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MASS TRANSPORT IN OXIDES FOR MEMBRANE REFORMING OF METHANE

机译:氧化物在甲烷膜重整中的传质

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Oxygen tracer diffusion (D~*) and surface exchange (k) have been measured, using isotopic exchange and depth profiling by Secondary Ion Mass Spectrometry (SIMS), in La_(1-x)Sr_xFe_(1-y)Cr_yO_(3-δ) (x=0.2, 0.4, 0.6, y= 0.2) as a function of temperature (700-1000℃) in dry oxygen and in a water vapour/forming gas mixture. The apparent activation energies for D~* in dry oxygen are 1.56 eV and 1.21 eV for x=0.4 and 0.6 respectively, and 1.24 eV and 1.65 eV for x=0.2 and x = 0.4 respectively, in water vapour/forming gas. D~* was found to increase with increasing temperature and decreasing oxygen activity, which is consistent with diffusion being proportional to the concentration of oxygen vacancies. Fast surface kinetics was observed under all conditions, which indicates a similar rate of exchange for oxygen from a H_2O molecule and an O_2 molecule at atmospheric pressure.
机译:在La_(1-x)Sr_xFe_(1-y)Cr_yO_(3-)中使用同位素交换和深度分布通过二次离子质谱(SIMS)测量了氧示踪剂扩散(D〜*)和表面交换(k)在干燥氧气和水蒸气/形成气体混合物中,δ(x = 0.2,0.4,0.6,y = 0.2)与温度(700-1000℃)的关系。在水蒸气/生成气体中,D_ *在干氧中的表观活化能分别为x = 0.4和0.6时分别为1.56 eV和1.21 eV,x = 0.2和x = 0.4时分别为1.24 eV和1.65 eV。发现D〜*随温度升高和氧活度降低而增加,这与扩散与氧空位浓度成正比是一致的。在所有条件下均观察到快速的表面动力学,这表明在大气压下来自H_2O分子和O_2分子的氧交换速率相似。

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