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首页> 外文期刊>International Journal of Quantum Chemistry >ELECTRICAL CONDUCTIVITY AND CHEMICAL DIFFUSION COEFFICIENT OF STRONTIUM-DOPED LANTHANUM MANGANITES
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ELECTRICAL CONDUCTIVITY AND CHEMICAL DIFFUSION COEFFICIENT OF STRONTIUM-DOPED LANTHANUM MANGANITES

机译:掺锶镧锰矿的电导率和化学扩散系数

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摘要

Electrical conductivity and chemical diffusion coefficient of Sr-doped lanthanum manganites, La1-xSrxMnO3+/-delta (x = 0.05-0.20), were measured by the de four-probe technique and relaxation type experiments where a sudden change of oxygen chemical potential was imposed on the pre-equilibrated sample and the change of electrical conductivity was followed as a function of elapsed time, A defect model is proposed to elucidate the oxygen partial pressure dependence of the measured conductivity and the reported oxygen nonstoichiometry. The transient conductivity behavior after an abrupt change of oxygen partial pressure was successfully described by a diffusion model with consideration of partial control by surface reaction. The determined chemical diffusion coefficients, of the order of 10(-5) to 10(-4) cm(2) s(-1) at 1000 degrees C, increased with decreased oxygen partial pressure due to the thermodynamic enhancement effect. Using the enhancement factor estimated by combination of the proposed defect model and the ambipolar diffusion theory, the oxygen vacancy diffusion coefficients were derived. High vacancy diffusivity comparable to that of Fe- or Co-based perovskites predicts fast oxide ion diffusion under conditions where the manganites show oxygen deficient type nonstoichiometry. (C) 1996 Academic Press, Inc. [References: 36]
机译:通过四探针技术和弛豫型实验测量了掺Sr的镧锰矿的电导率和化学扩散系数La1-xSrxMnO3 +/-δ(x = 0.05-0.20)在预先平衡的样品上,遵循随时间变化的电导率变化,提出了一种缺陷模型,以阐明所测得的电导率与氧分压的关系以及所报道的氧非化学计量。考虑到通过表面反应进行部分控制,通过扩散模型成功地描述了氧分压突然变化后的瞬态电导行为。所确定的化学扩散系数在1000摄氏度下为10(-5)到10(-4)cm(2)s(-1),由于热力学增强效应而随着氧分压的降低而增加。利用提出的缺陷模型和双极性扩散理论相结合的估计增强因子,推导了氧空位扩散系数。与基于铁或钴的钙钛矿相比,高的空位扩散率可预测在锰矿显示出缺氧型非化学计量的条件下,氧化物离子会快速扩散。 (C)1996 Academic Press,Inc. [参考:36]

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