首页|气团来源和云雾过程对华南高山背景区亚微米气溶胶数谱分布的影响

气团来源和云雾过程对华南高山背景区亚微米气溶胶数谱分布的影响

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在南岭国家大气背景站(南岭站,海拔1690m)采用扫描电迁移率粒径谱仪(SMPS)对亚微米气溶胶的数浓度及粒径谱分布进行了观测。结合同期常规污染和气象数据,分析了不同来源气团与气象条件下气溶胶数谱分布的特征,探讨了典型云雾天气条件下气溶胶数浓度及谱分布的变化规律。研究结果表明:观测期间南岭站气溶胶的平均数浓度为1。14×103个/cm3,低于国内外大多数高山背景站,云雾天气多是造成南岭站气溶胶数浓度低的重要原因;气溶胶主要以爱根核模态和积聚模态为主,二者占总数浓度超过95%;气溶胶数浓度呈现下午高于上午的规律,峰值出现在下午14:00时左右。在途径珠三角的南部气团(占比66。2%)和途径湖南地区的北部气团(占比33。8%)影响下的气溶胶数谱分布均为双峰模态,但南部气团影响下的气溶胶数浓度约是北部气团(7。9×102个/cm3)影响下的2倍,且40~300nm粒径段的粒子数浓度明显升高。云雾时段的核模态和积聚模态气溶胶数浓度明显低于非云雾时段,总气溶胶数浓度下降幅度可达80%,说明云雾对气溶胶具有明显的清除作用;云雾发展过程中,气溶胶数浓度粒径分布变化规律呈现双峰型-单峰型-双峰型,谱宽不断收窄,且峰值粒径逐渐减小。
Effects of air mass sources and fog event on the number spectrum distribution of submicron aerosols over the alpine background area in South China
To improve our understanding of the physical and chemical characteristics of aerosols in the background atmosphere in South China,the Scanning Mobility Particle Sizer(SMPS)were applied for the first time to measure the number concentration and particle number size distributions(PNSD)of submicron particulate matter(PM)at the Nanling National Atmospheric Background Station(Nanling site,1690m a.s.l.).Concurrently,the characteristics of PNSD under different sources of air mass and meteorological conditions along with variations in both the aerosol number concentration and the PNSD during a typical fog event were evaluated.Our results show that the average particle number concentration at the Nanling site was 1.14×103cm-3,being lower than most of the domestic and international mountainous background sites and exhibiting a relatively clean atmosphere;and the average particle number concentration was higher in the afternoon than in the morning with a peak concentration at around 2pm.During the observation period,the station was mainly influenced by the southern air masses(66.2%)originating from the South China Sea passing through the Pearl River Delta megacities,and the northern air masses(33.8%)passing through Hunan Province.The PNSD under the southern and northern air masses exhibited bimodal distributions,but the average aerosol number concentration from the southern air masses was twice that from the northern air masses(7.9× 102cm 3),and the number concentration of particles within a range of 40-300nm increased significantly.The number concentrations of aerosols in the Nuclear mode and Accumulation mode were 80%lower under the foggy weather than under non-foggy weather,showing an obvious aerosol scavenging effect of fog;During the development of a fog event,the PNSD evolved from bimodal to unimodal,then to bimodal,demonstrating that the spectral width narrowed and the peak value of aerosol number concentration shifted towards smaller particle sizes.In general,the aerosols were mainly present in Nuclear mode and Accumulation mode(the two account for more than 95%of the total concentration),and the low aerosol number concentration was mainly attributed to the frequent foggy weather at Nanling Station.

Nanling mountainsNational Atmospheric Background Stationfine particlessize distributionair mass transportfog

周淑婷、龚道程、张诗炀、张庆祖、王文路、刘小婷、张涛、周炎、王伯光、陈多宏、王好

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暨南大学环境与气候研究院,广东广州 511443

南岭森林大气环境与碳中和野外科学观测研究站,广东广州 511443

台湾"中央研究院"环境变迁研究中心,台湾台北11529

暨南大学附属第一医院眼科,广东广州 510630

广东省生态环境监测中心,国家环境保护区域空气质量监测重点实验室,广东广州 510308

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南岭 国家背景站 细颗粒物 粒径谱 气团传输

国家自然科学基金面上项目广东省科技厅科技创新平台类项目资金资助

418773702019B121202002

2024

中国环境科学
中国环境科学学会

中国环境科学

CSTPCDCHSSCD北大核心
影响因子:2.174
ISSN:1000-6923
年,卷(期):2024.44(1)
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