北江流域水化学时空变化及化学风化特征

为了研究我国南方湿润地区河流水化学时空变化特征及控制因素,选择珠江流域第二大水系的北江为研究对象,通过分析2015年6月（汛期）和12月（非汛期）干流和支流河水基本水质参数及主量离子,利用化学计量法及质量守恒法定量评估了自然过程及人类活动共同影响下的流域化学风化特征及其通量.结果表明:①北江河水主量离子浓度非汛期高于汛期.岩石的区域分布和矿山活动构成了河水离子浓度和水化学类型的空间异质性,其中北江干流和支流连江为Ca-HCO₃型,而支流滃江则以Ca-SO₄型为主.②岩石对北江流域化学风化贡献率依次为碳酸岩（78.44%）>硅酸岩（14.43%）>降水源（5.42%）>蒸发岩（1.71%）.基于碳酸岩是北江径流水化学的主要控制因素,滃江流域的矿山开采活动加速了碳酸岩的风化,其对北江流域化学风化的贡献为7%.③汛期与非汛期的碳酸岩风化速率分别为7.49和5.29 t/（km2·月）,年化学风化速率为87.63 t/（km2·a）.研究显示,由于受水热条件、流域面积以及岩性的影响,北江流域年化学风化速率略大于西江流域,远高于东江以及全球流域化学风化平均值,北江对整个珠江流域的风化贡献较大.      

半挥发性有机物GC/MS分析方法研究

用气相色谱／质谱（ＧＣ／ＭＳ）研究分析了环境中的半挥发性有机标准物。以十氟三苯基磷作调机物,对ＧＣ／ＭＳ仪器系统进行了调整,离子丰度值符合美国环保局（Ｕ．Ｓ．ＥＰＡ）１９８６年推荐的离子丰度标准。测定了３２种目标化合物的保留时间及相对保留因子ＲＦ值,结果表明除五氯苯酚不达标外,其余化合物的ＲＦ值均符合要求,３１种目标化合物的加标回收率为２１％～９７％,相对标准偏差为３．１％～２４．１％,符合美国环保局８２７０方法质量控制检验标准。最后对建立定量校正库与ＧＣ／ＭＳ分析进行了讨论     

水合二氧化锰界面特性及其除污染效能

研究了水合二氧化锰(δMnO2)的界面特性及其吸附性能.考察了δMnO2的比表面积、粒径分布、表面官能团及ζ电位;探讨了δMnO2对水中亚砷酸盐及腐殖酸的吸附去除效能.结果表明:δMnO2的比表面积为117.4m2·g-1,体积平均粒径为0.11μm;δMnO2表面具有丰富的表面羟基(Mn-OH);随着pH值由1.9升高至10.7,δMnO2的ζ电位由 22.7mV降低至53.5mV,其零电荷点在pH3.0附近.δMnO2对亚砷酸盐(As(III))及腐殖酸(HA)均表现出优良的吸附去除效能,其单位δMnO2质量的最大吸附量分别为137μgAs(III)·mg-1δMnO2和1.01mgTOC·mg-1δMnO2.亚砷酸盐与腐殖酸共存时,腐殖酸的存在使得亚砷酸盐的去除率下降10%—28%;而亚砷酸盐对腐殖酸的去除无明显影响.     

气相化学反应中的云盖效应

本文在ＣＢＭ－Ｉ机理的基础上考虑了ＯＨ和ＨＯ２自由基对ＳＯ２的氧化作用和云对光解率的影响，定量研究了气相色化学反应中的云盖效应。结果表明，云的存在将改变整个反应体系的平衡，气态物对云的响应是非线的。     

水中甲苯、对二甲苯磁化-光解耦合过程动力学研究

以甲苯、对二甲苯两种典型苯系污染物为研究对象 ,对其在水中的紫外光解(UV)、磁化 紫外光解 (PM UV)进行了过程动力学比较研究 ,结果证实高强度永久磁场 ( >0 1T)有促进光解的效应 ,并阐述了磁场通过影响污染物光解时 ,自由基对系间跃迁速度的变化而影响反应速度的作用机理 .     

Indicators for Chemicals: Sources,impacts and policy performance (5 pp)

Background Different types of indicators have been developed to describe the impact of chemicals on society and environment. Due to the high number of substances and their different types of use, most of these indicators are directed to specific areas of interest – regarding workplace safety, environmental health or consumer health. They address a specific subset of chemicals and can be used for monitoring enterprise-specific, national or international management measures. Main Features A survey of existing indicators for chemicals has shown that indicators already exist for a remarkable number of problem fields. As soon as the release and the environmental fate of chemicals are taken into account, the complexity of the approaches increases considerably. The distinction between indicators for drivers, pressures, state, impacts and responses, as proposed by the European Environmental Agency, supports the identification of proper indicators for a specific type of problem. Discussion and Conclusions. No single indicator exists which is able to cover the whole range of chemicals and their applications. Several indicator approaches cover at least a subset of the most relevant substances. If they are intended to be used for European monitoring, robust data must be provided by EU Member States. Chemicals in enterprises (ancillary inputs as well as process chemicals) are an important element of in-plant material flow management – in terms of occupational safety and health as well as environmental protection. Existing indicators for hazardous chemicals can be a valuable tool for process and product refinement regarding hazardous chemicals, especially for enterprises. Outlook Indicators for production and impact of chemicals, as well as policy performance indicators, are essential elements in order to monitor the management of chemicals. They have to be established for the national and for the EU level.     

Non-regulated water contaminants: emerging research

Those chemical pollutants that are regulated under various international, federal, and state programs represent but a small fraction of the universe of chemicals that occur in the environment as a result of both natural processes and human influence. Although the number of these targeted chemicals might be minuscule compared with the universe of both known and yet-to-be identified chemicals, an implicit assumption is that these selective lists of chemicals are responsible for the most significant share of risk with respect to environmental or economic impairment or to human health. This paper examines some of the less-discussed aspects of the background and assumptions that underlie society's relationship with chemical pollutants in water, particularly with respect to the need for a more holistic understanding of exposure and risk.     

Green chemistry

A grand challenge facing government, industry, and academia in the relationship of our technological society to the environment is reinventing the use of materials. To address this challenge, collaboration from an interdisciplinary group of stakeholders will be necessary. Traditionally, the approach to risk management of materials and chemicals has been through inerventions intended to reduce exposure to materials that are hazardous to health and the environment. In 1990, the Pollution Prevention Act encouraged a new tact-elimination of hazards at the source. An emerging approach to this grand challenge seeks to embed the diverse set of environmental perspectives and interests in the everyday practice of the people most responsible for using and creating new materials—chemists. The approach, which has come to be known as Green Chemistry, intends to eliminate intrinsic hazard itself, rather than focusing on reducing risk by minimizing exposure. This chapter addresses the representation of downstream environmental stakeholder interests in the upstream everyday practice that is reinventing chemistry and its material inputs, products, and waste as described in the “12 Principles of Green Chemistry”.     

祁连山东端地表及地下水水化学时空变化特征

于2016~2017年5~9月采集祁连山东端（乌鞘岭、古浪、天祝）的地表水和地下水样品进行水化学分析,综合运用统计分析、Piper三线图、Gibbs图以及离子比值等方法探究了祁连山东端地表水和地下水主要离子组成特征、来源以及时空变化.结果表明,祁连山东端地表水和地下水化学组成中优势阳离子为Ca²⁺和Na⁺,Ca²⁺的平均浓度为76.897mg/L,占比73.89%;Na⁺的浓度为16.592mg/L,占比15.94%.优势阴离子为HCO₃^-和SO₄^2-,HCO₃^-浓度190.117mg/L,占比68.71%;其次是SO₄^2-,平均值为67.565mg/L,占比为24.42%.乌鞘岭河水、地下水,天祝河水、地下水的水化学类型为HCO₃^--Ca²⁺型,古浪河水、地下水水化学类型为HCO₃^--Ca²⁺-Mg²⁺型,处于水化学易变区.不同水体离子来源于岩石风化,主要受碳酸盐与硅酸盐风化溶解共同作用控制,人类活动在一定程度上贡献了水体的离子来源.不同水体主要离子浓度的时间变化特征各不相同,整体上大部分水体的离子浓度随时间变化不明显,总体趋势较平缓.     

Spatial Convergence in Major Dissolved Ion Concentrations and Implications of Headwater Mining for Downstream Water Quality

Spatial patterns in major dissolved solute concentrations were examined to better understand impact of surface coal mining in headwaters on downstream water chemistry. Sixty sites were sampled seasonally from 2012 to 2014 in an eastern Kentucky watershed. Watershed areas (WA) ranged from 1.6 to 400.5 km² and were mostly forested (58%–95%), but some drained as much as 31% surface mining. Measures of total dissolved solutes and most component ions were positively correlated with mining. Analytes showed strong convergent spatial patterns with high variability in headwaters (<15 km² WA) that stabilized downstream (WA > 75 km²), indicating hydrologic mixing primarily controls downstream values. Mean headwater solute concentrations were a good predictor of downstream values, with % differences ranging from 0.55% (Na⁺) to 28.78% (Mg²⁺). In a mined scenario where all headwaters had impacts, downstream solute concentrations roughly doubled. Alternatively, if mining impacts to headwaters were minimized, downstream solute concentrations better approximated the 300 μS/cm conductivity criterion deemed protective of aquatic life. Temporal variability also had convergent spatial patterns and mined streams were less variable due to unnaturally stable hydrology. The highly conserved nature of dissolved solutes from mining activities and lack of viable treatment options suggest forested, unmined watersheds would provide dilution that would be protective of downstream aquatic life.