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Stability of Fe-Cr alloy interconnects under CH_4-H_2O atmosphere for SOFCs

机译:CH_4-H_2O气氛下Fe-Cr合金互连对于SOFC的稳定性

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The chemical stability of Fe-Cr alloys (ZMG232 and SUS430) was examined under humidified CH_4 gases at 1073 K to simulate the real anode atmosphere in SOFC operation. Surface microstructure change and oxide scale layer formation were observed on the oxidized Fe-Cr alloy surfaces. The main reaction products were Mn-Cr-(Fe) spinels for both alloys. Secondary ion mass spectrometry (SIMS) was applied to measure the elemental distribution of minor and major elements around the oxide scale/alloy interface. A high concentration of Mn on the oxide scale surface suggested the fast diffusion of Mn in the oxide scale to form the spinels. Annealing in CH_4-H_2O made the oxide scale thicker with duration time on the alloy surface. The parabolic growth rates (k_p) of oxide scale layer were evaluated from the thickness of oxide scales by secondary ion mass spectrometry (SIMS) depth profiles, which were calculated to the following: k_p = 6.25 x 10~(-6)μm~2/s for SUS430 and k_p = 4.42 x 10~(-6)μm~2/s for ZMG232. The electrical conductivity of oxidized alloys showed the semi-conductor temperature dependence for both alloys. The electrical conductivity of oxidized ZMG232 alloy was higher than that of oxidized SUS430.
机译:在1073 K的湿CH_4气体下检查了Fe-Cr合金(ZMG232和SUS430)的化学稳定性,以模拟SOFC操作中的实际阳极气氛。在氧化的Fe-Cr合金表面观察到表面微观结构变化和氧化皮层形成。两种合金的主要反应产物是Mn-Cr-(Fe)尖晶石。二次离子质谱(SIMS)用于测量氧化物和合金界面周围次要和主要元素的元素分布。在氧化皮表面上高浓度的Mn表明Mn在氧化皮中快速扩散以形成尖晶石。 CH_4-H_2O中的退火会使氧化皮随着合金表面上的持续时间变厚。通过二次离子质谱(SIMS)深度分布图根据氧化皮的厚度评估氧化皮层的抛物线生长速率(k_p),其计算公式如下:k_p = 6.25 x 10〜(-6)μm〜2 SUS430为/ s,ZMG232为k_p = 4.42 x 10〜(-6)μm〜2 / s。氧化合金的电导率表明两种合金的半导体温度依赖性。氧化的ZMG232合金的电导率高于氧化的SUS430。

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