Université de Toulouse, UPS Institut Carnot CIRIMAT, 118 Route de Narbonne, 31062 Toulouse Cedex 9, France.
Inorg Chem. 2009 Jul 6;48(13):6065-71. doi: 10.1021/ic900437x.
In this work, different CuFe(1-x)Cr(x)O(2) compositions with 0 <or= x <or= 1 were prepared by a standard solid-state reaction. These oxides crystallize with the delafossite structure. The phase stability and thermal behavior of the complete CuFe(1-x)Cr(x)O(2) solid solution was studied by thermogravimetric analysis and high-temperature X-ray diffraction experiments under an air atmosphere up to 1000 degrees C. For x = 0, CuFeO(2) is oxidized into the spinel (CuFe(2)O(4)) and copper monoxide (CuO) phases, whereas for x = 1, CuCrO(2) is thermally stable. For all of the intermediate compositions (0 < x < 1), complex oxidation, reduction, and phase transitions between delafossite and spinel have been observed. chromium tends to stabilize the stoichiometric delafossite phase, while iron favors the delafossite-to-spinel phase transition.
在这项工作中,通过标准的固相反应制备了不同组成的 CuFe(1-x)Cr(x)O(2)(0 <= x <= 1)。这些氧化物结晶为德劳方石结构。通过热重分析和高温 X 射线衍射实验,在空气气氛下研究了完整的 CuFe(1-x)Cr(x)O(2 固溶体的相稳定性和热行为,温度高达 1000 摄氏度。对于 x = 0,CuFeO(2) 被氧化成尖晶石(CuFe(2)O(4))和氧化亚铜(CuO)相,而对于 x = 1,CuCrO(2) 是热稳定的。对于所有的中间组成(0 < x < 1),观察到了德劳方石和尖晶石之间的复杂氧化、还原和相变。铬倾向于稳定化学计量的德劳方石相,而铁有利于德劳方石到尖晶石的相变。