.J. Chen's group [12], it is indicated that around 0.14 zinc was substituted for iron, giving LiFe 0.86 Zn 0.14 PO 4 when 20% zinc was in the reaction medium. A Rietveld analysis also indicated zinc on the iron site and not on the lithium site.…”
Section: Sample Preparationmentioning
confidence: 95%
“…It is well known that the ionic diffusion and electron conductivities can be remarkably improved by doping appropriate functional material to LFP, and the ameliorated microstructure is achieved which shortens the transmission distance of lithium ions and prevents the collapse of the crystal lattice [3][4][5][6][7]. And to prepare LiFePO 4 at a low cost and efficiently, the hydrothermal synthesis is well studied by many researchers [8][9][10][11][12][13][14][15][16]. Their results demonstrate that the particle size and conductivity of LFP can be controlled by appropriate additive, such as CTAB, ascorbic acid and carbon nanotube under hydrothermal conditions and the appropriate temperature is necessary.…”
Section: Introductionmentioning
confidence: 99%
“…Nano-LiMnPO 4 has been prepared by various wet chemical methods such as hydrothermal [21][22][23], thermal decomposition [20,24], solvothermal [17,25], polyol methods [15], etc. Wet chemical methods are preferable as they allow perfect mixing of precursors, better homogeneity and more regular morphology to obtain nanosized particles.…”
Section: Introductionmentioning
confidence: 99%
“…Crystallographic studies have shown in stoichiometric LiFePO 4 , that Li occupies fully the octahedral M1, 4a site and Fe occupies the octahedral M2, 4c site [2][3][4][5] . Cation disorder between the M1, M2 sites is an interesting research area in petrology 6 because it may give insight into the thermal history of the earth's upper mantle where olivine minerals are abundant.…”
Section: Introductionmentioning
confidence: 99%