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IONIC TRANSPORT IN SrCo_0.855Ti_0.15O_3-δ CERAMICS AT HIGH OXYGEN PRESSURES

机译:高压下SrCo_0.855Ti_0.15O_3-δ陶瓷中的离子迁移

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摘要

Oxygen permeation through dense ceramic membranes of the SrCo_0.85Ti_0.15O_3-δ cubic perovskite solid solution was studied in the range of the membrane feed-side oxygen partial pressures (p_2) 0.2l to l00 atm at temperatures of 850--l040 K. The dependence of the oxygen fluxes on membrane thickness suggests that bulk ionic conductivity is the permeation- determining factor at high oxygen pressures (p2 > to l atm). Increasing the oxygen pressure up to 80--l00 atm was found to result in a drastic increase of the permeation flux, accompanied by a partial decomposition of the cubic perovskite phase of Sroo_0.85Ti_0.15O_3-δ, forming two isostructural perovskite- type phases. No phase changes were observed after testing ceramics in the oxygen pressure range of l-60 atm. The high oxygen permeation fluxes obtained demonstrate the applicability of SrCo_0.85Ti_o.5O3-δ membranes at high oxygen pressures.
机译:研究了SrCo_0.85Ti_0.15O_3-δ钙钛矿固溶体在致密陶瓷膜中的透氧性,在膜进料侧氧分压(p_2)在850--040 K的条件下为0.2l至100 atm的氧气。氧气流量对膜厚度的依赖性表明,在高氧气压力下(p2>到l atm),体离子传导率是渗透的决定因素。发现将氧气压力提高到80--100 atm会导致渗透通量急剧增加,同时Sroo_0.85Ti_0.15O_3-δ的立方钙钛矿相部分分解,从而形成两个等结构的钙钛矿型相。在1-60 atm的氧气压力范围内测试陶瓷后,未观察到相变。获得的高氧气渗透通量证明了SrCo_0.85Ti_0.5O3-δ膜在高氧气压力下的适用性。

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