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DETERMINATION OF THE OXYGEN NON-STOICHIOMETRY OF SrFeO_(3-x)

机译:SRFEO_(3-X)的氧非化学计量的测定

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The oxygen non-stoichiometry in SrFeO_(3-x) was determined by coulometric titration in the temperature range, 750 to 1040°C and in the pO_2 range, 10~(-18) to 0.5 atm. At temperatures below 850°C, a two-phase region was observed composed of a mixture of perovskite and an oxygen vacancy ordered phase (Brownmillerite). Equilibrium was very difficult to achieve in this region. Above 850°C, no phase separation was apparent and reproducible data for the non-stoichiometry, x, were obtained both on increasing and decreasing pO_2. A simple, non-interacting point defect model reproduces the data at 1040°C but at lower temperatures, defect interactions must be included to obtain satisfactory agreement. The non-stoichiometry data are compared with previous results including recently reported conductivity data. The comparison shows that the p to n transition observed in the conductivity isotherms occurs at SrFeO_(2.505) at 950°C and SrFeO_(2.508) at 900°C, respectively.
机译:SRFEO_(3-X)中的氧非化学计量法通过在温度范围内的水库滴定,750-1040℃和PO_2范围内,10〜(-18)至0.5atm。在低于850℃的温度下,观察到由钙钛矿的混合物和氧空穴有序相(棕色镁)组成的两相区域。在该地区均衡均衡均难以实现。在850℃以上,在增加和减少的PO_2上,没有相分离是显而易见的,并且为非化学计量X进行可再现数据。简单的非交互点缺陷模型在1040°C下再现数据,但在较低的温度下,必须包括缺陷相互作用以获得令人满意的协议。将非化学计量数据与先前的结果进行比较,包括最近报告的电导数据。比较表明,在电导率等温物中观察到的P到N转变在950℃和SRFeO_(2.508)的SRFEO_(2.505)处分别在900℃下发生。

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