宁波市镇海区大气降尘矿物组成及来源解析

为探讨宁波市镇海区大气降尘矿物组成及来源，用X射线衍射法分析了镇海区6个土地功能区2019年12月至2020年11月4个季度的大气降尘样品的矿物组成和含量，并开展了矿物来源解析。结果显示，降尘中以石英、长石、碳酸盐类矿物和黏土矿物为主，年均质量分数分别为29.2%、33.3%、24.2%和7.7%,且不同功能区各季度降尘中矿物含量普遍有显著差异。来源解析表明，镇海区降尘中矿物来源主要以地面扬尘输入为主，同时周边源区输入及人类活动和工业密集区燃煤等输入对降尘矿物组成有较显著影响，除黏土矿物、碳酸盐类矿物和长石类矿物之外，其他矿物的含量还与不同季节的气温和风向有关。     

大气可吸入颗粒物(PM10)中矿物组分的X射线衍射研究

利用X射线衍射技术对北京2002春季和夏季的可吸入颗粒物进行了研究.结果表明,北京春季和夏季可吸入颗粒物的矿物组成明显不同,春季可吸入颗粒物中的矿物以硅铝酸盐为主,同时存在碳酸盐、硫酸盐、硫化物、铁的氧化物、粘土矿物以及难以鉴定的矿物;在夏季的样品中,矿物的种类有所减少,却有新的物种出现,如氯化氨、硫酸氨等.XRD定量分析显示,在沙尘天气时,可吸入颗粒物中石英和粘土矿物以及非晶质分别占到24.1%、28.5%和2 0%,斜长石和方解石分别占到10.4%和8.1%,其他矿物总共不到10%.矿物组分的确定对可吸入颗粒物来源的识别有一定的指导作用.     

上海市浦东新区大气细颗粒物中重金属污染特征及来源解析

于2017年对浦东城区和郊区大气PM2.5中的重金属特征和来源进行了分析。结果表明,K、Fe、Na、Ca、Mg、Al等矿物元素为浦东新区PM2.5中含量最高的金属元素,其中K的年均值为297.3 ng/m^3。浦东城区的不同元素在季节变化上呈现较为不同的变化规律,郊区的金属元素值大部分呈现春季先逐月下降,在夏、秋季有起伏波动,在10月之后逐渐上升;沙尘+道路源+建筑扬尘、煤燃烧、工业排放、金属冶炼、船舶排放、海盐+垃圾焚烧+生物质燃烧为浦东城区PM2.5中重金属元素的6大类主要来源。其中沙尘+道路源+建筑扬尘对Ca的贡献率为82.7%,煤燃烧对As的贡献率为86.6%,工业排放对SO4^2-的贡献率达到65.9%,金属冶炼对Cr的贡献率为75.7%,船舶排放对V的贡献率为97.5%、海盐+垃圾焚烧+生物质燃烧对Cl^-的贡献率为93.0%。煤燃烧和金属冶炼主要来自于西部方向。船舶排放分布在长江口及其延伸带。浦东新区PM2.5中重金属元素的质量浓度与本地源排放强度、外界传输和大气扩散条件均有密切关系。     

X射线荧光法分析甘草提取物中的微量元素

作者叙述了用X射线荧光灰化粉末法直接分析甘草提取物中的微量元素方法。     

湖北省黄石市城区降尘物相特征的研究

本文对黄石市若干主要工业污染源,山丘地表风化土,市区地面扬尘及不同高度降尘样品在分别作X射线粉未衍射(XRPD)分析的基础上,进行特征物相之间的比较,并与降尘粒度分析结果作对照,确定降尘的物质来源及扬尘高度。这对环境质量评价工作具有一定意义     

利用大气超级站对乌鲁木齐市一次沙尘天气过程及组份的分析

本研究利用大气超级站对乌鲁木齐市4月9日至10日沙尘天气过程,粒径谱、离子和重金属组成及变化进行分析。研究结果表明激光雷达观测结果与环境空气质量监测基本一致;小粒径颗粒在沙尘和非沙尘时段含量最多,但在沙尘时段大粒径颗粒的增长幅度远大于小粒径;沙尘过程中的离子主要来源于土壤一次源;沙尘过程中地壳元素浓度及占比均显著升高,会稀释环境空气中人为污染元素。     

京津冀地区一次浮尘过程的车载激光雷达走航观测

利用双波长三通道激光雷达与车载激光雷达,针对2018年3月28日京津冀区域的浮尘天气过程,分别进行了定点垂直观测与车载走航观测,对这次浮尘天气中沙尘的源地、沙尘气溶胶的时空分布、沙尘的传输路径与传输方式进行了综合分析。位于北京的激光雷达监测到28日凌晨开始,沙尘气溶胶与近地面污染物混合,受沙尘影响近地面污染物浓度迅速升高。北京到沧州的车载激光雷达走航观测结果显示,沙尘气溶胶先向南传输到京津冀南部区域,随后向西南方向传输,同时观测到京津冀区域上空1. 5 km左右存在沙尘传输带。结果表明,使用车载激光雷达走航观测,结合定点垂直激光雷达与其他地面监测数据,能可靠地观测到沙尘过程中颗粒物的时空变化特征。     

北京西北城区春季PM10单颗粒形貌类型及成分特征

主要对北京西北城区2010年度春季大气可吸入颗粒物的理化特征进行分析研究,通过利用高分辨率场发射扫描电镜和图像分析技术研究了区内可吸入颗粒物的微观形貌类型及百分含量特征,利用扫描电镜及能谱分析研究矿物颗粒的元素组成及富集类型。结果表明,在西北城区春季大气PM₁₀中可识别出烟尘集合体、球形颗粒、矿物和其他未知颗粒等4种单颗粒类型,沙尘暴天气对矿物颗粒的数量比例影响较大,同时影响颗粒物粒度分布。矿物颗粒按成分可分为"富Si"、"富Ca"、"富Fe"、"富S"、"富Na"、"富Ti"、"富Al"、"富Cl"和"富Mg"颗粒九大类,沙尘天气与非沙尘天气的矿物颗粒均以"富Si"颗粒、"富Ca"颗粒、"富Fe"颗粒、"富S"颗粒等为主。     

沙尘暴降尘的化学组份和粒径分布特征

对发生在我国西北地区沙尘暴降尘沉积物,采用中子活化法和Ｘ射线吸收－－沉降法对其中的３８种元素和粒径分布特征进行了分析和研究。并分别以地壳元素和本区域土壤背景值为参考,讨论了沙尘暴沉降物的富集因子等问题。     

春季一次典型沙尘天气对南京市空气质量影响研究

2016年5月6日—8日南京市经历了一次由沙尘影响的重污染过程,在此期间对南京城区的PM_(10)、PM_(2.5)和PM_(2.5)化学组分、消光系数、退偏振比等参数进行连续观测,结合HYSPLIT后向轨迹模拟对此次过程作相关分析。结果表明:此次沙尘为典型的北方传输影响,传输方向为西北至东南,受其影响南京市空气质量一度达到重度污染;PM_(2.5)中Ca2+平均质量浓度达1.52μg/m3,高出沙尘过境后2.45倍;近地面至高空1.2 km范围内消光系数值约0.4 km~(-1),退偏振比值达0.4左右,沙尘造成近地面PM_(10)和PM_(2.5)质量浓度均有升高。     

Elemental and individual particle analysis of atmospheric aerosols from high Himalayas

Atmospheric aerosols were collected during the scientific expedition to Mt. Qomolangma (Everest) in May–June, 2005. The elemental concentrations of the aerosols were determined by inductively coupled plasma mass spectrometry. This yielded data for the concentration of 14 elements: Na, Mg, Al, K, Ca, Ti, V, Cr, Mn, Fe, Ni, Cu, Zn, and Pb. The mean elemental concentrations were generally comparable with those from central Asia and the Arctic, while much higher than those from Antarctic. Size, morphology, and chemical composition of 900 individual aerosol particles were determined by scanning electron microscopy and energy-dispersive X-ray microanalysis. Based on morphology and elemental composition, the particles were clustered into eight groups: soot (8%), tar ball (3%), alumosilicates/silica (55%), calcium sulfate (16%), Ca/Mg carbonate (2%), Fe/Ti-rich particles (3%), Pb-rich particles (1%), and biological particles (12%). The sampling site, located at 6,520 m in the Himalayas, is particularly remote and located at high altitude. Nonetheless, high aerosol enrichment factors for copper, chromium, lead, nickel, vanadium, and zinc all suggest the influence of long-range transported pollution, while enrichment in calcium and the presence of alumino-silicates in individual particle analyses indicates a distinct mineral dust influence. The backward air mass trajectories showed that the northwestern part of India may contribute to the atmospheric aerosol in the central high Himalayas.     

西安城北地区秋季PM_(2.5)中的矿尘颗粒污染特征

采用单颗粒气溶胶飞行时间质谱仪(Single Particle Aerosol Mass Spectrometer,SPAMS)对西安市大气矿尘颗粒物进行连续12 d在线分析,共采集到107 425个同时含有正负质谱信息的矿尘颗粒,矿尘颗粒物占PM_(2.5)样本数的8.44%。结果表明,矿尘颗粒物的正离子碎片成分以Na~+、K~+、Al~+、Ca~+、CaO~+、Fe~+为主,同时还含有Pb~+等,负离子碎片成分以NO~-_2和NO~-_3为主,另外还含有HSO~-_4、SiO~-_3、HSiO~-_3、H(NO_3)~-_2等。在西安市大气细颗粒物中,矿尘颗粒物中贡献较大的几类(如含钙、含铁、铁氧颗粒物等)大多是老化的成分。将观测阶段采集到的矿尘颗粒纳入本地污染源谱进行来源分析,其主要来源为扬尘源、工业源、燃煤源和汽车尾气源等。     

Comparison of EC and BC and evaluation of dust aerosol contribution to light absorption in Xi'an, China

The concentrations of EC, BC and dust aerosols were determined for atmospheric samples collected from an observation station in Xi'an, China. The results show that the averaged correlation coefficient between EC and BC was founded to be 0.72 with 0.81 (n = 49) in autumn, 0.70 (n = 112) in winter and 0.69 (n = 57) in spring, respectively. Absorption coefficients of dust aerosol were estimated to be 2.7 m² g⁻¹ in autumn and 4.4 m² g⁻¹ in winter. The comparison of absorption coefficients of dust aerosol with those of BC implies that BC is the principal light-absorbing aerosol over Xi'an atmosphere. By combining thermal analysis of elemental carbon and dust contents in the aerosol samples, however, the fraction of dust absorption to total light absorption is estimated to be 19% in autumn and 31% in winter, respectively.     

Atmospheric Aerosol over a Southeastern Region of Texas: Chemical Composition and Possible Sources

Speciated samples of PM_2.5 were collected at a site in Jefferson County, Texas by US EPA (Environmental Protection Agency) from July of 2003 to August of 2005. A total of 269 samples with 52 species were measured; however, 22 species were excluded in this study because of too many below-detection-limit data. The data set was analyzed by positive matrix factorization (PMF) to infer the sources of PM observed at the site. The analysis identified ten sources: sulfate-rich secondary aerosol I (35.9%), sulfate-rich secondary aerosol II (21.0%), cement/carbon-rich (11.7%), wood smoke (8.8%), metal processing (6.3%), motor vehicle/road dust (5.7%), nitrate-rich secondary aerosol (3.3%), soil (3.2%), sea salt (2.6%), and chloride depleted marine aerosol (1.6%). Sulfate and nitrate mainly exist as salts. The two sulfate-rich secondary aerosols account for almost 57% of the PM_2.5 mass concentration. The factor containing highest concentrations of Cl and Na was attributed to sea salt due to the proximity of the monitoring site to the Gulf of Mexico. The chloride depleted marine aerosol was related to the sea salt aerosol. Cement/carbon-rich, wood smoke, metal processing, and motor vehicle/road dust factor were likely to be the local sources.     

Study on Size Distribution of Total Aerosol and Water-Soluble Ions During an Asian Dust Storm Event at Jeju Island, Korea

Soil dust particles transported from loess regions of the Asian continent, called Asian dust, highly influences the air quality of north-eastern Asia and the northern Pacific Ocean. In order to investigate the effects of these dust storms on the chemical composition of atmospheric aerosol particles with different size, measurements of size distributions of total aerosol and major ion species were carried out on Jeju Island, Korea during April 2001. Juju Island was chosen for the study because the levels of emissions of anthropogenic air pollutants are very low. A 5-stage cascade impactor was used to sample size-fractionated aerosol particles. Samples were analyzed for major water-soluble ions using Dionex DX-120 ion chromatograph. The average mass concentration of total aerosol was found to be 24.4 and 108.3 microg m(-3) for non-Asian dust and Asian dust periods, respectively. The total aerosol size distribution, measured during the non-Asian dust period, was bimodal, whereas the coarse particles dominated the size distribution of total aerosol during the Asian dust period. It was found that SO4(2-), NH4+ and K+ were mainly distributed in fine particles, while Cl-, NO3-, Na+, Mg2+ and Ca2+ were in coarse particles. Although SO4(2-) was mainly distributed in fine particles, during the Asian dust period, the concentrations in coarse particles were significantly increased. This indicates heterogeneous oxidation of SO2 on wet surfaces of basic soil dust particles. The NH4+ was found to exist as (NH4)2SO4 in fine particles, with a molar ratio of NH4+ to SO4(2-) of 2.37 and 1.52 for non-Asian dust and Asian dust periods, respectively. Taking into account the proximity of the sampling site to the sea, and the observed chloride depletion, coarse mode nitrate, during the non-Asian dust period, is assumed to originate from the reaction of nitric acid with sodium chloride on the surfaces of sea-salt particles although the chloride depletion was not shown to be large enough to prove this assumption. During the Asian dust period, however, chloride depletion was much smaller, indicating coarse nitrate particles were mainly produced by the reaction of nitric acid with surfaces of basic soil particles. Most chloride and sodium components were shown to originate from sea-salt particles. Asian dust aerosols, arriving at Jeju Island, contained considerable amounts of sea-salt particles as they passed over the Yellow Sea. Ca2+ was shown to be the most abundant species in Asian dust particles.     

因子分析法解析北京市大气颗粒物PM10的来源

2004年10月份在北京市6个采样点采集了大气PM10样品,分析了大气颗粒物的质量浓度、元素组成、离子、有机碳(OC)和元素碳(EC)的浓度,并用因子分析模型对颗粒物的来源进行了研究。结果显示,北京市大气颗粒物的来源主要有6类:建筑水泥尘/机动车尾气尘/燃煤尘、土壤风沙尘、二次粒子尘、工业粉尘、生物质燃烧尘和燃油尘。用模型计算得到的各源对PM10的贡献率分别为建筑水泥尘/机动车尾气尘/燃煤尘占36.57%、土壤风沙尘占16.07%、二次粒子尘占12.33%、工业粉尘占10.29%、生物质燃烧尘占6.07%、燃油尘占3.84%、其它占14.84%。其中建筑水泥/机动车尾气尘/燃煤尘、土壤风沙尘、二次粒子尘、工业粉尘是大气颗粒物PM10的主要来源。实验表明,在缺少源成分谱时可以用因子分析模型来分析大气颗粒物的来源及其相对贡献。     

Mineralogy of Atmospheric Suspended Dust in Three Indoor And One Outdoor Location in Oman

The aim of this work is to characterize the mineral phases present in the atmosphere at three locations in northern Oman. Samples of atmospheric particles were collected using a high volume sampler. Three indoor and one outdoor location were chosen in this investigation. Sampling locations included a residential house located nearby the cement plant, a residential house located nearby a refinery plant, and a residential house located at Al-Suwayq residential area. Indoor air was sampled from these three houses. Moreover, for the Al-Suwayq residential house, sampling was also taken outside the house for comparison. The dust samples were analysed for their microanalysis characterization and their mineral contents as well. The microanalysis enabled us to identify the metals present in the particles. Furthermore, the mineralogical analysis of the sample filters showed the presence of quartz as the principal phase inside the house of Al-Suwayq, whereas quartz, dolomite, and gypsum were common phases outside the house. In the residential house nearby the cement plant, it was found that calcite, quartz, dolomite and goethite were the principal phases whereas the particles collected from the house nearby the refinery composed primarily of dolomite and calcite. The airborne dust collected at the refinery and Al-Suwayq were probably sourced in the natural environment and mobilised by natural processes. However, at the cement factory the crushing and grinding of limestone during the industrial process has contributed significantly to the airborne dust load. Generally, the information obtained in this study will be invaluable as no data for the mineral content of atmospheric dust existed in the Oman.     

The return periods and risk assessment of severe dust storms in Inner Mongolia with consideration of the main contributing factors

This study presents a methodology for return period analysis and risk assessment of severe dust storm disaster. Meteorological observation data, soil moisture data, and remote sensing data from 30 meteorological stations in Inner Mongolia (western China) from 1985 to 2006 were used for the study. A composite index of severe dust storm disaster (Index I (SDS)) based on the influence mechanisms of the main contributing factors was developed by using the analytic hierarchy process and the weighted comprehensive method, and the hazard risk curves (i.e., the transcendental probability curves of I (SDS)) for the 30 stations were established using the parameter estimation method. We then analyzed the risk of the occurrence of severe dust storm under different scenarios of 5-, 10-, 20-, and 50-year return periods. The results show that the risk decreased from west to east across Inner Mongolia, and there are four severe dust storm occurrence peak value centers, including Guaizihu, Jilantai, Hailisu, and Zhurihe-Erenhot. The severity of dust storms in seven places will be intolerable in the 50-year return period scenario and in three places in the 20-year return period scenario. These results indicate that these locations should concentrate forces on disaster prevention, monitoring, and early warning. The I (SDS) was developed as an easily understandable tool useful for the assessment and comparison of the relative risk of severe dust storm disasters in different areas. The risk assessment was specifically intended to support local and national government agencies in their management of severe dust storm disasters in their efforts to (1) make resource allocation decisions, (2) make high-level planning decisions, and (3) raise public awareness of severe dust storm risk.     

Characteristics of Ion Components and Trace Elements of Fine Particles at Gosan, Korea in Spring time from 2001 to 2002

Size-segregated measurements of the composition of an aerosol are used to determine the transport of natural and anthropogenic aerosols to the Gosan site in springtime from 2001 to 2002. Although the transport of Asian dust is a well-known phenomenon in springtime, this study shows that not only is soil dust transported into Gosan each spring but so are anthropogenic aerosols, including sulfur, enriched trace metals such as Pb, Zn, Ni, K, S. This study also combines the size- and time-resolved aerosol composition measurements with isentropic, backward air-mass trajectories in order to identify some potential source regions of the anthropogenic aerosols. Finally, four types of transport episodes were identified: (1) anthropogenic pollutants, (2) dust storm mixed with the anthropogenic aerosols, (3) typical dust storms, (4) some sea salt with clean air mass. Overall, in addition to typical soil dust, a large amount of anthropogenic aerosols, whether mixed with the soil dust or not, are transported to Gosan each spring.     

利用激光雷达太阳光度计等多种遥感手段立体监测一次沙尘事件夏俊荣

利用位于北京以及河北香河的两台地基Mie散射激光雷达、星载激光雷达、太阳光度计以及颗粒物监测仪等一系列仪器对发生在2008年5月底的一次沙尘事件进行立体监测并分析.结果表明,这起较严重的沙尘是由蒙古国输送而来,影响范围很广,持续时间较长,有三次明显的峰值,对应三次沙尘的来袭;沙尘的每次来袭都对应有先升温后降温的现象,并伴随有相对湿度的急剧下降;沙尘入侵前北京香河两地以细粒子为主,入侵后代之以粗粒子为主.