Volume 179, Issue 1 pp. 205-210
Original Paper

Influence of Preparation on Structure and Properties of La0.67Ca0.33MnO3 Bulk Material

L.W. Zhang

L.W. Zhang

Physics Department, Tsinghua University, Beijing 100084, P.R. China

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Z.J. Chen

Z.J. Chen

Physics Department, Tsinghua University, Beijing 100084, P.R. China

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L.F. Di

L.F. Di

Physics Department, Tsinghua University, Beijing 100084, P.R. China

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B.S. Cao

B.S. Cao

Physics Department, Tsinghua University, Beijing 100084, P.R. China

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M.H. Zhu

M.H. Zhu

Physics Department, Tsinghua University, Beijing 100084, P.R. China

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Y.G. Zhao

Y.G. Zhao

Physics Department, Tsinghua University, Beijing 100084, P.R. China

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Abstract

During growth of La0.67Ca0.33MnO3 in an usual solid state reaction process, the diffusion of La-site metal ions is a rate-limiting factor. In the initial stage of the growth process, La-deficient manganite with rhombohedral structure was easily formed. With the repetition of the grinding– pressing–sintering process, the metal content on the La-site was gradually increased, and the phase was changed from rhombohedral to cubic structure. For slightly La-deficient (La,Ca)1–xMnO3 manganites, the ferromagnetic–paramagnetic (F–P) transition temperature TM is less sensitive to the La-site deficiency, but their electric transport properties are greatly affected. The slightly La-site deficient compound was characterized by double bumps on its resistivity versus temperature (RT) curve, one of which was located at higher temperature very near to its temperature TM. For the La0.67Ca0.33MnO3 single phase, only one resistance peak was observed at TR on its RT curve. For the sample sintered at lower temperatures (<1100 °C) in air TR is much less than TM, and no magnetoresistance (MR) peak was observed within the temperature range of 80 K < T < 300 K. But for the sample sintered at 1200 °C in air TR is well in agreement with TM and its MR is strongly peaked very close to TM. All the bulk samples showed substantial MR in a magnetic field of 0.6 T at low temperatures that increased almost linearly with decreasing temperature.

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