冠状病毒气溶胶传播及环境影响因素

当前,新型冠状病毒肺炎正在全球大范围流行,严重影响了人类健康和生产生活.目前已明确的新型冠状病毒的传播途径包括飞沫传播和接触传播,一些传播感染事件的研究间接证明新型冠状病毒可以通过空气传播,然而对于新型冠状病毒通过气溶胶传播机制的认识仍然不足,其对疾病传播的相对贡献等还在研究和论证中.本文分析了引起重症急性呼吸综合征、中东呼吸综合征和新型冠状病毒肺炎的不同冠状病毒通过气溶胶传播的研究结果,评述了病毒气溶胶的产生机制、病毒气溶胶的空气动力学特征、冠状病毒在气溶胶中的存活规律及环境因素的影响、以及冠状病毒在室内外环境气溶胶中的赋存和传播情况,探讨了当前对于明确新型冠状病毒的气溶胶传播研究的不足以及跨学科研究的展望.     

珠江三角洲大气排放源清单与时空分配模型建立

收集整理2012年珠江三角洲地区(简称“珠江三角洲”)各种大气人为源及天然源基础活动数据,以排放因子法“自下而上”为主计算多污染物排放量,并建立本地化污染物空间分配方案及基于行业排污特征的时间分配谱,构建了具备时空分布属性的区域性网格化大气源排放清单.清单结果显示,2012年珠江三角洲SO2、NOx、CO、PM10、PM2.5、VOCs和NH3排放总量分别为55.2万t、102.9万t、349.2万t、95.2万t、38.5万t、153.9万t和17.7万t. 固定燃烧源是珠江三角洲SO2和NOx的最大排放贡献源,其中电厂和锅炉分别贡献了35.0%和41.8%的SO2排放,以及28.2%和16.2%的NOx排放;VOCs的最大贡献源是过程源,其中家具制造、石油精炼、油气码头排放量总和占比为52.4%;扬尘源是颗粒物的主要来源之一,对PM2.5的排放贡献达42.3%;NH3的主要排放源为畜禽养殖和化肥施用源,两者排放量占比分别为50.7%和26.8%.珠江三角洲大气污染物空间与时间分布结果显示,高排放污染源主要集中于“东莞-广州-佛山”一带,呈半环带状结构分布;白天时段(9:00~20:00)的排放强度明显高于夜晚时段(21:00~次日8:00);夏秋季节(4~10月)的排放强度略高于冬春季节(11月~次年3月).     

新疆地区气溶胶对地表太阳辐射的影响初探

为了进一步认识大气气溶胶对气候环境的影响,基于2017年Aqua MODIS C006气溶胶光学厚度（aerosol optical depth,AOD）产品、CERES SSF Aqua MODIS Edition 4A数据集的地表短波辐射以及地面观测太阳辐射数据,对2017年新疆地区AOD和地表太阳辐射年变化进行研究,并以沙尘和人类活动气溶胶丰富的南疆典型地区喀什为代表城市,采用AccuRT辐射传输模式定量化研究晴空时气溶胶对地表短波辐射的影响.结果表明：①地表太阳辐射月均值最大值出现在和田站的5月,为441.62 W·m^-2,最小值出现在乌鲁木齐站点的12月,为37.03 W·m^-2;CERES/SSF地表短波辐射资料与地面观测结果相比,阿克苏站、焉耆站和伊宁站的差距最小,喀什站和若羌站全年存在高估现象,其他站点存在不同程度的高低估现象.②2017年新疆地区AOD格点平均的年均值最小值为0.0175,最大值为0.4610,南疆地区的AOD整体高于北疆地区;2017年AOD格点春夏季的AOD均值分布与全年均值分布特征相似,其中春季的AOD高值区区域面积高于其他季节.③根据AccuRT计算,当AOD由0.05增加为0.56时,四季的地表向下短波总辐射均呈下降趋势,夏季下降幅度最大,由923.02 W·m^-2变化为677.61 W·m^-2,其次为春季和秋季,冬季下降幅度最小.AOD的减少变化导致的地表向下短波总辐射通量、直射辐射通量和散射辐射通量变化敏感度明显高于AOD增加所导致的变化敏感度.     

合肥市黑炭气溶胶浓度分布和变化特征研究

根据合肥市黑炭气溶胶自动在线监测结果、相关污染物监测数据、气象数据,分析了合肥市城区黑炭气溶胶的浓度分布特征。结果表明,2013年6月—2014年5月黑炭浓度的年平均值为(4.88±2.99)μg/m3,总体呈现春夏季浓度较低、秋冬季浓度较高的分布。黑炭浓度日变化呈双峰型,峰值出现在早07:00和晚20:00,早间峰值受大气扩散条件和人为活动的共同影响,晚间峰值受人为活动影响较大。在与其他污染物的相关性研究中,黑炭浓度与粒径较小的颗粒物PM1质量浓度相关性最好,波长为950 nm的测量通道测得的黑碳气溶胶与元素碳的相关性最好。     

齐齐哈尔市春季PM2.5中水溶性离子特征分析

2014年4—6月,在齐齐哈尔大学设立采样点,采集PM2.5样品。采用离子色谱法测定其中的主要水溶性无机离子,分析主要组成及污染来源。结果表明,齐齐哈尔市春季PM2.5平均质量浓度为46μg/m3,水溶性无机离子平均质量浓度为20.67μg/m3,占PM2.5质量浓度的42.82%。齐齐哈尔市PM2.5中二次组分主要以酸式硫酸盐形式存在。来源分析发现,PM2.5主要来源于移动源(如汽车尾气)、生物质燃烧及垃圾焚烧、固定源(化石燃料燃烧)、土壤及建筑尘。     

珠江三角洲气溶胶中正构烷烃分布规律、来源及其时空变化

珠江三角洲地区主要城市气溶胶中正构烷烃分布可分为３种类型，第一类为前峰型，主要来源于汽车尾气；第二类为后峰型，主要来源于植物蜡；第三类为双峰型，来源于植物蜡，燃料燃烧和尾气。     

Carboxylic acids in the troposphere, occurrence, sources, and sinks: A review

Carboxylic acids are ubiquitous and important components of the troposphere; they are currently measured in different environments. They are thought to have several sources comprising primary biogenic and anthropogenic emissions, hydrocarbons gas-phase oxidations, and some carbonyl compounds aqueous-phase oxidations. In the present review we make a synthesis of the concentrations of low molecular weight carboxylic acids in tropospheric aqueous and gaseous phases and in aerosol particles for different environments. We also successively examine the major sources of carboxylic acids and discuss their relative contribution to tropospheric concentrations for various environments as well as the principal sinks of these compounds.     

Experiments probing the influence of air exchange rates on secondary organic aerosols derived from indoor chemistry

Reactions between ozone and terpenes have been shown to increase the concentrations of submicron particles in indoor settings. The present study was designed to examine the influence of air exchange rates on the concentrations of these secondary organic aerosols as well as on the evolution of their particle size distributions. The experiments were performed in a manipulated office setting containing a constant source of d-limonene and an ozone generator that was remotely turned “on” or “off” at 6 h intervals. The particle number concentrations were monitored using an optical particle counter with eight-channels ranging from 0.1–0.2 to>2.0 μm diameter. The air exchange rates during the experiments were either high (working hours) or low (non-working hours) and ranged from 1.6 to>12 h⁻¹, with intermediate exchange rates. Given the emission rates of ozone and d-limonene used in these studies, at an air exchange rate of 1.6 h⁻¹ particle number concentration in the 0.1–0.2 μm size-range peaked 1.2 h after the ozone generator was switched on. In the ensuing 4.8 h particle counts increased in successive size-ranges up to the 0.5–0.7 μm diameter range. At higher air exchange rates, the resulting concentrations of total particles and particle mass (calculated from particle counts) were smaller, and at exchange rates exceeding 12 h⁻¹, no excess particle formation was detectable with the instrument used in this study. Particle size evolved through accretion and, in some cases, coagulation. There was evidence for coagulation among particles in the smallest size-range at low air exchange rates (high particle concentrations) but no evidence of coagulation was apparent at higher air exchange rates (lower particle concentrations). At higher air exchange rates the particle count or size distributions were shifted towards smaller particle diameters and less time was required to achieve the maximum concentration in each of the size-ranges where discernable particle growth occurred. These results illustrate still another way in which ventilation affects human exposures in indoor settings. However, the ultimate effects of these exposures on health and well being remain to be determined.     

广州地区大气中C2～C9非甲烷碳氢化合物的人为来源

研究了广州地区13种人为源的C2～C9非甲烷碳氢化合物的源成分谱,及其在2002年夏季和冬季环境空气中的组成和变化规律.应用CMB 8.0受体模型对各人为源进行了源解析,得到了该地区人为源的平均浓度贡献率,分别为:乙烯化工厂29.7%,机动车24.2%,加油站12.1%,石油加工9.0%,电子加工8.3%,涂料工艺4.3%,工业垃圾焚烧2.4%,炼焦1.9%,油墨工艺1.1%,卷烟加工0.9%,制冷工艺0.7%.通过对6个受体点的源解析,结果表明乙烯化工工业点源和流动源为该地区NMHCs人为源的控制重点,面源是控制难点.     

Environmental–geochemical characteristics of Cu in the soil and water in copper-rich deposit area of southeastern Hubei Province, along the middle Yangtze River, Central China

In this study, the natural Cu background concentration and Cu natural and anthropogenic contamination in soil, water and crop were investigated systematically in Huangshi area. The results show that regional geology is the dominant factor controlling the natural Cu background concentration in soil and water, and that pH is important to control the vertical distribution of Cu in soil under the same geographical and climatic conditions. The mineralization of rock bodies causes the natural Cu increase in soil and water, whereas, a large number of mining–smelting plants and chemical works are the main sources of Cu anthropogenic contamination. Cu in naturally and anthropogenically polluted soil displays differences in total and available contents, vertical distribution patterns and physico-chemical properties, the same happens in water.