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凝聚相中过氧自由基促进有机硝酸盐生成

Enhanced Organic Nitrate Formation from Peroxy Radicals in the Condensed Phase.

作者信息

Barber Victoria P, LeMar Lexy N, Li Yaowei, Zheng Jonathan W, Keutsch Frank N, Kroll Jesse H

机构信息

Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, United States.

Department of Chemical Engineering, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, United States.

出版信息

Environ Sci Technol Lett. 2024 Aug 13;11(9):975-980. doi: 10.1021/acs.estlett.4c00473. eCollection 2024 Sep 10.

DOI:10.1021/acs.estlett.4c00473
PMID:39280078
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11391572/
Abstract

Organic alkoxy (RO) and peroxy (RO) radicals are key intermediates in multiphase atmospheric oxidation chemistry, though most of the study of their chemistry has focused on the gas phase. To better understand how radical chemistry may vary across different phases, we examine the chemistry of a model system, the 1-pentoxy radical, in three phases: the aqueous phase, the condensed organic phase, and the gas phase. In each phase, we generate the 1-pentoxy radical from the photolysis of -pentyl nitrite, run the chemistry under conditions in which RO radicals react with NO, and detect the products in real time using an ammonium chemical ionization mass spectrometer (NH CIMS). The condensed-phase chemistry shows an increase in formation of organic nitrate (RONO) from the downstream RO+NO reaction, which is attributed to potential collisional and solvent-cage stabilization of the RO-NO complex. We further observe an enhancement in the yield of carbonyl relative to hydroxy carbonyl products in the condensed phase, indicating changes to RO radical kinetics. The different branching ratios in the condensed phase impact the product volatility distribution as well as HO -NO chemistry, and may have implications for nitrate formation, aqueous aerosol formation, and radical cycling within atmospheric particles and droplets.

摘要

有机烷氧基(RO)和过氧自由基(RO₂)是多相大气氧化化学中的关键中间体,尽管对其化学性质的研究大多集中在气相。为了更好地理解自由基化学在不同相之间可能如何变化,我们研究了一个模型体系——1-戊氧基自由基在三个相中的化学性质:水相、凝聚有机相和气相。在每个相中,我们通过亚硝酸戊酯的光解产生1-戊氧基自由基,在RO自由基与NO反应的条件下进行化学反应,并使用铵化学电离质谱仪(NH₄⁺ CIMS)实时检测产物。凝聚相化学显示,下游RO + NO反应生成有机硝酸盐(RONO)的量增加,这归因于RO - NO络合物可能的碰撞和溶剂笼稳定作用。我们还进一步观察到,凝聚相中羰基产物相对于羟基羰基产物的产率有所提高,这表明RO自由基动力学发生了变化。凝聚相中不同的分支比会影响产物的挥发性分布以及HO₂ - NO₂化学性质,并可能对硝酸盐形成、水性气溶胶形成以及大气颗粒和液滴内的自由基循环产生影响。

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本文引用的文献

1
Using collision-induced dissociation to constrain sensitivity of ammonia chemical ionization mass spectrometry ( CIMS) to oxygenated volatile organic compounds.利用碰撞诱导解离来限制氨化学电离质谱(CIMS)对氧化挥发性有机化合物的灵敏度。
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2
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具有松散过渡态的无障碍反应决定了异戊二烯衍生有机硝酸盐的产率和寿命。
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4
Radical Cage Effects: The Prediction of Radical Cage Pair Recombination Efficiencies Using Microviscosity Across a Range of Solvent Types.自由基笼效应:使用不同溶剂类型的微观粘度预测自由基笼对复合效率。
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Multiphase Ozonolysis of Aqueous α-Terpineol.水相中α-松油醇的多相臭氧化反应。
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Large enhancement in the heterogeneous oxidation rate of organic aerosols by hydroxyl radicals in the presence of nitric oxide.在一氧化氮存在的情况下,羟基自由基对有机气溶胶非均相氧化速率的大幅增强。
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8
Formation of Secondary Organic Aerosol from the Direct Photolytic Generation of Organic Radicals.由有机自由基的直接光解生成二次有机气溶胶
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9
Secondary organic aerosol formation via the isolation of individual reactive intermediates: role of alkoxy radical structure.通过分离单个反应中间体形成二次有机气溶胶:烷氧基自由基结构的作用
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