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EFFECT OF SURFACE STATES ON OXYGEN PERMEABILITY OF PEROVSKITE-TYPE OXIDE DENSE DISK

机译:表面状态对钙钛矿型氧化物致密盘氧气渗透性的影响

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摘要

In order to collect information about the contribution of the surface reaction and bulk diffusion rates in oxygen permeation through mixed ionic-electronic conductive perovskites, La_(0.1)Sr_(0.9)Co_(0.9)Fe_(0.1)O_(3-δ) dense disks with different surface areas (roughness) and thicknesses were prepared and their oxygen permeability was measured. The oxygen permeation rate through the 1 mm-thick membrane was little dependent on the surface area below 700°C, indicating that oxygen permeation is almost exclusively controlled by the diffusion of oxide ions in the membrane. Above 750°C, on the other hand, the oxygen permeation rate increased with increasing surface area and therefore the rates of both diffusion and surface reactions contributed to the oxygen permeation flux; the contribution of the surface reaction became more significant with increasing temperature. The effect of surface area on the oxygen permeation flux through thinner membrane was more prominent than that through thicker membrane.
机译:为了通过混合离子电子导电钙钛矿,La_(0.1)SR_(0.9)CO_(0.1)o_(3-Δ)致密的La_(0.1)SR_(0.9)CO_(0.1)致密的氧渗透在氧渗透中的氧渗透中的氧渗透中的氧气渗透中的贡献制备具有不同表面积(粗糙度)和厚度的磁盘,并测量它们的透氧性。通过1mm厚膜的氧渗透速率几乎依赖于700℃以下的表面积,表明氧渗透几乎完全由膜中的氧化物离子的扩散来控制。另一方面,在750℃以上,氧气渗透率随着表面积的增加而增加,因此扩散和表面反应的速率导致氧渗透通量有助于;随着温度的增加,表面反应的贡献变得更加显着。表面积对通过较薄膜氧渗透通量的影响比通过较厚的膜更突出。

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