Färber Michelle, Vereecken Luc, Fuchs Hendrik, Gkatzelis Georgios I, Rohrer Franz, Wedel Sergej, Wahner Andreas, Novelli Anna
Institute for Energy and Climate Research, IEK-8: Troposphere, Forschungszentrum Jülich GmbH, 52428 Jülich, Germany.
Department of Physics, University of Cologne, 50932 Cologne, Germany.
Phys Chem Chem Phys. 2024 Feb 7;26(6):5183-5194. doi: 10.1039/d3cp04163h.
The formation of peroxynitrates (RONO) from the reaction of peroxy radicals (RO) and nitrogen dioxide (NO) and their subsequent redissociation are typically not included in chemical mechanisms. This is often done to save computational time as the assumption is that the equilibrium is strongly towards the RO + NO reaction for most conditions. Exceptions are the reactions of the methyl peroxy radical due to its abundance in the atmosphere and of acyl-RO radicals due to the long lifetime of peroxyacyl nitrates RONO (PANs). In this study, the nighttime oxidation of -2-butene and -2-hexene in the presence of NO is investigated in the atmospheric simulation chamber SAPHIR, Forschungszentrum Jülich, Germany, at atmospherically-relevant conditions at different temperatures (≈276 K, ≈293 K, ≈305 K). Measured concentrations of peroxy and hydroperoxy radicals as well as other trace gases (ozone, NO, volatile organic compounds) are compared to state-of-the-art zero-dimensional box model calculations. Good model-measurement agreement can only be achieved when reversible RO + NO reactions are included for all RO species using literature values available from the latest SAR by [Jenkin , , 2019, , 7691]. The good agreement observed gives confidence that the SAR, derived originally for aliphatic RO, can be applied to a large range of substituted RO radicals, simplifying generalised implementation in chemical models. RONO concentrations from non-acyl RO radicals of up to 2 × 10 cm are predicted at 276 K, impacting effectively the kinetics of RO radicals. Under these conditions, peroxy radicals are slowly regenerated downwind of the pollution source and may be lost in the atmosphere through deposition of RONO. Based on this study, 60% of RO radicals would be stored as RONO at a temperature of 10 °C and in the presence of a few ppbv of NO. The fraction increases further at colder temperatures and/or higher NO mixing ratios. This does not only affect the expected concentrations of RO radicals but, as the peroxynitrates can react with OH radicals or photolyse, they could comprise a net sink for RO radicals as well as increase the production of NO (= NO + NO) in different locations depending on their lifetime. Omitting this chemistry from the kinetic model can lead to misinterpreted product formation and may prevent reconciling observations and model predictions.
过氧自由基(RO)与二氧化氮(NO)反应生成过氧硝酸盐(RONO)及其随后的再解离过程通常不包含在化学机制中。这样做通常是为了节省计算时间,因为假定在大多数情况下平衡强烈倾向于RO + NO反应。例外情况是甲基过氧自由基的反应,这是由于其在大气中的丰度,以及酰基-RO自由基的反应,这是由于过氧酰基硝酸盐(RONO,即过氧乙酰硝酸酯,PANs)的寿命较长。在本研究中,在德国于利希研究中心的大气模拟舱SAPHIR中,在不同温度(约276 K、约293 K、约305 K)下的大气相关条件下,研究了-2-丁烯和-2-己烯在NO存在下的夜间氧化过程。将测量得到的过氧自由基和氢过氧自由基以及其他痕量气体(臭氧、NO、挥发性有机化合物)的浓度与最新的零维箱模型计算结果进行了比较。只有当使用[Jenkin等人,2019,7691]最新SAR中的文献值将所有RO物种的可逆RO + NO反应包括在内时,才能实现良好的模型-测量一致性。观察到的良好一致性让人相信,最初为脂肪族RO推导的SAR可以应用于大范围的取代RO自由基,从而简化化学模型中的通用实现。在276 K时预测非酰基RO自由基的RONO浓度高达$2\times10^{-9}$ cm$^{-3}$,这有效地影响了RO自由基的动力学。在这些条件下,过氧自由基在污染源下游缓慢再生,并且可能通过RONO的沉积而在大气中损失。基于这项研究,在10°C的温度和几个ppbv的NO存在下,60%的RO自由基将以RONO的形式储存。在更低的温度和/或更高的NO混合比下,该比例会进一步增加。这不仅会影响预期的RO自由基浓度,而且由于过氧硝酸盐可以与OH自由基反应或光解,它们可能构成RO自由基的净汇,并且根据其寿命在不同位置增加NO$_x$(= NO + NO$_2$)的生成。在动力学模型中忽略这种化学过程可能导致对产物形成的误解,并可能妨碍对观测结果和模型预测的协调。