环境空气中大气颗粒物源解析的研究进展

介绍了国内外用于大气颗粒物源解析研究的受体模型的进展情况，对受体模型的研究体系，测量分析技术、研究方法作了详细阐述，并对源解析近期的研究热点及发展趋势作了评述。     

大气环境质量分析与评价研究的新进展

简要地介绍了人工神经网络（ANN）、物元可拓集（MEES）、集对分析（SPA）、遗传算法（GA）和投影寻踪技术（PP）等的基本思想和特点，评述了近年来国内外将这些新理论和新技术应用于大气环境质量分析与评价取得的最新成果，指出了大气环境质量分析与评价研究的可能发展前景。     

基于指数标度法的大气污染物标准浓度限值

从韦伯—费希纳定律S＝KlogR出发,指出在大气污染物背景浓度限值C_ioo至明显危害浓度限值C_I∞范围内,当污染物浓度成等比变化时,人对污染物浓度刺激量的主观差别感觉成等差变化。应用＂等差分级、等比赋值＂的指数标度法计算出６种大气污染物的三级标准浓度限值与我国制定的《大气环境质量标准》,GB3095－82规定的污染物日平均浓度限值基本接近,为我国《大气环境质量标准》提供了合理依据。     

近地层氮氧化物和臭氧的区域分布研究

介绍了近地层氮氧化物和臭氧的区域分布研究方法,使用简化的区域尺度大气污染物传输模型和光化学反应模型,模拟计算了1990年中国主要城市排放氮氧化物的情景下,夏季(7月)主要城市的氮氧化物和相应的臭氧在近地层的浓度分布。      

我国大气环境监测质量控制及优化策略研究

随着各地雾霾等大气污染问题反复出现,各种复杂的大气环境质量问题开始在全球集中呈现。大气污染物在环流扰动之下已经开始了长距离传输,不再是过去单纯的点源污染,而是表现出了蔓延速度更加迅速、污染更加复杂的情况,加强大气环境监测工作刻不容缓。因此本文以大气环境质量现状为出发点,对目前我国大气环境质量监测中存在的问题进行了分析,并就此提出了完善我国大气环境质量监测工作的对策,希望能推动我国大气环境质量的进一步改善。     

大气磷干沉降采样方法对比分析

以四川农业大学成都校区为监测点,采用大气主动采样法(AA)、大气干表面法(ADS)及大气湿表面法(AWS)3种常用干沉降采集方法做大气磷干沉降通量对比试验。结果表明,3种采样方法获得的大气磷干沉降通量间具有显著的差异性及相关性(P0.05),三者间可以进行换算统一;AA法适用于较短采样周期的连续性监测研究,ADS法适用于较长采样周期(5 d)的监测研究,而AWS法更适用于在长采样周期(月)内选取一段时间作为干沉降监测的研究。     

A study of the atmospheric dispersion of a high release of krypton-85 above a complex coastal terrain, comparison with the predictions of Gaussian models (Briggs, Doury, ADMS4)

Atmospheric releases of krypton-85, from the nuclear fuel reprocessing plant at the AREVA NC facility at La Hague (France), were used to test Gaussian models of dispersion. In 2001-2002, the French Institute for Radiological Protection and Nuclear Safety (IRSN) studied the atmospheric dispersion of 15 releases, using krypton-85 as a tracer for plumes emitted from two 100-m-high stacks. Krypton-85 is a chemically inert radionuclide. Krypton-85 air concentration measurements were performed on the ground in the downwind direction, at distances between 0.36 and 3.3 km from the release, by neutral or slightly unstable atmospheric conditions. The standard deviation for the horizontal dispersion of the plume and the Atmospheric Transfer Coefficient (ATC) were determined from these measurements. The experimental results were compared with calculations using first generation (Doury, Briggs) and second generation (ADMS 4.0) Gaussian models. The ADMS 4.0 model was used in two configurations; one takes account of the effect of the built-up area, and the other the effect of the roughness of the surface on the plume dispersion. Only the Briggs model correctly reproduced the measured values for the width of the plume, whereas the ADMS 4.0 model overestimated it and the Doury model underestimated it. The agreement of the models with measured values of the ATC varied according to distance from the release point. For distances less than 2 km from the release point, the ADMS 4.0 model achieved the best agreement between model and measurement; beyond this distance, the best agreement was achieved by the Briggs and Doury models.     

Deposition of artificial radionuclides from atmospheric Nuclear Weapon Tests estimated by soil inventories in French areas low-impacted by Chernobyl

Soil inventories of anthropogenic radionuclides were investigated in altitudinal transects in 2 French regions, Savoie and Montagne Noire. Rain was negligible in these 2 areas the days after the Chernobyl accident. Thus anthropogenic radionuclides are coming hypothetically only from Global Fallout following Atmospheric Nuclear Weapon Tests. This is confirmed by the isotopic signatures (²³⁸Pu/^239+240Pu; ¹³⁷Cs/^239+240Pu; and ²⁴¹Am/^239+240Pu) close to Global Fallout value. In Savoie, a peat core age-dated by ²¹⁰Pb_ex confirmed that the main part of deposition of anthropogenic radionuclides occurred during the late sixties and the early seventies. In agreement with previous studies, the anthropogenic radionuclide inventories are well correlated with the annual precipitations. However, this is the first time that a study investigates such a large panel of annual precipitation and therefore of anthropogenic radionuclide deposition. It seems that at high-altitude sites, deposition of artificial radionuclides was higher possibly due to orographic precipitations.     

The sea–air exchange of mercury (Hg) in the marine boundary layer of the Augusta basin (southern Italy): Concentrations and evasion flux

The first attempt to systematically investigate the atmospheric mercury (Hg) in the MBL of the Augusta basin (SE Sicily, Italy) has been undertaken. In the past the basin was the receptor for Hg from an intense industrial activity which contaminated the bottom sediments of the Bay, making this area a potential source of pollution for the surrounding Mediterranean. Three oceanographic cruises have been thus performed in the basin during the winter and summer 2011/2012, where we estimated averaged Hg_atm concentrations of about 1.5 ± 0.4 (range 0.9–3.1) and 2.1 ± 0.98 (range 1.1–3.1) ng m⁻³ for the two seasons, respectively. These data are somewhat higher than the background Hg_atm value measured over the land (range 1.1 ± 0.3 ng m⁻³) at downtown Augusta, while are similar to those detected in other polluted regions elsewhere. Hg evasion fluxes estimated at the sea/air interface over the Bay range from 3.6 ± 0.3 (unpolluted site) to 72 ± 0.1 (polluted site of the basin) ng m⁻² h⁻¹. By extending these measurements to the entire area of the Augusta basin (∼23.5 km²), we calculated a total sea–air Hg evasion flux of about 9.7 ± 0.1 g d⁻¹ (∼0.004 t yr⁻¹), accounting for ∼0.0002% of the global Hg oceanic evasion (2000 t yr⁻¹). The new proposed data set offers a unique and original study on the potential outflow of Hg from the sea–air interface at the basin, and it represents an important step for a better comprehension of the processes occurring in the marine biogeochemical cycle of this element.     

大气污染扩散的高斯烟羽模型及其GIS集成研究

以VB6结合SuperMap Objects 5.2为开发平台,实现高斯烟羽模型与GIS的集成,可视化地表达大气污染物的扩散过程,并通过实例讨论了GIS与烟羽模型集成的方法、技术流程及其他相关问题.