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Formation of LaFeO3 and thermal decomposition reactions in lanthanum(III) oxalate-iron(II) oxalate crystalline mixture

机译:草酸镧(III)-草酸铁(II)结晶混合物中LaFeO3的形成和热分解反应

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摘要

Thermal processes involved during the decomposition course of La-2(C2O4)(3)center dot 10H(2)O-FeC2O4 center dot 2H(2)O (1:2 mole ratio) mixture up to 750 degrees C, in an atmosphere of air, were monitored by thermogravimetry and differential thermal analysis. X-ray diffraction and Mossbauer spectroscopy were used to characterize the intermediates and the final product. The results showed that a microcrystalline or possibly amorphous iron(III) oxide with a paramagnetic nature was appeared in the early stages of decomposition at 250 degrees C. By increasing the temperature, a well crystalline hematite with ferromagnetic properties was obtained. XRD pattern of the mixture calcined at 1100 degrees C shows the formation of LaFeO3 single phase in consistent with the hyperfine magnetic splitting (one sextet of lines) characteristic of LaFeO3 obtained in the Mossbauer spectra of the mixture calcined at the same temperature.
机译:La-2(C2O4)(3)中心点10H(2)O-FeC2O4中心点2H(2)O(1:2摩尔比)的混合物在大气中的分解过程中涉及的热过程通过热重分析和差热分析监测空气的质量。 X射线衍射和Mossbauer光谱用于表征中间体和最终产物。结果表明,在250℃分解的早期出现了具有顺磁性的微晶或可能具有非晶态的铁(III)氧化物。通过提高温度,可获得具有铁磁性能的良好结晶的赤铁矿。在1100摄氏度下煅烧的混合物的XRD图谱显示,形成了LaFeO3单相,这与在相同温度下煅烧的混合物的Mossbauer光谱中获得的LaFeO3的超细磁裂特征(一条线的六边形)一致。

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