Local structure of Fe in Fe-doped misfit-layered calcium cobaltite: An X-ray absorption spectroscopy study
Local structure of Fe in Fe-doped misfit-layered calcium cobaltite: An X-ray absorption spectroscopy study
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DOI:
10.1016/j.jssc.2013.05.038
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发表时间:
2013-08
影响因子:
3.3
通讯作者:
N. Prasoetsopha;S. Pinitsoontorn;Atipong Bootchanont;P. Kidkhunthod;P. Srepusharawoot;T. Kamwanna;V. Amornkitbamrung;K. Kurosaki;S. Yamanaka
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文献类型:
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作者:
N. Prasoetsopha;S. Pinitsoontorn;Atipong Bootchanont;P. Kidkhunthod;P. Srepusharawoot;T. Kamwanna;V. Amornkitbamrung;K. Kurosaki;S. Yamanaka
Polycrystalline Ca3Co4−xFexO9+δceramics (x=0, 0.01, 0.03, 0.05) were fabricated using a simple thermal hydro-decomposition method and a spark plasma sintering technique. Thermoelectric property measurements showed that increasing Fe concentration resulted in a decrease in electrical resistivity, thermopower and thermal conductivity, leading to an improvement in the dimensionless figure-of-merit, >35% forx=0.05 at 1073 K. An X-ray absorption spectroscopy technique was used to investigate the local structure of Fe ions in the Ca3Co4−xFexO9+δstructure for the first time. By fitting data from the extended X-ray absorption fine structure (EXAFS) spectra and analyzing the X-ray absorption near-edge structure (XANES) spectra incorporated with first principle simulation, it was shown that Fe was substituted for Co in the the Ca2CoO3(rocksalt, RS) layer rather than in the CoO2layer. Variation in the thermoelectric properties as a function of Fe concentration was attributed to charge transfer between the CoO2and the RS layers. The origin of the preferential Fe substitution site was investigated considering the ionic radii of Co and Fe and the total energy of the system.