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首页> 外文期刊>The Journal of Chemical Physics >Ab initio study of nitrogen and position-specific oxygen kinetic isotope effects in the NO + O-3 reaction
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Ab initio study of nitrogen and position-specific oxygen kinetic isotope effects in the NO + O-3 reaction

机译:从头开始研究NO + O-3反应中氮和特定位置的氧动力学同位素效应

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Ab initio calculations have been carried out to investigate nitrogen (k(15)/k(14)) and position-specific oxygen (k(17)/k(16)O & k(18)/k(16)) kinetic isotope effects (KIEs) for the reaction between NO and O-3 using CCSD(T)/6-31G(d) and CCSD(T)/6-311G(d) derived frequencies in the complete Bigeleisen equations. Isotopic enrichment factors are calculated to be -6.7 parts per thousand, -1.3 parts per thousand, -44.7 parts per thousand, -14.1 parts per thousand, and -0.3 parts per thousand at 298 K for the reactions involving the (NO)-N-15-O-16, (NO)-N-14-O-18, (OOO)-O-18-O-16-O-16, (OOO)-O-16-O-18-O-16, and (OOO)-O-16-O-16-O-18 isotopologues relative to the (NO)-N-14-O-16 and 16O(3) isotopologues, respectively (CCSD(T)/6-311G(d)). Using our oxygen position-specific KIEs, a kinetic model was constructed using Kintecus, which estimates the overall isotopic enrichment factors associated with unreacted O-3 and the oxygen transferred to NO2 to be -19.6 parts per thousand and -22.8 parts per thousand, respectively, (CCSD(T)/6-311G(d)) which tends to be in agreement with previously reported experimental data. While this result may be fortuitous, this agreement suggests that our model is capturing the most important features of the underlying physics of the KIE associated with this reaction (i.e., shifts in zero-point energies). The calculated KIEs will useful in future NOx isotopic modeling studies aimed at understanding the processes responsible for the observed tropospheric isotopic variations of NOx as well as for tropospheric nitrate. Published by AIP Publishing.
机译:从头算进行了研究氮(k(15)/ k(14))和位置特定的氧(k(17)/ k(16)O&k(18)/ k(16))动力学同位素在完整的Bigeleisen方程中,使用CCSD(T)/ 6-31G(d)和CCSD(T)/ 6-311G(d)得出的频率,NO和O-3之间的反应的反应效应(KIEs)。对于涉及(NO)-N的反应,同位素富集因子经计算为-6.7千分,-1.3千分,-44.7千分,-14.1千分和-0.3千分。 -15-O-16,(否)-N-14-O-18,(OOO)-O-18-O-16-O-16,(OOO)-O-16-O-18-O-16 ,和(OOO)-O-16-O-16-O-18同位素,相对于(NO)-N-14-O-16和16O(3)同位素,(CCSD(T)/ 6-311G( d))。使用我们的特定于氧气位置的KIE,使用Kintecus构建了动力学模型,该模型估计与未反应的O-3和转移至NO2的氧气有关的总同位素富集因子分别为-19.6千分和-22.8千分(CCSD(T)/ 6-311G(d)),它倾向于与以前报道的实验数据一致。尽管此结果可能是偶然的,但该协议表明我们的模型正在捕获与该反应相关的KIE的基础物理学的最重要特征(即零点能量的位移)。计算得出的KIEs将在未来的NOx同位素建模研究中有用,该研究旨在了解造成观察到的NOx对流层同位素变化以及对流层硝酸盐变化的过程。由AIP Publishing发布。

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