在烯烃-臭氧气相反应中,Criegee中间物的反应动力学及其反应性

本文通过烯烃-臭氧气相反应产生的Criegee中间物,研究其与二氧化硫及乙醛的反应动力学及反应性。实验结果表明:(1)稳定的Criegee中间物是通过烯烃-臭氧起始反应生成“热”的中间物和第三种惰性分子碰撞形成的,随后与二氧化硫或乙醛发生双分子反应;(2)在我们的实验条件下,当加入足够过量的乙醛时,可以用反应生成的次级臭氧化物产率的极限值来表征稳定的Criegee中间物的生成量;(3)通过测定稳定的Criegee中间物的单分子分解速度常数和它的双分子反应速度常数的比值,得到了稳定的CH_2OO、CH_3CHOO与二氧化硫、乙醛反应的速度常数的比值。     

挥发性有机物生成二次有机气溶胶影响因素的研究进展

二次有机气溶胶(SOA)的生成不仅受前体物排放量的影响,还与一些环境因素有关。为了更为科学地提出SOA污染防治对策,可以采用烟雾箱对SOA生成的影响因素进行模拟研究。介绍了近年来烟雾箱的设计与表征方法,分析了温度、相对湿度、光照强度、种子气溶胶、SO_2、NO_x等典型影响因素的研究现状。指出了现有研究的不足,认为SOA生成过程的模拟工具升级、定性分析和复合影响因素探讨是今后研究的重点。     

硫酸铵气溶胶对甲苯-NOx-空气体系光化学反应的影响

利用大气模拟烟雾箱,研究了硫酸铵气溶胶对甲苯-NOx-空气体系光化学反应的影响.结果表明,硫酸铵作为气溶胶种子,其存在可以加快反应过程中颗粒物(particle matter,PM)的生成速度,并提高甲苯的气溶胶产率.在高浓度的硫酸铵气溶胶种子条件下,其初始浓度对反应过程中NOx、NO和O3的浓度变化没有明显的影响,但对二次有机气溶胶(secondary organic aemsol,SOA)的生成有显著影响.在硫酸铵气溶胶种子浓度小于160 μg·m-3时,SOA的产率随初始气溶胶种子浓度的增大而增大,从最小7.2%到最大11.7%,其增幅超过60%.     

硫酸铵气溶胶对甲苯-NOx-空气体系光化学反应的影响

利用大气模拟烟雾箱,研究了硫酸铵气溶胶对甲苯-NO_x-空气体系光化学反应的影响.结果表明,硫酸铵作为气溶胶种子,其存在可以加快反应过程中颗粒物（particle matter, PM）的生成速度,并提高甲苯的气溶胶产率.在高浓度的硫酸铵气溶胶种子条件下,其初始浓度对反应过程中NO_x、NO和O₃的浓度变化没有明显的影响,但对二次有机气溶胶（secondary organic aerosol, SOA）的生成有显著影响.在硫酸铵气溶胶种子浓度小于160 μg·m^-3时,SOA的产率随初始气溶胶种子浓度的增大而增大,从最小7.2％到最大11.7％,其增幅超过60％.     

大气模拟烟雾箱中HONO的表征

NO2与H2O在烟雾箱表面生成HONO的异相反应是导致烟雾箱实验数据不确定性增加的主要原因之一,因此.必须对该反应进行表征.本研究采用烟雾箱实验与箱式模型模拟相结合的方法,确定实验系统特有的HONO释放速率.实验在室内烟雾箱实验系统完成,通过NO、NO2沉积实验获得的气态反应物在烟雾箱壁面(Teflon膜)上的沉积速率分别为0.0026 h-1及0.0025 h-1;光解实验得到NO2的光解速率为0.21min-1,在此基础上利用量子产率、吸收截面积、光谱分布计算出其它6个光解反应的速率常数.将实验获取的速率常数与CB-Ⅳ反应机理联合使用建立箱式模拟系统,利用c0一NO实验数据对模拟参数进行优化,得到该系统的HONO的释放速率为1.65×10-5cm3·mol-1·s-1.由此提供了一种表征实验与箱式模型联合使用确定烟雾箱系统HONO释放速率的有效方法.     

光化学烟雾箱的表征及初步应用

介绍了一套自制的用于光化学臭氧和二次有机气溶胶生成研究的室内烟雾箱系统,对该烟雾箱系统进行了一系列表征实验,包括活性物种的壁损失速率常数的测定,以及由CO-NOx光氧化实验确定的反应器内·OH源,并进行了乙烯-NOx和苯-NOx光氧化的初步实验.结果表明,O3和NO2在新反应袋中壁损失受湿度影响很小,而在旧反应袋中影响...     

大气模拟烟雾箱系统的研究进展

烟雾箱是研究大气光化学反应的主要工具.30年来国内外有多个研究机构建立了烟雾箱,并对各种光化学反应进行了研究,以收集数据来发展和检验大气光化学反应机理.从系统构造、配置仪器及所进行的光化学实验几个方面,综述了国内外烟雾箱系统的研究进展,其中背景影响较小的烟雾箱能为评价化学反应机理提供精度较高的数据,二次有机气溶胶(secondary organic aerosol,SOA)的形成机理成为目前的研究热点.     

用于汽车尾气光氧化的烟雾箱研究及其表征实验

大气中光氧化反应是造成大气中复合污染,加剧中国大气环境污染的重要因素。为了研究汽车尾气在大气中的光氧化反应,设计制作了一套用于汽车尾气光氧化反应的较大容积的室内烟雾箱实验系统,该系统主要包括反应系统、进样系统和检测分析系统。反应系统采取了移动式对箱设置,尾气进样系统考虑了汽车尾气的排放特点,检测系统采取了负压采气装置。通过对该烟雾箱的光强分布、光解实验、NO_2及O_3衰减等系列的表征实验表明,该烟雾箱系统的一些性能较国内已有的烟雾箱有一定程度的提高,而且更适合于模拟汽车尾气的光氧化反应,同时,该系统具有采样方便、两箱对比和可模拟多种环境等特点。     

NO2对二甲苯光氧化生成SOA及其吸光度影响

NO₂是大气中常见污染气体,影响大气二次有机气溶胶（Secondary organic aerosol,SOA）的形成.运用实验室烟雾箱模拟二甲苯大气光氧化反应过程,研究NO₂对二甲苯SOA生成量、光学特性和化学组成的影响.结果显示,NO₂促进二甲苯SOA的形成,NO₂浓度从0增长到900×10^-9,二甲苯SOA的质量浓度增长2倍左右,并且邻二甲苯SOA质量浓度大于对二甲苯SOA.这是因为邻位取代基相比于对位取代基更倾向于形成醛,有利于聚合反应形成低聚物,促进SOA形成.此外,NO₂浓度增加显著提高所生成SOA的单位质量吸光度（Mass absorption coefficients,MAC）,这是由于前体物邻二甲苯和对二甲苯化学结构不同,邻二甲苯所生成的含氮有机物具有更强吸光性,从而导致邻二甲苯SOA的MAC_{λ=365 nm}大于对二甲苯SOA的MAC_{λ=365 nm}.在线气溶胶质谱仪分析结果进一步显示：二者光化...     

深圳大气中VOCs的二次有机气溶胶生成潜势

使用气溶胶生成系数法和产率法,对深圳四季5种芳香烃和异戊二烯所生成的二次有机气溶胶(SOA)量分季节计算并比较得出:四季中除春季外,其余三季产率法计算得到的SOA量均高于生成系数法计算的结果,四季所生成SOA的平均值分别为(2.48±2.02)μg/m3和(2.10±1.21)μg/m3.2种方法计算结果均为夏季SOA的生成量最大,秋季和冬季次之,春季最小.生成系数法计算得出人为源和天然源的贡献分别为96%和4%,而产率法得到两种源的贡献分别为86%和14%.将生成系数法和产率法计算得到的夏季SOA值与实测值进行比较,发现计算值均低于实测值,分别占实测值的21%和31%.最后计算芳香烃和异戊二烯的自由基反应速率得出,与OH自由基反应是其生成SOA最主要的途径,比例为75%,与NO3自由基和O3的反应比例分别为22%和3%.在生成SOA速度上,苯乙烯的速度最快,苯的速度最慢.     

Assessing the influence of environmental conditions on secondary organic aerosol formation from a typical biomass burning compound

The atmospheric chemistry in complex air pollution remains poorly understood. In order to probe how environmental conditions can impact the secondary organic aerosol (SOA) formation from biomass burning emissions, we investigated the photooxidation of 2,5-dimethylfuran (DMF) under different environmental conditions in a smog chamber. It was found that SO₂ could promote the formation of SOA and increase the amounts of inorganic salts produced during the photooxidation. The formation rate of SOA and the corresponding SOA mass concentration increased gradually with the increasing DMF/OH ratio. The addition of (NH₄)₂SO₄ seed aerosol accelerated the SOA formation rate and significantly shortened the time for the reaction to reach equilibrium. Additionally, a relatively high illumination intensity promoted the formation of OH radicals and, correspondingly, enhanced the photooxidation of DMF. However, the enhancement of light intensity accelerated the aging of SOA, which led to a gradual decrease of the SOA mass concentration. This work shows that by having varying influence on atmospheric chemical reactions, the same environmental factor can affect SOA formation in different ways. The present study is helpful for us to better understand atmospheric complex pollution.     

Transient species in the ozonolysis of tetramethylethene

The reaction of alkenes with ozone has great effect on atmospheric oxidation, its transient species can produce OH radicals and contribute to the formation of secondary organic aerosols (SOA). In the present study, the reaction of tetramethylethene (TME) with ozone was investigated using self-assembled low temperature matrix isolation system. The TME and ozone were co-deposited on a salt plate at 15 K, and then slowly warmed up the plate. The first transient species primary ozonide (POZ) was detected, indicating that the reaction followed Criegee mechanism. Then POZ began to decompose at 180 K. However, secondary ozonide (SOZ) was not observed according to Criegee mechanism. Probably, Criegee Intermediate (CI) did not react with inert carbonyl of acetone, but with remaining TME formed tetra-methyl epoxide (EPO).     

Compilation of reaction kinetics parameters determined in the Key Development Project for Air Pollution Formation Mechanism and Control Technologies in China

A compilation of new advances made in the research field of laboratory reaction kinetics in China's Key Development Project for Air Pollution Formation Mechanism and Control Technologies was presented. These advances are grouped into six broad, interrelated categories, including volatile organic compound (VOC) oxidation, secondary organic aerosol (SOA) formation, new particle formation (NPF) and gas-particle partitioning, ozone chemistry, model parameters, and secondary inorganic aerosol (SIA) formation, highlighting the laboratory work done by Chinese researchers. For smog chamber applications, the current knowledge gained from laboratory studies is reviewed, with emphasis on summarizing the oxidation mechanisms of long-chain alkanes, aromatics, alkenes, aldehydes/ketones in the atmosphere, SOA formation from anthropogenic emission sources, and oxidation of aromatics, isoprene, and limonene, as well as SIA formation. For flow tube applications, atmospheric oxidation mechanisms of toluene and methacrolein, SOA formation from limonene oxidation by ozone, gas-particle partitioning of peroxides, and sulfuric acid-water (H₂SO₄-H₂O) binary nucleation, methanesulfonic acid-water (MSA-H₂O) binary nucleation, and sulfuric acid-ammonia-water (H₂SO₄-NH₃-H₂O) ternary nucleation are discussed.     

Review of the influencing factors of secondary organic aerosol formation and aging mechanism based on photochemical smog chamber simulation methods

The formation and aging mechanism of secondary organic aerosol (SOA) and its influencing factors have attracted increasing attention in recent years because of their effects on climate change, atmospheric quality and human health. However, there are still large errors between air quality model simulation results and field observations. The currently undetected components during the formation and aging of SOA due to the limitation of current monitoring techniques and the interactions among multiple SOA formation influencing factors might be the main reasons for the differences. In this paper, we present a detailed review of the complex dynamic physical and chemical processes and the corresponding influencing factors involved in SOA formation and aging. And all these results were mainly based the studies of photochemical smog chamber simulation. Although the properties of precursor volatile organic compounds (VOCs), oxidants (such as OH radicals), and atmospheric environmental factors (such as NO_x, SO₂, NH₃, light intensity, temperature, humidity and seed aerosols) jointly influence the products and yield of SOA, the nucleation and vapor pressure of these products were found to be the most fundamental aspects when interpreting the dynamics of the SOA formation and aging process. The development of techniques for measuring intermediate species in SOA generation processes and the study of SOA generation and aging mechanism in complex systems should be important topics of future SOA research.     

苯水相光氧化反应形成二次有机气溶胶的实验研究

来源于机动车尾气的苯能溶于大气水滴、云雾等水相中并发生水相光氧化反应,在水分蒸发后,产物保留在颗粒相中形成二次有机气溶胶(SOA)粒子.本文采用雾化器将羟基启动苯水相光氧化反应溶液雾化产生气溶胶粒子,通过扩散干燥管除去水蒸气后产生SOA粒子,采用气溶胶激光飞行时间质谱仪进行在线检测,利用紫外可见吸收光谱仪、红外光谱仪和液相色谱串联质谱仪离线测量SOA的化学组分.实验结果表明,激光解吸附质谱中存在醛类(m/z=29(CHO~+)、57(CHOCO~+))、羧酸(m/z=44(COO~+))和苯环(m/z=39(C_3H~+_3)、65(C_5H~-_5))特征裂解碎片峰.SOA粒子的红外光谱图中存在苯环C—H和C=C双键,以及C=O双键、C—O、O—H和C—O—C键的伸缩振动吸收峰,电喷雾电离质谱中存在m/z高达915的离子峰.这表明醛类、羧酸、酚类、芳香醚类产物和酚类产物发生聚合形成的高分子量化合物是SOA粒子的主要化学组分.这为研究人为源挥发性有机化合物水相反应形成SOA的机理提供了实验依据.     

氨对甲苯二次有机气溶胶形成和化学组分的影响研究

氨(NH_3)是大气中常见的主要碱性污染气体,能够影响二次有机气溶胶(SOA)的形成和化学组分.本文利用自制的烟雾腔系统开展了NH_3对甲苯SOA形成和化学组分的影响研究,先后采用扫描移动粒径谱仪(SMPS)、气溶胶激光飞行时间质谱仪(ALTOFMS)、紫外-可见分光光度计(UV-Vis)、衰减全反射傅里叶变换红外光谱仪(ATR-FTIR)和荧光光谱仪(MF)测量反应产生的SOA粒子的物理化学性质.结果显示,在光照60 min的时间范围内,有NH_3条件下形成的SOA质量浓度和中心粒径相比于无NH_3条件下分别增加了50%和25%,这说明NH_3能够显著促进甲苯SOA的形成.与无NH_3条件下相比,NH_3存在时甲苯SOA化学组分的紫外可见吸收光谱在270 nm处有明显的吸收峰;红外吸收光谱出现了CN、C—N、N—H键的吸收峰;激光解吸附质谱图中含有m/z=67(C_3H_3N_2~+)、m/z=41(C_2H_2N~+)和m/z=28(CH2N+)碎片峰.这些谱图信息综合表明是NH_3和甲苯SOA中的二醛组分反应形成了咪唑类新产物.这为研究人为源SOA的形成机制提供了实验依据.     

Competing esterification and oligomerization reactions of typical long-chain alcohols to secondary organic aerosol formation

Organosulfate (OSA) nanoparticles,as secondary organic aerosol (SOA) compositions,are ubiquitous in urban and rural environments.Hence,we systemically investigated the mechanisms and kinetics of aqueous-phase reactions of 1-butanol/1-decanol (BOL/DOL) and their roles in the formation of OSA nanoparticles by using quantum chemical and kinetic calculations.The mechanism results show that the aqueous-phase reactions of BOL/DOL start from initial protonation at alcoholic OH-groups to form carbenium ...     

Homogeneous and heterogeneous reactions of anthracene with selected atmospheric oxidants

The reactions of gas-phase anthracene and suspended anthracene particles with O3 and O3-NO were conducted in a 200-L reaction chamber, respectively. The secondary organic aerosol (SOA) formations from gas-phase reactions of anthracene with O3 and O3-NO were observed. Meanwhile, the size distributions and mass concentrations of SOA were monitored with a scanning mobility particle sizer (SMPS) during the formation processes. The rapid exponential growths of SOA reveal that the atmospheric lifetimes of gas-phase anthracene towards O3 and O3-NO are less than 20.5 and 4.34 hr, respectively. The particulate oxidation products from homogeneous and heterogeneous reactions were analyzed with a vacuum ultraviolet photoionization aerosol time-of-flight mass spectrometer (VUV-ATOFMS). Gas chromatograph/mass spectrometer (GC/MS) analyses of oxidation products of anthracene were carried out for assigning the time-of-flight (TOF) mass spectra of products from homogeneous and heterogeneous reactions. Anthrone, anthraquinone, 9,10- dihydroxyanthracene, and 1,9,10-trihydroxyanthracene were the ozonation products of anthracene, while anthrone, anthraquinone, 9-nitroanthracene, and 1,8-dihydroxyanthraquinone were the main products of anthracene with O3-NO.     

复合污染条件下人为源VOCs的SOA生成研究进展

大气细颗粒物(PM_2.5)仍是我国空气质量持续改善的重大挑战.近年来,二次有机气溶胶(SOA)对PM_2.5的贡献日益凸显.因此,深入认识复合污染条件下SOA生成机制和影响因素可以为进一步降低PM_2.5提供重要理论依据.实验室模拟是深入认识SOA生成机制的关键途径,也是模式模拟参数化方案的可靠来源之一.主要综述了我国多污染物共存条件下典型人为源挥发性有机物(VOCs)的SOA生成研究进展,包括汽油蒸气VOCs、生物质燃烧VOCs和含氧VOCs形成SOA过程中,前体物浓度、芳香烃含量、无机气体、种子气溶胶和相对湿度(RH)等不同因素对SOA生成的影响;阐述了实际大气VOCs的SOA生成潜势及其影响因素,最后提出了目前在SOA机制研究方面存在的关键科学问题,并对未来的研究方向进行了展望.     

Size distribution of the secondary organic aerosol particles from the photooxidation of toluene

In a smog chamber, the photooxidation of toluene was initiated by hydroxyl radical （OH.） under different experimental conditions. The size distribution of secondary organic aerosol（SOA） particles from the above reaction was measured using aerodynamic particle sizer spectrometer. It was found from our experimental results that the number of SOA particles increased with increasing the concentration of toluene. As the reaction time prolonged, the sum of SOA particles was also increased. After a reaction time of 130 min, the concentration of secondary organic aerosol particles would be kept constant at 2300 particles/cm^3. Increasing illumination power of blacklamps could significantly induce a higher concentration of secondary organic aerosol particle. The density of SOA particles would also be increased with increasing concentration of CH30NO, however, it would be decreased as soon as the concentration of CH30NO was larger than 225.2 ppm. Nitrogen oxide with initial concentration higher than 30. 1 ppm was also found to have little effect on the formation of secondary organic aerosol.