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Shock wave kinetics of Fe plus NO based on Fe, O, and N atom measurements

机译:基于Fe,O和N原子测量的Fe加NO的冲击波动力学

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摘要

The reaction of Fe atoms with NO was studied behind incident shock waves in the temperature range of 780 - 1,020 K at pressures between 0.3 and 1.2 bar. Atomic-resonance-absorption spectroscopy (ARAS) was applied for the time-resolved measurement of Fe, N, and O atoms in gas mixtures containing Fe(CO)(5) and NO, highly diluted in argon. The experiments showed a Fe-atom consumption without an associated O- or N-atom formation which can be explained by a recombination of Fe and NO: Fe + NO -->(k1) FeNO. The rate coefficient k(1) was obtained from pseudo-first-order analysis of the measured Fe-absorption profiles to be k(1) = 10(8.99 +/- 0.3) exp(7, 020 +/- 840 K/T) cm(3)/(mol s) with the uncertainty given at the 1 - sigma level. It showed an inverse temperature dependency. Variation of the experimental pressure does not have any effect on the rate coefficient.
机译:研究了Fe原子与NO在780至1,020 K温度范围内在0.3至1.2 bar压力下的入射冲击波之后的反应。原子共振吸收光谱法(ARAS)用于时间分辨测量含有高度稀释于氩气的Fe(CO)(5)和NO的气体混合物中的Fe,N和O原子。实验表明,Fe原子的消耗没有相关的O原子或N原子的形成,这可以通过Fe和NO的复合来解释:Fe + NO->(k1)FeNO。速率系数k(1)是通过对测得的Fe吸收曲线的拟一阶分析得出的,即k(1)= 10(8.99 +/- 0.3)exp(7,020 +/- 840 K / T )cm(3)/(mol s),不确定性在1-sigma级别给出。它显示出反温度依赖性。实验压力的变化对速率系数没有任何影响。

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