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.     

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.     

Hygroscopicity of particles generated from photooxidation of α-pinene under different oxidation conditions in the presence of sulfate seed aerosols

Smog chamber experiments were conducted to investigate the hygroscopicity of particles generated from photooxidation of α-pinene/NOx with different sulfate seed aerosols or oxidation conditions. Hygroscopicity of particles was measured by a tandem differential mobility analyzer （TDMA） in terms of hygroscopic growth factor （Gf）, with a relative humidity of 85%. With sulfate seed aerosols present, Gf of the aerosols decreased very fast before notable secondary organic aerosols （SOA） formation was observed, indicating a heterogeneous process between inorganic seeds and organic products might take place as soon as oxidation begins, rather than only happening after gas-aerosol partition of organic products starts. The final SOA-coated sulfate particles had similar or lower Gf than seed-free SOA. The hygroscopicity of the final particles was not dependent on the thickness but on the hygroscopicity properties of the SOA, which were influenced by the initial sulfate seed particles. In the two designed aging processes, Gf of the particles increased more significantly with introduction of OH radical than with ozone. However, the hygroscopicity of SOA was very low even after a long time of aging, implying that either SOA aging in the chamber was very slow or the Gf of SOA did not change significantly in aging. Using an aerosol composition speciation monitor （ACSM） and matrix factorization （PMF） method, two factors for the components of SOA were identified, but the correlation between SOA hygroscopicity and the proportion of the more highly oxidized factor could be either positive or negative depending on the speciation of seed aerosols present.     

大气中挥发性有机物(VOCs)对二次有机气溶胶(SOA)生成贡献的参数化估算

大气中二次有机气溶胶(SOA)是PM25中的重要组成部分,挥发性有机物(VOCs)的光化学氧化是其主要来源之一.从VOCs转化生成SOA的过程非常复杂,参数化方法是一种相对简化的估算方式,可以用于区分不同VOCs物种对SOA生成的贡献.本文介绍了基于二产物和基于挥发性分级两种常用的参数化估算方法,并总结分析文献报道的SOA估算结果.文章中也指出现在的参数化估算还存在一些问题,如何准确量化VOCs向SOA的转化过程将是大气化学未来的重要研究工作.     

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.     

Roles of semivolatile and intermediate-volatility organic compounds in secondary organic aerosol formation and its implication: A review

Secondary organic aerosol (SOA) is a very important component of fine particulate matter (PM_2.5) in the atmosphere. However, the simulations of SOA, which could help to elucidate the detailed mechanism of SOA formation and quantify the roles of various precursors, remains unsatisfactory, as SOA levels are frequently underestimated. It has been found that the performance of SOA formation models can be significantly improved by incorporating the emission and evolution of semivolatile and intermediate-volatility organic compounds (S/IVOCs). In order to explore the roles of S/IVOCs in SOA formation, this study reviews some simulation models which could consider S/IVOCs for SOA formation as well as the development of emission inventories of S/IVOCs and S/IVOC modules for SOA formation. In addition, the future research directions for simulations of the effect of S/IVOCs on SOA formation are suggested.     

四乙基愈创木酚液相·OH氧化SOA产率及特征分析:初始浓度的影响

液相化学过程作为二次有机气溶胶（SOA）形成的一种必不可少的途径,引起了学界对大气化学的广泛关注.由于其反应复杂性,反应机制、产物特性及对SOA质量的贡献还没有完全理解.本文选择四乙基愈创木酚（4-ethylguaiacol,EG）为前体物,系统地研究了初始浓度（0.03、0.3和3 mmol·L^-1）的EG液相·OH氧化形成的液相二次有机气溶胶（aqSOA）特性的影响.用黑炭-气溶胶质谱（SP-AMS）测定aqSOA产率和氧化特性,气相色谱-质谱联用仪（GC/MS）、离子色谱（IC）测定产物和低分子有机酸.紫外分光光度计（UV-vis）和高效液相色谱测定了类腐殖质（HULIS）等表征光吸光产物的形成.结果表明,不同初始浓度（mmol·L^-1）下aqSOA的O/C都表现为随着反应时间延长而升高,分别在0.42~0.61（0.03 mmol·L^-1）、0.49~0.84（0.3 mmol·L^-1）和0.49~0.63（3 mmol·L^-1）之间变化.SP-AMS测定aqSOA组分发现高初始浓度时二聚体（C₁₆H₁₈ O₂⁺,m/z 302）量明显高,说明高浓度下更容易发生聚合反应.UV-vis分析表明,随光氧化反应的进行,250 nm处吸光明显增强,可能是由于250 nm处新的吸光性产物生成所致.反应过程中生成的HULIS浓度不断升高,与UV-vis测定的300~400 nm区域内吸光度增强结论一致,说明水相反应形成了棕色碳.IC检测到产物中含有小分子有机酸：甲酸、乙醇酸和草酸,其中甲酸浓度最高.GC/MS检测到aqSOA中含酮、单聚体和二聚体等,说明发生了官能团化和聚合化过程.     

Reactor characterization and primary application of a state of art dual-reactor chamber in the investigation of atmospheric photochemical processes

Increasing attention has been paid to the air pollution more recently. Smog chamber has been proved as a necessary and effective tool to study atmospheric processes, including photochemical smog and haze formation. A novel smog chamber was designed to study the atmospheric photochemical reaction mechanism of typical volatile organic compounds (VOCs) as well as the aging of aerosols. The smog chamber system includes an enclosure equipped with black lights as the light source, two parallel reactors (2 m³ of each) with separate control of light source and temperature, with a series of coupled instruments for online monitoring of gas phase and particle phase reactants and products. Chamber characterization, including air source stability, effective light intensity, temperature stability, as well as gas phase and particle phase wall losses, were carried out before further research. The results showed that our smog chamber systems developed by other domestic and international groups. It was also observed that the wall loss of aromatic VOCs varied with different functional groups as well as the isomerism. The results of preliminary simulation experiment from styrene-NO_x demonstrated that the chamber can be well utilized to simulate gas-particle conversion progresses in the atmosphere.     

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.     

长江三角洲2017年机动车IVOCs排放清单构建及其对SOA的生成影响

中等挥发性有机物（IVOCs）对大气中二次有机气溶胶（SOA）的生成有重要贡献,但尚未包括在目前的排放清单中.本研究以长三角地区为研究对象,分别基于排放因子法和IVOCs/POA比例系数法对长三角地区2017年机动车IVOCs的排放量进行估算,构建长三角地区2017年机动车IVOC排放清单,分析其不确定性并估算其对SOA生成潜势的影响.基于排放因子法的结果表明,2017年长三角地区机动车IVOCs排放总量为3.58万t,SOA的生成潜势为695 t,其中载货汽车的IVOCs排放量在长三角大部分城市的占比均超过70%;从燃料类型来看,柴油车的IVOCs排放量远高于汽油车.基于IVOCs/POA比例系数法的结果表明,由不同的IVOCs/POA比例以及不同的POA/PM_2.5占比得到的排放清单结果差别巨大,最大值可达64.2万t,最小仅为5.2万t,造成的SOA生成潜势分别为1.55万t和1032 t.本研究表明基于不同的估算方法构建的IVOCs排放清单结果差别巨大,具有很大的不确定性,将直接影响后续空气质量模型对SOA的模拟结果.因此,需进一步将不同清单结果用于空气质量模型中对SOA进行模拟,通过与观测值的比较,从而获得较为准确的长三角地区机动车IVOCs排放清单.     

我国机动车排放VOCs及其大气环境影响

挥发性有机化合物(volatile organic compounds,VOCs)作为大气中主要污染物之一,是O3和二次有机气溶胶(secondary organic aerosol,SOA)的重要前体物.为全面了解我国城市机动车排放VOCs对空气质量的影响,本文系统介绍了我国部分城市大气中VOCs的源解析最新成果,并分车型、分燃料综述了我国机动车VOCs的排放因子、成分谱及其对二次污染的贡献,以期为未来机动车VOCs排放和控制提供数据和理论支持.研究发现,机动车是我国城市大气VOCs的最大源,平均贡献率为36.8%;摩托车和轻型汽油车是主要排放车型.机动车尾气排放VOCs对城市O3和SOA生成都有重要贡献,随着排放标准提升和运行工况改善,机动车排放因子和臭氧生成潜势(ozone formation potentials,OFPs)明显降低,成分谱以芳香烃和烯烃等活性组分为主,对二次污染的贡献较大.     

一个沿海城市大气臭氧的本地生成过程及其对前体物的敏感性

在威海市两个采样点用苏码罐采集了全空气样品,利用三级冷阱预浓缩-GC/MS方法离线测定了空气样品中109种大气挥发性有机物(VOCs).使用基于观测的MCM机理大气化学模式(OBM-MCM)分析了大气臭氧生成对VOCs组分的敏感性及本地生成过程.结果表明:观测期间两个采样点的总挥发性有机物(TVOCs)平均浓度分别为27.84×10~(-9)和17.85×10~(-9),对TVOCs贡献最大的均是烷烃.模拟分析表明,大气臭氧生成与前体物的控制关系存在空间差异性,在一个观测点受VOCs控制,而在另一个观测点受NO_x和VOCs共同控制;模拟结果还表明,臭氧生成对活性烃类最为敏感,但是,含氧有机物、卤代烃和高碳烷烃对臭氧生成的影响和贡献也不可忽视;此外,计算了日平均臭氧净生成速率P(O_3)_(net),分别为6.41×10~(-9) h~(-1)和3.22×10~(-9) h~(-1),臭氧的本地生成过程扮演重要角色.     

氯化钙种子气溶胶对甲苯二次有机气溶胶与氨形成含氮有机物的影响

苯系物光氧化反应形成的二次有机气溶胶(SOA)是大气细粒子的重要组成部分.SOA羧酸和二元醛组分能与氨反应形成有机酸铵和咪唑类含氮有机物,它们能够吸收205 nm和270 nm的紫外辐射,是棕色碳的主要组分.氯化钙等无机种子气溶胶具有较大的比表面积,可为气相羰基化合物和氨提供凝结与反应载体,从而影响含氮有机物的形成.基于此,本文利用烟雾腔研究氯化钙种子气溶胶存在时甲苯SOA与氨的反应,采用紫外-可见分光光度计测量产物溶液在205 nm和270 nm处的吸光度,并定性研究不同浓度、湿度和酸度的氯化钙种子气溶胶对含氮有机物形成的影响.结果表明:氯化钙种子气溶胶能够促进甲苯SOA含氮有机物的形成;含氮有机物的生成浓度随着氯化钙种子气溶胶浓度和pH值的增加而逐渐增大.但当氯化钙种子气溶胶为碱性时,OH~-会与凝结的有机酸发生酸碱中和反应并抑制二元醛化合物水合形成四醇产物,从而不利于含氮有机物的生成;水分子的增加占据了氯化钙种子气溶胶表面的吸附活性位点,氨被吸附和凝结的量减少,从而导致含氮有机物的生成浓度随着相对湿度的增大而降低.本研究可为人为源SOA棕色碳的形成机制和化学组成研究提供实验依据.     

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.     

典型橡胶制品业VOCs排放特征及对周边环境影响

选取衡水市3家典型橡胶制品企业作为研究对象,通过GC-MS/FID对其VOCs排放特征进行研究,并运用最大增量反应活性系数（maximum incremental reactivity,MIR）和气溶胶生成系数（fractional aerosol coefficient,FAC）分别对其臭氧生成潜势（ozone formaiton potential,OFP）和二次有机气溶胶（secondary organic aerosol,SOA）生成潜势进行评估.结果表明,橡胶制品行业的VOCs排放种类主要包括烷烃类、酮类、醛类、醇类和苯系物等.对于传统的只有炼胶工艺和硫化工艺的橡胶制品企业,其特征污染物主要为酮类和醇类,而对于涉及涂胶工艺和喷漆工艺的橡胶制品企业来说,其特征污染物为苯系物.对典型生产工艺的臭氧和SOA的生成潜势进行了评估：臭氧影响方面,对于不涉及涂胶和喷漆工艺的橡胶制品企业,臭氧生成贡献主要来自于含氧烃,对于涉及涂胶和喷漆工艺的企业,由于胶黏剂和漆料等有机溶剂的大量使用,苯系物对臭氧生成的贡献还是要远远大于其它VOCs物种,占到了VOCs总贡献的82.9%;SOA影响方面,橡胶制品企业的SOA贡献基本全部来自于苯系物,其中炼胶和硫化环节的贡献非常小,SOA贡献的主要来源是涂胶和喷漆环节,其中又以喷漆环节的贡献最大.因此,对于只有炼胶和硫化等工艺的传统橡胶制品企业,应优先控制含氧烃的排放,而对于涉及涂胶和喷漆等工艺的橡胶制品企业,应优先控制苯系物的排放.     

Effect of illumination intensity and light application time on secondary organic aerosol formation from the photooxidation of α-pinene

Secondary organic aerosol (SOA) formation from hydroxyl radical (OH.) initiated photooxidation of α-pinene was investigated in a home-made smog chamber. The size distribution of SOA particles was measured using aerodynamic particle sizer spectrometer. The effects of illumination intensity and light application time on SOA formation for α-pinene were evaluated. Experimental results show that the concentration of SOA particles increased significantly with an increasing of illumination intensity, and the light...     

秋冬季节华北背景地区PM1污染特征及来源

利用高分辨率飞行时间气溶胶质谱仪(HR-ToF-AMS)在华北背景地区——上甸子区域大气本底站开展亚微米气溶胶(NR-PM_1)化学组分及粒径分布的连续观测实验,观测时段为2015年10月17日至2016年1月27日,涵盖了秋、冬两季.结果表明,整个观测期间NR-PM_1平均质量浓度为25.2μg·m~(-3),PM_1中有机物占绝对优势,硝酸盐占的比例高于硫酸盐.各化学组分平均粒径分布以积聚模态为主,其中,有机物峰形最宽,峰值粒径最小,硝酸盐峰值粒径最大,表明有机物在颗粒物形成、增长初期及老化阶段均有贡献,硝酸盐在气溶胶粒子老化过程中更易于增长为大粒子.有机物种元素特性分析结果显示,秋、冬季有机气溶胶平均氧碳比(O/C)和氢碳比(H/C)为0.58和1.58,OM/OC达1.91,有机气溶胶的氧化程度高于城市站点平均水平.在华北地区污染环境下,有机气溶胶演变途径Van Krevelen拟合曲线斜率为-0.21,其老化潜质和速率较珠三角地区和欧美地区城市要慢.对比污染时段和清洁时段化学组成特征发现,在污染时段,硝酸盐质量浓度及其对PM_1的贡献率超过硫酸盐,有机物氧化程度明显高于清洁时段.后径向轨迹气团分析结果显示,污染时段气团来向较为复杂,来自西部,南部以及东北部气团均有贡献,清洁时段,主要受来自西伯利亚洁净空气的影响,对站点污染物扩散作用明显.     

基于工艺过程的金属包装业VOCs污染特征

识别金属包装业挥发性有机化合物(volatile organic compounds,VOCs)产生和排放节点,定量分析不同类型生产工艺所排放VOCs的物种及含量,结合最大增量反应活性法和修正的气溶胶生成系数法对行业二次污染进行核算.结果表明,金属包装业排放的VOCs主要为苯系物、醇类、酮类和酯类,苯系物和醇类在不同类型工序和排污节点中贡献较大,酮类和酯类贡献相对较少,单物种浓度最高的VOCs为正丁醇,浓度达269.08mg·m~(-3);生产线与相应的排气筒之间VOCs物种浓度相关性较好,但物种种类存在差异;行业的O_3和二次有机气溶胶(secondary organic aerosol, SOA)生成潜势(以O_3/VOCs和SOA/VOCs计)分别为(3.09±0.94)g·g~(-1)和(2.58±1.99)g·g~(-1),苯系物和内全涂烘干工序为O_3和SOA的主要前体物和首要生成节点.     

兰州市低碳数正构烷烃组分特征及大气化学反应活性分析

为明确兰州市大气环境常态下低碳数正构烷烃（C₅~C₁₉）质量浓度变化、组分特征及大气化学反应活性之间的关系,于2017年11月-2018年6月选取兰州市5个采样点,利用TENAX吸附管采集空气样品,应用TD-GC/MS（热脱附-气质联用）法对样品进行分析.对空气样品中低碳数正构烷烃大气化学反应活性的OFP（臭氧生成潜势）、·OH消耗速率、SOA（二次有机气溶胶）生成潜势进行评估计算,通过相关性分析及因子分析法分析低碳数正构烷烃的大气化学反应活性贡献率特征.结果表明:①在10种低碳数正构烷烃中,正己烷（C₆）对OFP的贡献率最大,正辛烷（C₈）对·OH消耗速率的贡献率最大,二者的贡献率分别为37.71%和37.64%.②在10种低碳数正构烷烃中正辛烷（C₈）对SOA生成潜势的贡献率最大,为50.02%.③大气化学反应活性参数相关性分析表明,低碳数正构烷烃总质量浓度与OFP、·OH消耗速率相关性显著（R分别为0.895和0.948）.④因子分析表明,5个未知因子所包含的化学反应活性信息量在94.511%以上,所含信息量也体现了未知因子组成的重要性,可为进一步解析大气化学反应活性提供参考.研究显示,正辛烷、正己烷是低碳数正构烷烃的2个关键活性组分,正辛烷是大气化学反应活性贡献率最大的化合物之一,也是汽车尾气排放源的主要组成部分,正己烷是人为源与自然源的混合产物.      

长株潭城市群人为源VOCs排放清单及其对环境的影响

基于长株潭城市群环境统计数据和排放系数,建立了2014年长株潭城市群人为源VOCs排放清单,并根据空间特征数据进行了3 km×3 km的空间网格分配,同时还估算了各类人为源排放VOCs的臭氧生成潜势与二次有机气溶胶生成潜势.结果表明,长株潭地区人为源VOCs排放总量为113.49 kt,其中工艺过程源、溶剂使用源和移动源为最主要的排放源,排放量分别为35.88、28.72、22.13 kt,工艺过程源中75.34%的VOCs排放量来自建材生产,溶剂使用源中建筑涂料和汽车喷涂为主要排放源;各区县中醴陵市的VOCs排放量最高为16.58 kt;长株潭地区总臭氧生成潜势为375.33 kt,溶剂使用源贡献最大为27.28%,生物质燃烧源的臭氧生成能力最强;二次有机气溶胶生成潜势中,溶剂使用源贡献比例最大为35.35%,其二次有机气溶胶生成能力也强于其它源类;空间分布特征显示城区的网格排放量较大.