二次有机气溶胶的水相形成研究

二次有机气溶胶是大气颗粒物中的主要成分,对大气环境、气候以及人类健康等有重要影响。近年来的研究表明,水相形成二次有机气溶胶与传统气相形成二次有机气溶胶对二次有机气溶胶的贡献相当,且能够解释用传统气相形成方法无法解释的野外观测与模型模拟以及野外观测与室内烟雾箱模拟二次有机气溶胶在颗粒大小、分布、浓度以及老化程度等方面的差异,因而成为研究的热点。本综述重点介绍了目前大气中二次有机气溶胶水相形成的实验室研究,包括黑暗条件下的非自由基反应(水合、缩醛/半缩醛、醇醛缩合和催化反应)和光照条件下的自由基反应。同时,对二次有机气溶胶水相形成研究的发展方向进行了展望。     

用于研究大气氧化过程和机制的双反应器烟雾箱的评估和应用

设计并搭建了一个新的双反应器烟雾箱, 用于研究可生成臭氧或二次有机气溶胶(SOAs)的大气氧化过程. 该烟雾箱包括一个绝热的箱体及其内部两个体积为5 m³的氟化乙丙烯(FEP)薄膜反应器, 箱内的温度可以精确控制在-10到40 ℃之间. 利用该烟雾箱研究了光源对丙烯气相氧化机理的影响, 发现相对于传统的黑光灯光源, 采用的多重光源所得到的结果可以与模型更好地匹配. 进行了丙烯和间二甲苯的光氧化的初步实验, 发现该烟雾箱可用于模拟可产生臭氧或SOAs的气相氧化过程, 并可以通过不同初始浓度的对比实验找寻不同物种对反应过程的影响. 间二甲苯在不同NO_x条件下光氧化得到的SOA产率与之前的研究比较符合, 这表明该烟雾箱可以实现气-粒转化过程的模拟. 双反应器可以实现在一个关键条件的存在区别, 而其他条件完全一致的情况下的对比实验, 从而帮助我们进一步理解在大气复合污染过程中起关键作用的因素.     

二次有机气溶胶的气体/粒子分配理论

本文重点评述了二次有机气溶胶形成的气体/粒子分配理论,简要介绍了它的发展和可能的应用.在大气中,气体有机物种的氧化可以产生半挥发性的有机化合物,二次有机气溶胶的形成可以用气体/粒子分配的吸收模型来评估.气体/粒子分配过程决定于半挥发性化合物的成分、浓度和蒸气压,以及吸收性材料的浓度和成分.在气体/粒子分配理论的基础上,人们又研究和开发出二次有机气溶胶的分子组分的气体/粒子分配的热力学模型,它可以用来预估气溶胶中液态水的含量、无机物的分布、亲水性和疏水性有机物的分布.二次有机气溶胶形成的化学机理和气体/粒子分配的热力学模型与加利福尼亚工学院三维都市/区域性大气模型相结合,可以用于气相和气溶胶相模拟.     

大气颗粒物中有机硝酸酯的研究进展

有机硝酸酯是大气中挥发性有机物与自由基反应的产物,半挥发性的气相有机硝酸酯可以通过氧化反应或气粒分配作用进入颗粒相,是二次有机物的一个重要组成部分,逐渐引起大气化学研究者的广泛关注。颗粒相有机硝酸酯具有分子种类众多、理化性质复杂的特点,其全组分的测定有较高的难度,故目前开展的研究还较为有限。基于近年来国内外相关研究,本文对大气颗粒物中有机硝酸酯的形成机制、测定技术和估算方法进行了总结。随着测定技术的不断发展,外场观测已成为颗粒相有机硝酸酯的主要研究方法。热解析管激光诱导荧光系统(TD-LIF)和气溶胶质谱(AMS)为颗粒相有机硝酸酯的总量估算提供了方法,同时其较高时间分辨率的测定方法也为研究有机硝酸酯的大气行为提供更多信息。化学电离源质谱(CIMS)可以提供颗粒相有机硝酸酯的分子信息,有望在外场观测中得到广泛运用。在未来研究中,将外场观测研究、模型模拟和烟雾箱模拟实验相互结合,以实现对颗粒相有机硝酸酯的前体物追踪、大气化学过程的深入了解,为揭示大气颗粒物中有机硝酸酯的生成机制提供新的方向。     

乙苯光氧化产生二次有机气溶胶的化学成分及反应机理分析

在自制的烟雾腔内,研究羟基自由基(OH·)启动的乙苯的光氧化反应和一系列后续反应,产生了二次有机气溶胶. 采用空气动力学直径粒谱分析仪分析了气溶胶粒子的尺寸分布;并用自制的气溶胶飞行时间质谱仪快速、实时地测量了单个二次有机气溶胶粒子的分子组分. 初步探讨了这些组分的可能反应机理.     

大气有机硫酸酯化合物的特征及形成机制

本文总结了大气二次有机气溶胶的重要组分——有机硫酸酯化合物的特征及其形成机制的研究进展,并对相关研究进行了展望。近年来,通过实验室模拟与欧美地区的实际大气气溶胶样品的分析对比,发现有机硫酸酯化合物多由异戊二烯、α-/β-蒎烯以及其他单萜烯和倍半萜烯等经OH自由基、NO₃自由基或臭氧氧化后的反应产物与硫酸或硫酸盐气溶胶进一步反应而形成。有机硫酸酯化合物也可以通过硫酸或硫酸盐气溶胶反应性获取乙二醛等羰基化合物而形成。硫酸盐气溶胶酸性的增强会促进有机硫酸酯化合物的生成。有机硫酸酯化合物在水溶液中比较稳定,强酸性条件下才会发生水解作用。目前有机硫酸酯化合物的有效检测手段是离线电喷雾电离质谱(electrospray ionization mass spectrometry, ESI-MS)或在线气溶胶质谱(aerosol mass spectrometry, AMS)方法。     

二次有机气溶胶形成的化学过程

挥发性有机化合物的光氧化过程和光氧化产物的气态/粒子态均分过程是二次有机气溶胶形成的重要原因.二次有机气溶胶形成的化学机理主要涉及到挥发性有机化合物的光氧化过程及其一系列的后续反应,它们导致了对流层中臭氧浓度的增加和二次有机气溶胶的形成.本文将重点介绍二次有机气溶胶形成的重要化学过程和量子化学计算研究.     

挥发性和半挥发性有机物向二次有机气溶胶转化的机制*

从近20年二次有机气溶胶形成机制的研究成果可发现,挥发性和半挥发性有机物转化为二次有机气溶胶的主要物理化学过程可概述为光化学氧化机制、成核过程、凝结和气/粒分配机制以及非均相反应机制。本文系统总结了这些物理化学反应的发生过程及其影响因素,重点阐述了异戊二烯和甲苯同系物的光氧化机制,总结了二次有机气溶胶气/粒分配的两种理论--吸收机制和吸附机制,评述了发生在颗粒相上的非均相反应对二次有机气溶胶形成的重要作用。最后,对二次有机气溶胶形成机制研究的发展方向进行了展望。     

用自组织特征映射神经网络对飞行时间质谱采集的大气气溶胶单粒子进行分类

气溶胶飞行时间质谱仪(ATOFMS)在对气溶胶粒子的测量过程中,产生大量包含单粒子化学成分和粒径信息的数据。本研究采用具备矢量量化与数据降维能力的自组织特征映射网络(SOM),对自制的气溶胶飞行时间质谱仪24 h采集到的室内大气气溶胶质谱数据进行聚类分析。获得"含钙"、"盐类和二次气溶胶"、"二次颗粒"、"有机胺"、"富含钾有机物"、"无机盐"和"土壤"等20类颗粒。相比于其它聚类方法,SOM可进行可视化分析,对神经元进行再次聚类,聚类中心多。这些分类信息将有助于评估气溶胶粒子的反应和毒性,以及鉴别气溶胶粒子的起源。     

用气溶胶飞行时间质谱实时探测甲苯光氧化产生的单个二次有机气溶胶粒子

在烟雾腔内, 用紫外光照射甲苯、亚硝酸甲酯、一氧化氮和空气的混合物, 可以启动甲苯和羟基自由基(OH·)的光氧化反应和一系列的后续反应, 产生非挥发性和半挥发性有机化合物. 半挥发性有机化合物可以在气态和粒子态之间进行分配, 产生二次有机气溶胶粒子. 用自制的气溶胶飞行时间质谱仪, 快速、实时测量这些粒子的尺度、它们的分子成分和直径分布.     

Secondary organic aerosol formation from low-NO(x) photooxidation of dodecane: evolution of multigeneration gas-phase chemistry and aerosol composition

The extended photooxidation of and secondary organic aerosol (SOA) formation from dodecane (C(12)H(26)) under low-NO(x) conditions, such that RO(2) + HO(2) chemistry dominates the fate of the peroxy radicals, is studied in the Caltech Environmental Chamber based on simultaneous gas and particle-phase measurements. A mechanism simulation indicates that greater than 67% of the initial carbon ends up as fourth and higher generation products after 10 h of reaction, and simulated trends for seven species are supported by gas-phase measurements. A characteristic set of hydroperoxide gas-phase products are formed under these low-NO(x) conditions. Production of semivolatile hydroperoxide species within three generations of chemistry is consistent with observed initial aerosol growth. Continued gas-phase oxidation of these semivolatile species produces multifunctional low volatility compounds. This study elucidates the complex evolution of the gas-phase photooxidation chemistry and subsequent SOA formation through a novel approach comparing molecular level information from a chemical ionization mass spectrometer (CIMS) and high m/z ion fragments from an Aerodyne high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS). Combination of these techniques reveals that particle-phase chemistry leading to peroxyhemiacetal formation is the likely mechanism by which these species are incorporated in the particle phase. The current findings are relevant toward understanding atmospheric SOA formation and aging from the "unresolved complex mixture," comprising, in part, long-chain alkanes.     

Low‐Molecular Weight and Oligomeric Components in Secondary Organic Aerosol from the Photooxidation of p‐Xylene

A laboratory study was performed to investigate the composition of secondary organic aerosol (SOA) products from photooxidation of the aromatic hydrocarbon p‐xylene. The experiments were conducted by irradiating p‐xylene/CH₃ONO/NO/air mixtures in a home‐made smog chamber. The aerosol time‐of‐flight mass spectrometer (ATOFMS) was used to measure the size and the chemical composition of individual secondary organic aerosol particles in real‐time. According to a large number of single aerosol diameters and mass spectra, the size distribution and chemical composition of SOA were determined statistically. Experimental results showed that aerosol created by p‐xylene photooxidation is predominantly in the form of fine particles, which have diameters less than 2.5 μm (i.e. PM2.5), and aromatic aldehyde, unsaturated dicarbonys, hydroxyl dicarbonys, and organic acid are major product components in the SOA after 2 hours photooxidation. After aging for more than 8 hours, about 10% of the particle mass consists of oligomers with a molecular mass up to 600 daltons. The possible reaction mechanisms leading to these products are also proposed.     

Chemical Composition and Reaction Mechanisms for Secondary Organic Aerosol from Photooxidation of Toluene

A laboratory study was carried out to investigate the secondary organic aerosol (SOA) products from photooxidation of the aromatic hydrocarbon toluene. The experiments were conducted by irradiating toluene/CH₃ONO/NO/air mixtures in a home‐made smog chamber. The aerosol time‐of‐flight mass spectrometer (ATOFMS) was used to measure the size and the chemical composition of individual secondary organic aerosol particles in real‐time. According to a large number of single aerosol diameters and mass spectra, we obtained the size distribution and chemical composition of SOA statistically. Expeperimental results showed that aerosol created by toluene photooxidation is predominantly in the form of fine particles, which have diameters less than 2.5 μm (i.e. PM2.5), and the predominant components of aerosol are furane, methyl glyoxylic acid, phenol, benzaldehyde, benzyl alcohol, cresol, 3‐hydroxy‐2,4‐dioxo‐pentanal, methyl nitrophenol, and 5‐hydroxy‐4,6‐dioxo‐2‐heptenal. The possible reaction mechanisms leading to these products were also discussed.     

Real-time analysis of secondary organic aerosol particles formed from cyclohexene ozonolysis using a laser-ionization single-particle aerosol mass spectrometer.

A real-time analysis of secondary organic aerosol (SOA) particles formed from cyclohexene ozonolysis in a smog chamber was performed using a laser-ionization single-particle aerosol mass spectrometer (LISPA-MS). The instrument obtains both size and chemical compositions of individual aerosol particles with a high time-resolution (approximately 2 s at the maximum). Both positive and negative-ion mass spectra are obtained. Standard particles generated from dicarboxylic acid solutions using an atomizer were also analyzed. For both standard and SOA particles, the negative-ion mass spectra provided information about the molecular weights of the organic compounds in the particles, since the intense ions in the negative-ion mass spectra are mainly attributable to the molecular-related ions [M-H]-. It was demonstrated that the real-time single-particle analysis of SOA particles by the LISPA-MS technique can reveal the formation and transformation processes of SOA particle in smog chambers.     

Kinetics of N(2)O(5) hydrolysis on secondary organic aerosol and mixed ammonium bisulfate-secondary organic aerosol particles

The kinetics of the hydrolysis reaction of N(2)O(5) on secondary organic aerosol (SOA) produced through the ozonolysis of α-pinene and on mixed ammonium bisulfate-SOA particles was investigated using an entrained aerosol flow tube coupled to a chemical ionization mass spectrometer. We report room temperature uptake coefficients, γ, on ammonium bisulfate and SOA particles at 50% relative humidity of 1.5 × 10(-2) ± 1.5 × 10(-3) and 1.5 × 10(-4) ± 2 × 10(-5), respectively. For the mixed ammonium bisulfate-SOA particles, γ decreased from 2.6 × 10(-3) ± 4 × 10(-4) to 3.0 × 10(-4) ± 3 × 10(-5) as the SOA mass fraction increased from 9 to 79, indicating a strong suppression in γ with the addition of organic material. There is an order-of-magnitude reduction in the uptake coefficient with the smallest amount of SOA material present and smaller additional reductions with increasing aerosol organic content. This newly coated organic layer may either decrease the mass accommodation coefficient of N(2)O(5) onto the particle or hinder the dissolution and diffusion of N(2)O(5) into the remainder of the aerosol after it has been accommodated onto the surface. The former corresponds to a surface effect and the latter to bulk processes. The low value of the uptake coefficient on pure SOA particles will likely make N(2)O(5) hydrolysis insignificant on such an aerosol, but atmospheric chemistry models need to account for the role that organics may play in suppressing the kinetics of this reaction on mixed organic-inorganic particles.     

Chemical composition of secondary organic aerosol formed from the photooxidation of isoprene

Recent work in our laboratory has shown that the photooxidation of isoprene (2-methyl-1,3-butadiene, C(5)H(8)) leads to the formation of secondary organic aerosol (SOA). In the current study, the chemical composition of SOA from the photooxidation of isoprene over the full range of NO(x) conditions is investigated through a series of controlled laboratory chamber experiments. SOA composition is studied using a wide range of experimental techniques: electrospray ionization-mass spectrometry, matrix-assisted laser desorption ionization-mass spectrometry, high-resolution mass spectrometry, online aerosol mass spectrometry, gas chromatography/mass spectrometry, and an iodometric-spectroscopic method. Oligomerization was observed to be an important SOA formation pathway in all cases; however, the nature of the oligomers depends strongly on the NO(x) level, with acidic products formed under high-NO(x) conditions only. We present, to our knowledge, the first evidence of particle-phase esterification reactions in SOA, where the further oxidation of the isoprene oxidation product methacrolein under high-NO(x) conditions produces polyesters involving 2-methylglyceric acid as a key monomeric unit. These oligomers comprise approximately 22-34% of the high-NO(x) SOA mass. Under low-NO(x) conditions, organic peroxides contribute significantly to the low-NO(x) SOA mass (approximately 61% when SOA forms by nucleation and approximately 25-30% in the presence of seed particles). The contribution of organic peroxides in the SOA decreases with time, indicating photochemical aging. Hemiacetal dimers are found to form from C(5) alkene triols and 2-methyltetrols under low-NO(x) conditions; these compounds are also found in aerosol collected from the Amazonian rainforest, demonstrating the atmospheric relevance of these low-NO(x) chamber experiments.     

Secondary organic aerosol formation during the photooxidation of toluene: NOx dependence of chemical composition

The photooxidation of toluene is a potential source of secondary organic aerosol (SOA) in urban air, but only a small portion of the compounds present in SOA have been identified. In this study, we analyzed the chemical compositions of SOA produced by photoirradiation of the toluene/NOx/air system in laboratory chamber experiments by a combination of liquid chromatography-mass spectrometry, hybrid high-performance liquid chromatography-mass spectrometry, and iodometry-spectrophotometry. The dependence of the chemical composition on the initial NOx concentration was examined at initial NO concentrations ([NO]0) of 0.2 and 1 ppmv. Fifteen semivolatile products, including aromatic and ring-cleavage compounds, were quantified. However, the quantified products comprised only a small portion ( approximately 1 wt %) of the total aerosol mass. The total SOA yield ( approximately 13 wt %), the ratio of organic peroxides to total SOA mass ( approximately 17 wt %), and the density of SOA ( approximately 1.4 g cm-3) were independent of the NOx level, suggesting that the reaction mechanisms of the formation of major SOA products at [NO]0 = 0.2 and 1 ppmv are essentially the same. The negative-ion mass spectra of SOA samples showed that ion signals attributed to hemiacetal oligomers and/or decomposition products of peroxy hemiacetal oligomers were detected in the range of mass-to-charge ratios (m/z) between 200 and 500. The highest signals were detected at m/z = 155 and 177, and these were tentatively assigned to C7 unsaturated oxacyclic oxocarboxylic acids and C7 unsaturated oxacyclic dicarboxylic acids, respectively. We conclude that the major chemical components of the aerosol are hemiacetal and peroxy hemiacetal oligomers and low-molecular-weight dicarboxylic acids.     

Organic constituents on the surfaces of aerosol particles from southern Finland, amazonia, and california studied by vibrational sum frequency generation

This article summarizes and compares the analysis of the surfaces of natural aerosol particles from three different forest environments by vibrational sum frequency generation. The experiments were carried out directly on filter and impactor substrates, without the need for sample preconcentration, manipulation, or destruction. We discuss the important first steps leading to secondary organic aerosol (SOA) particle nucleation and growth from terpene oxidation by showing that, as viewed by coherent vibrational spectroscopy, the chemical composition of the surface region of aerosol particles having sizes of 1 μm and lower appears to be close to size-invariant. We also discuss the concept of molecular chirality as a chemical marker that could be useful for quantifying how chemical constituents in the SOA gas phase and the SOA particle phase are related in time. Finally, we describe how the combination of multiple disciplines, such as aerosol science, advanced vibrational spectroscopy, meteorology, and chemistry can be highly informative when studying particles collected during atmospheric chemistry field campaigns, such as those carried out during HUMPPA-COPEC-2010, AMAZE-08, or BEARPEX-2009, and when they are compared to results from synthetic model systems such as particles from the Harvard Environmental Chamber (HEC). Discussions regarding the future of SOA chemical analysis approaches are given in the context of providing a path toward detailed spectroscopic assignments of SOA particle precursors and constituents and to fast-forward, in terms of mechanistic studies, through the SOA particle formation process.     

Products and mechanism of secondary organic aerosol formation from reactions of linear alkenes with NO3 radicals

Secondary organic aerosol (SOA) formation from reactions of linear alkenes with NO(3) radicals was investigated in an environmental chamber using a thermal desorption particle beam mass spectrometer for particle analysis. A general chemical mechanism was developed to explain the formation of the observed SOA products. The major first-generation SOA products were hydroxynitrates, carbonylnitrates, nitrooxy peroxynitrates, dihydroxynitrates, and dihydroxy peroxynitrates. The major second-generation SOA products were hydroxy and oxo dinitrooxytetrahydrofurans, which have not been observed previously. The latter compounds were formed by a series of reactions in which delta-hydroxycarbonyls isomerize to cyclic hemiacetals, which then dehydrate to form substituted dihydrofurans (unsaturated compounds) that rapidly react with NO(3) radicals to form very low volatility products. For the approximately 1 ppmv alkene concentrations used here, aerosol formed only for alkenes C(7) or larger. SOA formed from C(7)-C(9) alkenes consisted only of second-generation products, whereas for larger alkenes first-generation products were also present and contributions increased with increasing carbon number apparently due to the formation of lower volatility products. The estimated mass fractions of first- and second-generation products were approximately 50:50, 30:70, 10:90, and 0:100, for 1-tetradecene, 1-dodecene, 1-decene, and 1-octene SOA, respectively. This study shows that delta-hydroxycarbonyls play a key role in the formation of SOA in alkene-NO(3) reactions and are likely to be important in other systems because delta-hydroxycarbonyls can also be formed from reactions of OH radicals and O(3) with hydrocarbons.