School of Chemistry, University of Leeds, Leeds LS2 9JT, U.K.
National Centre for Atmospheric Science (NCAS), University of Leeds, Leeds LS2 9JT, U.K.
J Phys Chem A. 2021 Dec 9;125(48):10439-10450. doi: 10.1021/acs.jpca.1c08104. Epub 2021 Nov 24.
Emissions of amines and amides to the atmosphere are significant from both anthropogenic and natural sources, and amides can be formed as secondary pollutants. Relatively little kinetic data exist on overall rate coefficients with OH, the most important tropospheric oxidant, and even less on site-specific data which control the product distribution. Structure-activity relationships (SARs) can be used to estimate both quantities. Rate coefficients for the reaction of OH with -butylamine (), -methyl-1,3-propanediamine (), and -methylformamide () have been measured using laser flash photolysis coupled with laser-induced fluorescence. Proton-transfer-reaction mass spectrometry (PTR-MS) has been used to ensure the reliable introduction of these low-vapor pressure N-containing compounds and to give qualitative information on products. Supporting ab initio calculations are presented for the -butylamine system. The following rate coefficients have been determined: = (1.66 ± 0.20) × 10 cm molecule s, () = 1.65 × 10 (/300) cm molecule s, = (7.09 ± 0.22) × 10 cm molecule s, and = (1.03 ± 0.23) × 10 cm molecule s. For OH + -butylamine, ab initio calculations predict that the fraction of N-H abstraction is 0.87. The dominance of this channel was qualitatively confirmed using end-product analysis. The reaction of OH with -methyl-1,3-propanediamine also had a negative temperature dependence, but the reduction in the rate coefficient was complicated by reagent loss. The measured rate coefficient for reaction 3 is in good agreement with a recent relative rate study. The results of this work and the literature data are compared with the recent SAR estimates for the reaction of OH with reduced nitrogen compounds. Although the SARs reproduce the overall rate coefficients for reactions, site-specific agreement with this work and other literature studies is less strong.
胺和酰胺向大气中的排放来自人为和自然来源,并且酰胺可以作为二次污染物形成。与最重要的大气氧化剂 OH 反应的整体速率系数的动力学数据相对较少,而控制产物分布的特定地点的数据则更少。结构-活性关系 (SAR) 可用于估计这两个数量。使用激光闪光光解结合激光诱导荧光测量了 OH 与 -丁胺 (), -甲基-1,3-丙二胺 () 和 -甲基甲酰胺 () 的反应速率系数。质子转移反应质谱 (PTR-MS) 已被用于可靠地引入这些低蒸气压含氮化合物,并提供有关产物的定性信息。为 -丁胺体系提供了支持的从头计算。已确定以下速率系数:= (1.66 ± 0.20) × 10 cm molecule s, () = 1.65 × 10 (/300) cm molecule s, = (7.09 ± 0.22) × 10 cm molecule s 和 = (1.03 ± 0.23) × 10 cm molecule s。对于 OH + -丁胺,从头计算预测 N-H 抽取的分数为 0.87。使用最终产物分析定性证实了该通道的主导地位。OH 与 -甲基-1,3-丙二胺的反应也具有负温度依赖性,但由于试剂损失,速率系数的降低变得复杂。测量的反应 3 的速率系数与最近的相对速率研究很好地吻合。这项工作和文献数据的结果与最近 OH 与还原氮化合物反应的 SAR 估计值进行了比较。尽管 SAR 再现了反应的整体速率系数,但与这项工作和其他文献研究的特定地点的一致性则较弱。