Taatjes Craig A
Combustion Research Facility, Mail Stop 9055, Sandia National Laboratories, Livermore, California 94551-0969, USA.
J Phys Chem A. 2006 Apr 6;110(13):4299-312. doi: 10.1021/jp056997f.
The reactions of alkyl radicals (R) with molecular oxygen (O(2)) are critical components in chemical models of tropospheric chemistry, hydrocarbon flames, and autoignition phenomena. The fundamental kinetics of the R + O(2) reactions is governed by a rich interplay of elementary physical chemistry processes. At low temperatures and moderate pressures, the reactions form stabilized alkylperoxy radicals (RO(2)), which are key chain carriers in the atmospheric oxidation of hydrocarbons. At higher temperatures, thermal dissociation of the alkylperoxy radicals becomes more rapid and the formation of hydroperoxyl radicals (HO(2)) and the conjugate alkenes begins to dominate the reaction. Internal isomerization of the RO(2) radicals to produce hydroperoxyalkyl radicals, often denoted by QOOH, leads to the production of OH and cyclic ether products. More crucially for combustion chemistry, reactions of the ephemeral QOOH species are also thought to be the key to chain branching in autoignition chemistry. Over the past decade, the understanding of these important reactions has changed greatly. A recognition, arising from classical kinetics experiments but firmly established by recent high-level theoretical studies, that HO(2) elimination occurs directly from an alkylperoxy radical without intervening isomerization has helped resolve tenacious controversies regarding HO(2) formation in these reactions. Second, the importance of including formally direct chemical activation pathways, especially for the formation of products but also for the formation of the QOOH species, in kinetic modeling of R + O(2) chemistry has been demonstrated. In addition, it appears that the crucial rate coefficient for the isomerization of RO(2) radicals to QOOH may be significantly larger than previously thought. These reinterpretations of this class of reactions have been supported by comparison of detailed theoretical calculations to new experimental results that monitor the formation of products of hydrocarbon radical oxidation following a pulsed-photolytic initiation. In this article, these recent experiments are discussed and their contributions to improving general models of alkyl + O(2) reactions are highlighted. Finally, several prospects are discussed for extending the experimental investigations to the pivotal questions of QOOH radical chemistry.
烷基自由基(R)与分子氧(O₂)的反应是对流层化学、碳氢化合物火焰和自燃现象化学模型中的关键组成部分。R + O₂反应的基本动力学受基本物理化学过程丰富的相互作用支配。在低温和中等压力下,反应形成稳定的烷基过氧自由基(RO₂),它们是碳氢化合物大气氧化中的关键链载体。在较高温度下,烷基过氧自由基的热解离变得更快,氢过氧自由基(HO₂)和共轭烯烃的形成开始主导反应。RO₂自由基的内部异构化产生氢过氧烷基自由基,通常用QOOH表示,导致OH和环醚产物的生成。对于燃烧化学更关键的是,短暂的QOOH物种的反应也被认为是自燃化学中链分支的关键。在过去十年中,对这些重要反应的理解发生了很大变化。经典动力学实验得出但最近的高水平理论研究坚定确立的一种认识是,HO₂的消除直接从烷基过氧自由基发生,无需中间异构化,这有助于解决关于这些反应中HO₂形成的顽固争议。其次,在R + O₂化学的动力学建模中,纳入形式上直接的化学活化途径的重要性已得到证明,特别是对于产物的形成,但也对于QOOH物种的形成。此外,RO₂自由基异构化为QOOH的关键速率系数似乎可能比以前认为的要大得多。通过将详细的理论计算与监测脉冲光解引发后碳氢化合物自由基氧化产物形成的新实验结果进行比较,支持了对这类反应的这些重新解释。在本文中,讨论了这些最近的实验,并强调了它们对改进烷基 + O₂反应通用模型的贡献。最后讨论了将实验研究扩展到QOOH自由基化学关键问题的几个前景。