{"title":"Thermoelectric properties and local electronic structure of rare earth-doped Ca3Co2O6","authors":"N. Nong, M. Ohtaki","doi":"10.1109/ICT.2006.331270","DOIUrl":null,"url":null,"abstract":"Thermoelectric properties of a series of rare earth metal-doped polycrystalline samples of (Ca<sub>1-x</sub>R<sub>x</sub>)<sub>3</sub>Co <sub>2</sub>O<sub>6</sub> with R = Gd, Tb, Dy and Ho (x = 0 - 0.1) were investigated in the temperature range from 300 K to 1300 K. In a high temperature region above 900 K, a partial rare earth substitution with R <sup>3+</sup> for Ca<sup>2+</sup> resulted in appreciable increase in the Seebeck coefficient (S). However, the S value decreased abruptly at low temperatures, and turned to negative values for the Gd- and Tb-doped samples at temperatures below 400 K. With decreasing ionic radii of rare earth elements (Gd<sup>3+</sup> > Tb<sup>3+</sup> > Dy<sup>3+</sup> > Ho<sup>3+</sup>), the S values increased, while the thermal conductivity (kappa) decreased particularly at temperatures above 700 K. Contrastingly, the influence of rare earth metal substitution on the electrical resistivity (rho) was small; in high temperature region the rho values increased only slightly with decreasing ionic radii of rare earth metals. High-temperature thermoelectric figure-of-merit (Z) of the samples was thereby improved by the late rare-earth metal substitution for Ca<sup>2+</sup>, particularly for those with Ho<sup>3+</sup>. A maximum Z value of the Ho-doped sample for x = 0.03 was 1.83 times 10<sup>-4</sup> K<sup>-1 </sup> at 1100 K as compared with 0.37 times 10<sup>-4</sup> K<sup>-1 </sup> for non-doped sample. The electronic structure of the samples was also investigated by x-ray photoemission spectroscopy (XPS) technique. The charge-transfer satellite structure of Co 2p core-level spectra was observed for the Gd-and Tb-doped samples, while the satellite is negligible for the other samples","PeriodicalId":346555,"journal":{"name":"2006 25th International Conference on Thermoelectrics","volume":"1 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2006-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"4","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"2006 25th International Conference on Thermoelectrics","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/ICT.2006.331270","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 4
Abstract
Thermoelectric properties of a series of rare earth metal-doped polycrystalline samples of (Ca1-xRx)3Co 2O6 with R = Gd, Tb, Dy and Ho (x = 0 - 0.1) were investigated in the temperature range from 300 K to 1300 K. In a high temperature region above 900 K, a partial rare earth substitution with R 3+ for Ca2+ resulted in appreciable increase in the Seebeck coefficient (S). However, the S value decreased abruptly at low temperatures, and turned to negative values for the Gd- and Tb-doped samples at temperatures below 400 K. With decreasing ionic radii of rare earth elements (Gd3+ > Tb3+ > Dy3+ > Ho3+), the S values increased, while the thermal conductivity (kappa) decreased particularly at temperatures above 700 K. Contrastingly, the influence of rare earth metal substitution on the electrical resistivity (rho) was small; in high temperature region the rho values increased only slightly with decreasing ionic radii of rare earth metals. High-temperature thermoelectric figure-of-merit (Z) of the samples was thereby improved by the late rare-earth metal substitution for Ca2+, particularly for those with Ho3+. A maximum Z value of the Ho-doped sample for x = 0.03 was 1.83 times 10-4 K-1 at 1100 K as compared with 0.37 times 10-4 K-1 for non-doped sample. The electronic structure of the samples was also investigated by x-ray photoemission spectroscopy (XPS) technique. The charge-transfer satellite structure of Co 2p core-level spectra was observed for the Gd-and Tb-doped samples, while the satellite is negligible for the other samples