海洋酸化与重金属、有机污染物和人工纳米颗粒的联合毒性效应研究进展

由于大量人类活动的影响,大气CO_2浓度持续增加,其中约1/3被海洋吸收,导致表层海水pH值降低和碳酸盐平衡体系波动,即"海洋酸化"现象。污染物的海洋环境效应一直是全球环境科学领域研究的热点。在实际环境中,海洋酸化往往与污染物共同存在并作用于海洋生态系统,且海洋酸化极有可能改变污染物的海洋环境行为从而影响其毒性效应。但现有研究大多针对海洋酸化或者污染物单独作用下的毒性效应展开,对海洋酸化与污染物的联合毒性效应的研究不足、亟待加强。为此,综述了近年来海洋酸化与典型污染物(重金属、有机污染物)及新型污染物(人工纳米颗粒)的相关文献,重点阐述了海洋酸化对污染物环境行为的影响和海洋酸化与污染物对海洋生物的联合毒性效应,指出当前的研究不足,并对未来的研究方向进行了展望。     

煤烟型复合污染物相互作用与转移过程及其特点

粉尘,ＳＯ２,ＮＯｘ等的煤烟型复合污染是我国尤其是南方我的主要类型。本文根据实验观测,详细分析了主要污染物间的相互作用过程及其复污染物从产生,转移至植物界面的运动过程及其特点。     

中国水环境非点源污染负荷的估算研究

中国已占水环境容量中,除了点源污染以外,非点源污染也占有相当比重,非点源污染负荷的定量化研究势在必行.国外对非点源污染的研究开始较早,成果也较成熟.从20世纪80年代以来,中国也逐渐认识到非点源污染的存在及其危害性,开始了非点源污染的控制研究.但是中国对非点源污染问题的研究现在尚处于初级阶段,多为借鉴国外模型.文章分析了国内外对非点源污染的研究方法和研究现状,介绍了适合中国国情的非点源污染负荷估算的方法,包括流域水文估算法、大尺度区域中非点源污染负荷估算的方法.     

生物难降解有机污染物微生物处理技术的进展

耗氧有机污染物的微生物处理技术已日趋完善，研究重点转向生物难解污染物处理，文章详细阐述了几种生物难降解污染物微生物处理技术的研究进展：（１）几种污染物的高效降解微生物的分离培养以及这些高效降解微生物的降解效率和最佳降解条件研究。（２）利用微生物共代谢作用降解污染物的研究，为一些难以作为微生物唯一碳源和能源的污染物生物降解提供一条有效的途径；（３）利用基因工程技术创建高效降解菌的研究，该项技术在提高     

光氧化吸附矿井水中微量有机物试验研究

针对目前煤矿矿井水资源化过程中存在有机污染物的问题，考察了采用紫外光氧化分解的机理及影响因素。结果表明：紫外光对矿井水中有机物（主要是乳化油）有一定的氧化分解能力，能有效地促使有机物大分子破裂，有利于活性炭的吸附处理。在合理的工艺条件下，可使水中有机物去除率达到95%以上。     

我国一些城市污泥中多环芳烃(PAHs)的研究

应用GC／MS对我国内地和香港地区共11个城市污泥中的17种多环芳烃化合物（PAHs）进行了研究，各城市污泥中∑PAHs的含量在2．271－143．804mg/lg之间，依次为兰州污泥＞珠海污泥＞北京污泥＞广州污泥＞佛山污泥＞无锡污泥＞沙田污泥（香港）＞元朗污泥（香港）＞大埔污泥（香港）＞西安污染＞深圳污泥，含量较高的化合物主要是蒽、荧蒽、苯并（a）蒽和屈等，珠海污泥和北京污泥的苯并(a）芘含量超过我国城市污泥农用标准，各化合物的最高含量分别分布在兰州污泥、珠海污泥、北京污泥和广州污泥中，各城市污泥中的PAHs具有不同的分布特征，均以少数化合物为主，主要是3和4个苯环的化合物，2、5和6个苯环的化合物含量普遍较低。     

环境优先污染物的筛选原则、程序和方法

确定环境优先污染物,是控制和防治化学品污染的带有战略性的一项基础性工作。本文根据研究编别区域环境优先污染物名单中的实践,并借鉴国内外有关经验,就筛选环境优先污染物的有关原则、程序和方法进行探讨。     

锡工业砷和铅排放标准的初步研究

根据污染源现场调研结果,结合现有污染控制工艺所能达到的技术水平,建议污水排放标准中As浓度由现国家排放标准的0 5mg/L调整为0 1mg/L;Pb不变为1 0mg/L。大气污染物排放标准中As和Pb不变为1 0mg/L。大气污染物排放标准As和Pb的浓度限值分别是为0 5mg/m3和0 7mg/m3。     

Modeling mobile source emissions during traffic jams in a micro urban environment

Urbanization typically involves a continuous increase in motor vehicle use, resulting in congestion known as traffic jams. Idling emissions due to traffic jams combine with the complex terrain created by buildings to concentrate atmospheric pollutants in localized areas. This research simulates emissions concentrations and distributions for a congested street in Minsk, Belarus. Ground-level (up to 50-meters above the street's surface) pollutant concentrations were calculated using STAR (version 3.10) with emission factors obtained from the U.S. Environmental Protection Agency, wind speed and direction, and building location and size. Relative emissions concentrations and distributions were simulated at 1-meter and 10-meters above street level. The findings demonstrate the importance of wind speed and direction, and building size and location on emissions concentrations and distributions, with the leeward sides of buildings retaining up to 99 percent of the emitted pollutants within 1-meter of street level, and up to 77 percent 10-meters above the street.     

Isotopic modelling of the significance of bacterial sulphate reduction for phenol attenuation in a contaminated aquifer

A Triassic sandstone aquifer polluted with a mixture of phenolic hydrocarbons has been investigated by means of high-resolution groundwater sampling. Samples taken at depth intervals of 1 m have revealed the presence of a diving pollutant plume with a sharply defined upper margin. Concentrations of pollutant phenols exceed 4 g/l in the plume core, rendering it sterile but towards the diluted upper margin evidence for bacterial sulphate reduction (BSR) has been obtained. Groundwaters have been analysed for both delta34S-SO4 and delta18O-SO4. Two reservoirs have been identified with distinct sulphate oxygen isotope ratios. Groundwater sulphate (delta18O-SO4 = 3-5/1000) outside the plume shows a simple linear mixing trend with an isotopically uniform pollutant sulphate reservoir (delta18O-SO4 = 10-12/1000) across the plume margin. The sulphur isotope ratios do not always obey a simple mixing relation, however, at one multilevel borehole, enrichment in 34SO4 at the plume margin is inversely correlated with sulphate concentration. This and the presence of 34S-depleted dissolved sulphide indicate that enrichment in 34SO4 is the result of bacterial sulphate reduction. Delta34S analysis of trace hydrogen sulphide within the plume yielded an isotope enrichment factor (epsilon) of -9.4/1000 for present-day bacterial sulphate reduction. This value agrees with a long-term estimate (-9.9/1000) obtained from a Rayleigh model of the sulphate reduction process. The model was also used to obtain an estimate of the pre-reduction sulphate concentration profile with depth. The difference between this and the present-day profiles then gave a mass balance for sulphate consumption. The organic carbon mineralisation that would account for this sulphate loss is shown to represent only 0.1/1000 of the phenol concentration in this region of the plume. Hence, the contribution of bacterial sulphate reduction to biodegradation has thus far been small. The highest total phenolic concentration (TPC) at which there is sulphur isotope evidence of bacterial sulphate reduction is 2000 mg/l. We suggest that above this concentration, the bactericidal properties of phenol render sulphate-reducing bacteria inactive. Dissolved sulphate trapped in the concentrated plume core will only be utilised by sulphate reducers when toxic phenols in the plume are diluted by dispersion during migration.