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庐山三级分档雾水化学特征的对比分析
引用本文:张鸿伟,樊曙先,胡春阳,朱丹丹,康博识.庐山三级分档雾水化学特征的对比分析[J].中国环境科学,2019,39(11):4589-4598.
作者姓名:张鸿伟  樊曙先  胡春阳  朱丹丹  康博识
作者单位:1. 南京信息工程大学, 大气环境与装备技术协同创新中心, 中国气象局气溶胶与云降水重点开放实验室, 江苏 南京 210044;2. 南京信息工程大学大气物理学院, 江苏 南京 210044;3. 中国人民解放军94582部队 确山 463217;4. 辽宁省气象装备保障中心, 辽宁 沈阳 110000
基金项目:国家重点研发计划项目(2018YFC1507905);国家自然科学基金资助项目(41675132;41775134;41675136)
摘    要:为研究庐山冬季不同粒径雾滴化学成分特征,于2015年和2016年在庐山开展冬季云雾物理化学特征的很高综合观测实验,利用主动式分档雾水采集器(three-stage CASCC)共采集44组3级粒径雾滴的雾水样品,其分档空气动力学直径为4~16μm(S3级),16~22μm(S2级)和>22μm(S1级).用850professional IC型色谱仪(瑞士万通)分析雾水中的水溶性离子浓度,讨论3级分档雾水化学特征和不同粒径雾水中各离子组分的来源及相关性.结果表明,2015年和2016年庐山冬季3级雾水多呈酸性,2016年酸性更强,pH值与雾滴的粒径大小有依赖性关系,4~16μm的小雾滴酸性更强.雾水中主要离子有Ca2+,NH4+,SO42-,NO3-和Cl-.NH4+,SO42-,NO3-主要集中在4~16μm的小雾滴中,受海洋和土壤源的影响比较小,主要是人为活动所导致,2015年雾水Cl-主要受人为源的影响,2016年人为输入显著降低,主要受海洋源影响.Mg2+,Ca2+主要集中在>22μm的大雾滴中.SO2、NOx排放逐年降低导致2016年雾水中SO42-和NO3-浓度明显小于2015年.

关 键 词:庐山  三级分档雾水  化学特征  
收稿时间:2019-04-16

Comparative analysis of the chemical properties of the three-stage fog water in Mount Lushan
ZHANG Hong-wei,FAN Shu-xian,HU Chun-yang,ZHU Dan-dan,KANG Bo-shi.Comparative analysis of the chemical properties of the three-stage fog water in Mount Lushan[J].China Environmental Science,2019,39(11):4589-4598.
Authors:ZHANG Hong-wei  FAN Shu-xian  HU Chun-yang  ZHU Dan-dan  KANG Bo-shi
Institution:1. Key Laboratory for Aerosol Cloud Precipitation of China Meteorological Administration, Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science and Technology, Nanjing 210044, China;2. Department of Atmospheric Physics, Nanjing University of Information Science and Technology, Nanjing 210044, China;3. Unit 94582 of PLA, Queshan, 463217, China;4. Liaoning Meteorological Equipment Support Center, Shenyang 110000, China
Abstract:In order to investigate the physical and chemical properties of fog water in Mount Lushan, comprehensive observations were carried out during the wintertime of 2015 and 2016. A three-stage Caltech Active Strand Cloud Collector (CASCC) was used to collect the fog droplets within three size ranges (4~16μm, 16~22μm and >22μm), and in total 44 samples were obtained during the observations. Concentrations of cations and anions in each sample were also measured by using Ion Chromatography instrument. We then analyzed the correlation between the ions in each stage as well as the sources of these ions. The composition and the chemical characteristics of the fog water were also given. The results showed that the fog water in 2015 and 2016 was mostly acidic, while the pH value is lower in 2016. A correlation between the pH value and the droplet size was also found, showing a stronger acidity for smaller droplets. The major ions found in fog water were Ca2+, NH4+, SO42-, NO3- and Cl-. NH4+, SO42-, NO3- mostly reside in small droplets, and they are strongly influenced by the human activities instead of the natural sources such as ocean and soil. It is interesting to find that Cl- in 2015 was mainly affected by anthropogenic sources while in 2016 they were influenced by marine sources due to a significant reduction of the human inputs. Moreover, Mg2+ and Ca2+ were found mostly concentrated in large droplets. Due to the decrease of SO2 and NOx emission, the concentrations of SO42- and NO3- in fog water in 2016 were found remarkably lower than those in 2015.
Keywords:Mount Lushan  three-stage fog water  chemical properties  
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