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Oxygen permeation in Co-containing perovskites: surface oxygen exchange vs bulk oxygen diffusion

机译:含钴钙钛矿中的氧渗透:表面氧交换与大量氧扩散

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The oxygen permeation fluxes of Co-containing ceramic membranes with perovskite structure were measured by Gas Chromatography as functions of oxygen chemical potential gradient, temperature and thickness. A power index n>0 is obtained when J_(o2) vs Po_2'~n-Po_2"~n is plotted as a straight-line in conditions of 950 deg C >= T >= 810 deg C, 0.21 atm >= Po_2" >= 3x10~(-3) atm and membrane thickness 2.5 mm >= L >= 0.50mm. The results indicate an overall permeation process controlled by both surface oxygen exchange and bulk oxygen diffusion. The mechanism of the surface exchange is discussed and an analytic expression that agrees well with the experimental results is obtained. The determination of oxygen-vacancy conductivity across a perovskite membrane by measurement of oxygen permeation where ther is no reactant on the reducing side can be misleading.
机译:通过气相色谱法测量了含钙钛矿结构的含钴陶瓷膜的氧渗透通量,该通量是氧化学势梯度,温度和厚度的函数。当在950摄氏度> = T> = 810摄氏度,0.21大气压> = Po_2的条件下将J_(o2)与Po_2'〜n-Po_2“〜n绘制为直线时,获得的功率指数n> 0 “> = 3x10〜(-3)atm,膜厚度2.5 mm> = L> = 0.50mm。结果表明,整个渗透过程受表面氧交换和大量氧扩散的控制。讨论了表面交换的机理,并获得了与实验结果吻合的解析表达式。在还原面上没有反应物的情况下,通过测量氧渗透率来确定钙钛矿膜两端的氧空位电导率可能会产生误导。

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