稀土掺杂Ca3Co2O6的热电性质和局域电子结构

N. Nong, M. Ohtaki
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引用次数: 4

摘要

研究了R = Gd, Tb, Dy和Ho (x = 0 ~ 0.1)的稀土金属掺杂(Ca1-xRx) 3co2o6多晶样品在300 ~ 1300 K温度范围内的热电性能。在900 K以上的高温区域,稀土被R 3+部分取代Ca2+导致塞贝克系数(S)明显增加,但在低温下,S值突然下降,在400 K以下的温度下,Gd和tb掺杂样品的S值变为负值。随着稀土元素离子半径的减小(Gd3+ > Tb3+ > Dy3+ > Ho3+), S值增大,导热系数(kappa)在700 K以上温度下下降尤为明显。相反,稀土金属取代对电阻率(rho)的影响较小;在高温区,rho值随着稀土金属离子半径的减小而略有增加。通过后期稀土金属取代Ca2+,特别是Ho3+,提高了样品的高温热电性能(Z)。在1100 K时,当x = 0.03时,ho掺杂样品的最大Z值为1.83倍10-4 K-1,而未掺杂样品的Z值为0.37倍10-4 K-1。并用x射线光电发射光谱(XPS)技术研究了样品的电子结构。在gd和tb掺杂样品中观察到Co 2p核能级光谱的电荷转移卫星结构,而在其他样品中卫星可以忽略不计
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Thermoelectric properties and local electronic structure of rare earth-doped Ca3Co2O6
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
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