成都市大气颗粒物源解析的PPR法

应用投影寻踪回归新技术(PPR),对成都市区大气采集样本中的元素含量数据和成都市大气颗粒物源成分谱进行分析,得到成都市大气颗粒物排放源的权重贡献率。结果表明:影响成都市大气颗粒物的主要贡献源为燃煤尘和土壤道路尘,它们的贡献率均达40%以上,与成都市区内大气污染来源的实际情况相符合。      

上甸子本底站地面臭氧变化特征及影响因素

利用TE Model 49C型臭氧监测仪,于2004年1月1日-12月31日,在上甸子本底站进行了地面φ(O₃)的连续在线监测.分析了全年φ(O₃)的变化特征及其与同期气象要素的相关关系,并对φ(O₃)高值日的个例分析进行了验证.结果表明,上甸子本底站地面φ(O₃)具有明显的季节变化和日变化规律,并且与同期的气象条件密切相关.主要特征:①夏初φ(O₃)较高,6月的平均值达到最高,小时平均最大值可达129.7 μL/m3;而冬季φ(O₃)较低,12月的平均值达到最低,小时平均最大值仅为32.7 μL/m3.②日变化趋势较为明显,在4:00-7:00出现最低值,在15:00-18:00出现最高值,变化幅度为夏季最大、冬季较小.③气温与φ(O₃)呈显著正相关,夏季相对湿度与φ(O₃)呈显著负相关,风向和辐射强度也与φ(O₃)及其变化规律呈显著相关关系.      

抚顺市大气环境质量及其对策研究

利用环境空气污染综合指数法分析抚顺市大气环境质量监测数据.结果表明:ρ(TSP)年日均值为0.255 mg/m3,超过国家环境空气质量二级标准,超标0.3倍;ρ(SO₂)年日均值为0.034 mg/m3,ρ(NO₂)年日均值为0.035 mg/m3,ρ(CO)年日均值为1.42 mg/m3,均达到国家环境空气质量二级标准.同时也得出各功能区的污染状况、主要污染物特征以及贡献率,从而提出相应的解决方案和对策,为改善抚顺市大气环境质量提供科学依据.      

沙尘暴事件中大气颗粒物化学组分的浓度变化和硫酸盐的形成

应用电感耦合等离子体原子发射光谱、质谱和离子色谱分析了2002年3月28日-4月8日在山东长岛县采集的共11对粗、细大气颗粒物样品的化学组成,探讨4月6-8日沙尘暴事件中大气颗粒物化学组分的变化和硫酸盐的形成.沙尘暴事件应区分前锋和后续部分,前锋与大气中各种污染物相互作用,具有硫富集的特征.后续部分较好地保持了长距离传输风沙尘本身的特征.硫酸盐的形成机理可能是多相氧化而不是简单的酸碱中和.硫酸铵是首先生成的含硫物种,这是细颗粒主导的形成过程.硫酸铵逐渐转化为其他硫酸盐,硫的成分也逐渐向粗颗粒转移.在沙尘暴事件中含硫污染物不但有一个从气相向颗粒物转变的过程,也有一个从细颗粒向粗颗粒转化的过程.      

大气气溶胶中有机成分研究进展

有机物是大气气溶胶的重要组成部分,尤其是在细颗粒中,可占其干重的10%～70%。由于有机气溶胶的健康及气候效应,有机物的组成、源分布、颗粒行为等的研究越来越受到人们的重视。其中,有机物成分的鉴别和定量已成为近年来的研究热点。在分析中,就目前有机气溶胶的采样、有机成分提取、分离及定性、定量分析方法进行了综述,并比较了各种方法的优缺点。     

克拉玛依市区大气尘污染研究

通过对克拉玛依市区大气尘污染的特性及变化规律所进行的全面分析和研究,结果表明：市区的尘污染有加重的趋势,降尘属中度污染,针对现状,提出了大力植树造林;加强对建筑施工和道路改造施工现场的管理;加强对低空排放的小型燃煤锅炉的监督管理;充分利用石油天然气资源;强化以环境管理为中心的环境政策体系等五项具体措施。     

我国大气腐蚀研究进展

总结了近几年来我国在大气腐蚀方面的研究现状和进展,尤其是国产、常用、量大、面广的4大类材料在我国9类主要典型大气环境下的腐蚀数据;各类典型材料在典型环境下的大气腐蚀行为规律;大气环境因素对材料大气腐蚀的影响;碳钢、低合金铜大气腐蚀行为预测.特别是在根据8年试验结果所总结出的大气腐蚀速度与试验时间之间具有幂函数关系的基础上,又进一步建立了腐蚀速度与合金元素之间的数学模型关系;探讨了采用ACM技术评估大气腐蚀严酷性;初步建立了大气腐蚀数据库,并进一步采用计算机发展网络查询服务系统,实现科学数据共享;经过20余年的研究,撰写并出版了中国材料自然环境腐蚀专著中的大气腐蚀篇,研制和生产了经济耐候钢.     

Exploratory Analysis of the Winter Chemistry of Five Lakes on the North Slope of Alaska1

Abstract: Lakes are important water resources on the North Slope of Alaska. Freshwater is required for oilfield production as well as exploration, which occurs largely on ice roads and pads. Since most North Slope lakes are shallow, the quantity and quality of the water under ice at the end of winter are important environmental management issues. Currently, water‐use permits are a function of the presence of overwintering fish populations, and their sensitivity to low oxygen concentrations. Sampling of five North Slope lakes during the winter of 2004‐2005 shed some light on the winter chemistry of four lakes that were used as water supplies and one undisturbed lake. Field analysis was conducted for oxygen, conductivity, pH, and temperature throughout the lake depth, as well as ice thickness and water depth. Water samples were retrieved from the lakes and analyzed for Na, Ca, K, Mg, Fe, dissolved‐organic carbon, and alkalinity in the laboratory. Lake properties, rather than pumping, were the best predictors of oxygen depletion, with the highest dissolved‐oxygen levels maintained in the lake with the lowest concentration of constituents. Volume weighted mean dissolved‐oxygen concentrations ranged from 4 to 94% of saturation in March. Dissolved oxygen and specific conductance data suggested that the lakes began to refresh in May.     

Using Lichen Chemistry to Assess Airborne Tungsten and Cobalt in Fallon, Nevada

This paper describes the use of lichen chemistry to assess airborne tungsten and cobalt in Fallon, Nevada, where a cluster of childhood leukemia has been on going since 1997. Lichens and their rock substrates were collected from Rattlesnake Hill within Fallon as well as from four different rock outcrops located north, east, south, and west of Fallon and at least 20 km away from the town center. In the lichens themselves, W and Co are significantly higher within Fallon than in the combined control site outside of Fallon. In the rock substrates of the lichens, no differences exist in W and Co. The W and Co differences in lichens cannot be attributed to substrate geochemistry. Fallon is distinctive in west central Nevada for high airborne W and Co, and given its cluster of childhood leukemia, it stands to reason that additional biomedical research is in order to test directly the leukogenicity of combined airborne W and Co.     

Long term changes in atmospheric N and S throughfall deposition and effects on soil solution chemistry in a Scots pine forest in the Netherlands

In a Scots pine forest the throughfall deposition and the chemical composition of the soil solution was monitored since 1984. (Inter)national legislation measures led to a reduction of the deposition of nitrogen and sulphur. The deposition of sulphur has decreased by approximately 65%. The total mineral-nitrogen deposition has decreased by ca. 25%, which is mainly due to a reduction in ammonium-N deposition (−40%), since nitrate-N deposition has increased (+50%). The nitrogen concentration in the upper mineral soil solution at 10 cm depth has decreased, leading to an improved nutritional balance, which may result in improved tree vitality. In the drainage water at 90 cm depth the fluxes of NO₃⁻ and SO₄²⁻ have decreased, resulting in a reduced leeching of accompanying base cations, thus preserving nutrients in the ecosystem. It may take still several years, however, before this will meet the prerequisite of a sustainable ecosystem.