2022年青岛市沿海区域臭氧污染特征及传输影响分析

基于2022年1—12月青岛市沿海区域臭氧（O₃）自动监测数据和气象观测资料,对O₃污染变化特征及影响因素进行了分析,结合后向轨迹聚类与潜在源区分析等方法,对O₃外来输送通道及潜在源分布情况进行分析研究。结果表明：青岛市沿海区域O₃污染主要集中在4—10月份,日变化特征呈单峰单谷趋势,峰值出现在15：00—16：00;气象因素中,地面短波辐射对O₃浓度变化的相对贡献最大,偏南风易导致O₃污染;受二氧化氮（NO₂）滴定作用以及海陆风转换影响,沿海区域O₃峰值与谷值均滞后青岛城区1 h左右;O₃生成整体处于VOCs控制区,1-丁烯、正丁烷与异戊烷是O₃污染期间导致O₃浓度上升的关键组分;O₃污染的主要潜在源区为长三角北部和黄海近岸海域,以及山东中南部地区。     

云南省臭氧污染特征及气象影响分析

为研究云南省臭氧(O₃)污染特征及其与气象因子的关系,基于统计学方法及ArcGIS空间差异分析、线性趋势分析、空间离散系数等方法,对全省16个市(州)2015—2017年33个环境监测站点的监测数据进行了研究。结果表明:研究期间,O₃逐渐取代其他大气常规污染物成为首要污染物,其浓度变化范围为19～138 μg/m³。云南省各市(州)O₃浓度年变化呈现周期性,月度峰值集中出现在春季(3—5月);日变化呈单峰形,峰值集中在14:00—17:00。O₃浓度的空间格局由纵向集聚为主转变为横向集聚为主,各集聚区交错分布,低值区由西北部转移到西南部;O₃浓度增长率为正的区域集中于东北部和中部,面积约为20.81万km²,占全省总面积的54.29%,其余半环状区域增长率为负。迪庆州O₃污染情况与其他市(州)明显不同,且受其他市(州)传输的影响较小。气象因子对O₃浓度的影响随时间和地域条件的变化而变化,对典型市(州)(迪庆州、丽江市、昭通市)O₃浓度影响最大的为偏南风,影响的浓度区间为20～160 μg/m³。     

2013—2016年74城市臭氧浓度变化特征

利用2013—2016年74城市臭氧（O₃）监测数据,综合探讨了全国74城市O₃浓度时空变化特征、变化趋势。结果表明：2013—2016年,74城市O₃-8 h各百分位浓度总体呈上升趋势,且百分位较高区间O₃浓度逐年上升速率越快,O₃-8 h第95百分位浓度年增长5.3 μg/m³,其次是第90百分位;O₃区域性污染特征明显,京津冀及周边、长三角、珠三角O₃污染问题突出;74城市O₃浓度超标天数年增长3 d/城市,O₃污染呈明显日、季节变化特征,午后14：00—17：00达到小时浓度峰值,超标日主要集中于5—10月;O₃对环境空气质量综合指数贡献率逐年增加,北京、上海和广州O₃贡献率年增长分别为1.9%、1.1%和0.8%。     

基于Matlab小波分析的南京北郊大气O3浓度变化特征研究

以2008年南京北郊大气中O₃ 质量浓度观测资料和常规观测资料为基础,利用Matlab小波分析工具,对O₃浓度的年时间序列进行分析,得出该地区的O₃ 日均浓度的变化特征：春、夏季节O3浓度大于秋、冬季节,最高浓度出现在春末夏初,最低浓度出现在冬季;并且全年共有5个突变点;弱高压的天气系统、较高的温度、较低的湿度和晴朗少云的天气是造成南京北郊O₃浓度突变的主要气象因素。结合HYSPLIT气流后向轨迹模拟,对污染源来源进行追踪,结果表明：南京北郊O₃高浓度污染来源主要分为本地局地污染和外来污染物输送两类;垂直方向上,O₃的区域尺度或中尺度的输送主要稳定在混合层的底层。     

江苏省2014-2016年臭氧污染区域特征分析

分析2014—2016年江苏省O₃污染状况,以及苏北、苏中和苏南3个典型区域O₃年度、季度、日变化和频度占比等分布特征。结果表明,江苏省的O₃空间分布呈现北低南高,2014—2016年的O₃超标占比由18.4%上升至34.9%;2016年苏北、苏中和苏南地区O₃-8h第90百分位数与2014年相比,上升2.7%,21.8%和3.3%;3个区域夏季O₃-8h均值最高,春、秋2季次之,冬季最低;O₃-1h日变化呈单峰状态,最低值出现在06:00—07:00,最高值出现在15:00—16:00;2016年3个地区的O₃频度占比均呈正态分布,主要集中在40~80 μg/m³,所占比例均>15%;苏中和苏南区域2016和2014年相比O₃频率占比的变化幅度较大,苏北地区变化幅度不大。指出,江苏省的O₃污染程度在逐年提高,污染范围从苏南逐渐往中部和北部城市扩大。     

三亚市臭氧污染特征、输送路径及潜在源区分析

基于2015-2019年三亚市空气质量自动监测数据和气象观测资料,结合后向轨迹聚类与潜在源区分析等方法,分析了三亚市O₃污染特征。结果表明:2015-2019年三亚市O₃浓度总体优良,优良天数比例为97.9%(标准状态),超标天均为轻度污染,多发生在秋冬季。O₃浓度与平均相对湿度、气温和降水量呈负相关关系,与平均风速呈正相关关系,同时与风向密切相关。6-8月气温较高,主导风向为偏南风,O₃及其前体物以本地排放为主,O₃浓度较低;秋冬季盛行东北风,易受到来自内陆的污染传输影响,O₃浓度相对较高。当日最高气温为20~30℃、日均相对湿度为65%~85%、日均风速为3~8 m/s、主导风向为东北风时,三亚市发生O₃超标的概率较高。台风外围和冷高压南下是导致三亚市O₃超标的2种典型天气形势。经聚类分析得到,2019年2个污染过程气团输送路径均来自东北方向,潜在源区分析WPSCF与WCWT的高值区一致性较好,均表明珠三角地区是三亚市重要的O₃污染潜在源区,需要加强与珠三角地区O₃污染的联防联控。     

宜都市PM2.5与O3季节性分布特征及潜在源区分析

为了解宜都市PM_2.5与O₃的污染特征及潜在来源,利用宜都市2020年3月至2022年2月在线监测数据及气象数据,对宜都市PM_2.5与O₃质量浓度变化特征、气象影响因素及潜在源区进行了分析,结果表明:宜都市PM_2.5质量浓度冬高夏低,日变化呈双峰特征,O₃质量浓度夏高冬低,日变化呈单峰特征。高湿、静稳的气象条件以及较强偏北风作用下的区域污染传输对PM_2.5污染有重要影响,高温以及中湿度对O₃污染过程有重要作用。春、夏、秋季偏南方向气流轨迹占主导,且携带较高的污染物浓度,冬季来自湖北东北及西南方向的气流占比较高且携带的PM_2.5浓度较高;宜都市PM_2.5、O₃的潜在源区具有季节性差异,总体来看,主要分布在河南南部、湖北东部及湖南的北部区域。     

“十三五”期间赣州市环境空气质量特征及变化趋势

为科学谋划赣州市“十四五”期间大气污染防治工作,重点对赣州市“十三五”期间整体空气质量变化情况,以及影响赣州市优良天数的两个重要参数——臭氧(O₃)和细颗粒物(PM_2.5)的污染规律进行了分析。结果表明,赣州市“十三五”期间空气质量改善明显,优良天数整体增加。O₃浓度和O₃超标天数占总污染天数的比例整体均呈现波动上升趋势,对空气质量综合指数的贡献率逐年增加;高浓度O₃污染通常发生在干燥、高温条件下,高发期主要集中在4—5月和7—11月,空间分布呈西高东低的特点,与2018年大气污染源排放清单中挥发性有机物(VOCs)的排放量分布情况较为一致。PM_2.5浓度呈逐年下降趋势,在2019年和2020年达到国家空气质量二级标准;PM_2.5污染天数在2016年同比增加26 d,而后逐年减少,其中2020年较2015年减少了12 d;PM_2.5浓度的季节变化特征整体呈现为冬季高、春秋次之、夏季低,空间分布特征与O₃类似。建议赣州市在“十四五”期间以PM_2.5和O₃协同治理为主要思路,继续深入打好蓝天保卫战。     

山东省O3污染概况及预报效果评估

对山东省各市2018—2021年的O₃污染特征进行了分析,并对2021年5—9月O₃污染较重月份空气质量模型的O₃预报结果进行了分析评估。结果表明:山东省2018—2021年O₃-8 h第90百分位数(O₃-8 h-90per)先升高后降低,O₃污染呈现波动变化,污染月主要集中在5—9月,并呈现内陆高、沿海低,中北部高、南部低的空间分布特征。集合预报模式对O₃模拟效果最好,预测结果与O₃监测值的相关性最大、偏差最小,但较难预测出O₃的峰值浓度,易漏报O₃重度污染。WRF-Chem、CMAQ、CAMx、NAQPMS对O₃的模拟效果比集合预报稍差,CMAQ、CAMx存在系统性偏低的情况,但对优级别的模拟效果明显好于其他模式;WRF-Chem、NAQPMS存在系统性偏高的情况,WRF-Chem能较好地模拟出O₃超标日,对中度、重度日的24h级别准确率分别达94.08%、100%,对O₃超标预报尤其是中至重度污染的预测预报有重要指导意义。     

内蒙古近地面臭氧污染时空分布特征及气象条件分析

使用2018—2020年内蒙古臭氧(O₃)、气象要素观测资料和NCEP FNL资料,统计分析内蒙古近地面O₃质量浓度的时空分布特征和变化趋势,并针对全区O₃污染典型个例分析其天气形势和气象要素的影响作用。结果表明:内蒙古2018—2020年O₃质量浓度年评价值呈逐年下降趋势,2020年较2018年下降10.3%,各盟市O₃超标率也显著降低,仅赤峰市和通辽市略微上升。内蒙古O₃质量浓度高值分布在中西部偏南地区,尤其是乌海市和鄂尔多斯市;O₃超标率峰值主要出现在5—7月,周末效应存在东西部差异。O₃浓度变化和天气形势关系密切,南部暖平流和暖高压控制有利于O₃生成,西北部冷平流和冷涡发展使得O₃浓度下降;高温、低湿、微风和较高的能见度均为诱发O₃污染的重要气象条件,而西北大风通过降低温度、能见度和易于扩散的风向使得内蒙古O₃浓度降低,但同时可能会导致PM₁₀污染。     

Dissipation and residue of metalaxyl and cymoxanil in pepper and soil

A simple and accurate method of determining metalaxyl and cymoxanil in pepper and soil was developed by ultra-performance liquid chromatography–photodiode array detection. The limits of detection were 0.015 mg/kg for metalaxyl and 0.003 mg/kg for cymoxanil. The limits of quantification were 0.05 mg/kg for metalaxyl in pepper and soil as well as 0.01 mg/kg for cymoxanil in pepper and soil. Recoveries of pepper and soil were investigated at three spiking levels and ranged within 77.52 to 102.05 % for metalaxyl and 87.15 to 103.21 % for cymoxanil, with relative standard deviations below 9.30 %. For field experiments, the half-lives of metalaxyl were 3.2 to 3.9 days in pepper and 4.4 to 9.5 days in soil at the three experimental locations in China. At harvest, pepper samples were found to contain metalaxyl and cymoxanil well below the maximum residue limit MRLs of the European Union (EU) following the recommended dosage and the interval of 21 days after last application.     

我国沙尘暴灾害及其治理对策初步研究

分析研究了沙尘暴的成因、时空分布、发展趋势及造成的灾害,结合国外经验提出了我国治理的对策建议。     

Determination and study on dissipation and residue of bismerthiazol and its metabolite in Chinese cabbage and soil

A simple and accurate method for the determination of bismerthiazol and its metabolite 2-amino-5-mercapto-1,3,4-thiadiazole was developed in Chinese cabbage and soil by high-performance liquid chromatography-diode array detection in this study. The limits of detection were 0.06 mg/kg for bismerthiazol and 0.03 mg/kg for 2-amino-5-mercapto-1,3,4-thiadiazole, respectively. Recoveries of cabbage and soil were investigated at three spiking levels and were in the range of 84.0–96.0 % for bismerthiazol and 71.0–74.6 % for 2-amino-5-mercapto-1,3,4-thiadiazole, with relative standard deviations below 7.0 %. For field experiments, the half-life of bismerthiazol was 2.4–2.5 days in Chinese cabbage and 2.5–4.8 days in soil at the two experimental locations in China. Dissipation residues of 2-amino-5-mercapto-1,3,4-thiadiazole were lower than 0.72 mg/kg. Terminal residues of bismerthiazol and its metabolite were less than 3.0 and 0.3 mg/kg in Chinese cabbage, respectively. No bismerthiazol or metabolite residues were detected in soil on days 5, 7, 10, and 14 after the last spraying at the two dosage levels.     

新疆室内环境污染监测和治理工作现状与建议

针对目前室内环境监测工作出现的种种问题,就如何规范的开展室内环境监测工作,更好地为社会提供真实、准确、有效的监测数据,本文提出相关的探讨。     

Residues and dissipation of trifloxystrobin and its metabolite in tomatoes and soil

A simple residue analytical method using the quick, easy, cheap, effective, rugged, and safe (QuEChERS) procedure for the determination of trifloxystrobin and its metabolite trifloxystrobin acid (CGA321113) in tomato and soil was developed using high-performance liquid chromatography-tandem mass spectrometry (HPLC-MS/MS). The limits of detection were 0.0005 mg/kg for trifloxystrobin and 0.001 mg/kg for trifloxystrobin acid, respectively. The average recoveries in tomato and soil ranged from 73–99 % for trifloxystrobin and 75–109 % for trifloxystrobin acid, with relative standard deviations below 15 %. The method was then used to study the dissipation and residues in tomato and soil. The dissipation half-lives of trifloxystrobin in tomato were 2.9 days (Beijing) and 5.4 days (Shandong), while in soil were 1.9 days (Beijing) and 3.0 days (Shandong), respectively. The final results showed that the major residue compound was trifloxystrobin in tomato whereas it was its metabolite, trifloxystrobin acid, in soil. The final residues of total trifloxystrobin (including trifloxystrobin acid) were below the EU maximum residue limit of 0.5 mg kg^?1 in tomato 3 days after the treatment.     

太原市冬、夏季醛酮化合物污染特征及来源分析

针对太原市空气臭氧污染较为严重的问题,开展臭氧主要前体物醛酮化合物质量浓度及其变化规律研究.利用2,4-二硝基苯肼固相吸附/高效液相色谱方法,通过对太原市2019年冬季和夏季大气的醛酮化合物进行分析,发现太原市冬季总醛酮化合物的平均质量浓度为13μg/m3,低于夏季的27μg/m3.其中甲醛、乙醛和丙酮质量浓度最高,且...     

Lake destratification and speciation of iron and manganese

A long-term study of the effect of artificial aeration (destratification) of a water storage dam upon the speciation of iron and manganese in the dam waters has been undertaken. Separation of dam samples into soluble and insoluble forms by selective membrane filtration was undertaken before using the techniques of EPR spectroscopy, ion chromatography and gel filtration to assess the speciation of soluble species, and selective extraction and surface analysis (ESCA, SIMS and SEM) techniques to determine the speciation of particulate iron and manganese species. The percentages of soluble iron and manganese before (1983–85) and after (1986–88) artificial aeration are compared for the periods Jan–Dec, Jan–Mar, and Jun–Aug at three depths 6 m, 15 m and 0.5 m above the dam base, to assess the importance of seasonal changes in the various depths of the dam. Although aeration had an initial marked reduction in levels of soluble iron and manganese at all depths of the dam, the concentrations of these mtals showed a steady increase over succeeding years. Analysis of the figures over summer and winter periods shows that the reduction of soluble iron was maintained in summer, but not during winter. Upon aeration, the initial reduction of soluble manganese concentration was maintained in succeeding years in the epilimnic regions of the dam, but not in the hypolimnion. Statistical analysis of data has been undertaken to correlate the changes in relationship between the various forms of iron and manganese with the advent of aeration.     

Disembodied and Disembedded? The Social and Economic Implications of Atmospheric Change and Biodiversity

The social and economic implications of atmospheric change on biodiversity need to be seen in a global context of major shifts in the conceptualization and management of our relationship with nature. Traditionally, we have conceptualized the atmosphere and the other creatures of the biosphere as separate from the human, but their quasi-autonomy is now becoming subject to more and more human management. This raises not only economic issues, but social, political, and ethical concerns that will have substantial influence on public policy. Among these are the commodification of genetic material; the privatization of traditional knowledge; and the management of information. In this broader context, the paper examines an array of current and proposed strategies of response to changes in biodiversity as a result of climatic and other stresses.     

Atmospheric Change and Biodiversity: Co-Networks and Networking

Canada responded to the Global Biodiversity Convention by completing the Canadian Biodiversity Strategy in 1995. At the same time, Environment Canada also completed a national Science Assessment on Biodiversity. During this period, the Smithsonian Institution, in partnership with Parks and Environment Canada, initiated the implementation of a global biodiversity monitoring program in Canada. Under the auspices of the United Nations Man and the Biosphere Program, the SI/MAB monitoring protocols and plots have spread across Canada at an unprecedented rate. National champions in the science and educational sectors, working within an inter-disciplinary ecological framework, have guided the development, education, quality control and sharing of atmosphere-biodiversity observations electronically.Atmospheric-Biodiversity Networks and Networking have traditionally operated within separate mandates with little degree of integration. Air-Bio Networks were designed within an integrated framework to better understand the atmospheric stress on biodiversity and the adaptation actions, nationally and regionally. Detailed examples of the cumulative effects of climate change, stratospheric ozone depletion, acid deposition, ground-level ozone, suspended particulate matter and hazardous air pollutants on biodiversity will be discussed using a Southern Ontario case study. In addition, recommendations will be presented for future paired SI/MAB plots, linked networks and networking for adaptation within the context of climate, chemical and ecological gradients.