湖北省湖泊水环境化学特征及其与人类活动的关系

通过对湖北省近３０个湖泊水环境化学的分析，探讨了湖北省湖泊水质状况和湖水的化学稳定性，指出远离工业区和居民生活区的湖泊水质一般较好，城区或城效型湖泊在不同程度上受到了工业废水和生活污水的影响。控制，消除湖泊污染是今后经济、社会和环境建设不可忽视的重要工作。     

大坝拦截对河流水溶解组分化学组成的影响分析——以夏季乌江渡水库为例

以乌江渡水库为主要研究对象，揭示了大坝拦截条件下的夏季水化学特征：阴离子以HCO-3,SO2-4为主，阳离子以Ca2+,Mg2+为主，其余离子含量低于10%，说明了碳酸盐岩的风化对水体化学组成起到了主要控制作用，蒸发盐岩石的风化对水体化学组成影响较小。水库水体存在温度分层现象，形成了不同层位的水体有着不同的水化学组成，即水化学分层。水化学的分层形成了溶解组分在水库垂直深度上的规律分布，比如受藻类的影响，Si和叶绿素随深度成相反的变化特征；HCO-3受光合作用和有机质降解的影响，30 m 以上随着水深的增加而递增，30 m 以下呈现相反趋势；水库泄水方式明显改变了水化学各种参数和离子在水体中的分配。乌江水库两主要支流（息烽河和偏岩河）分别对乌江渡坝前水体中的Ca2+,SO2-4,HCO-3,Mg2+和K+,Na+,Cl-有贡献。网箱养鱼、生活污水、农业施肥、酸性矿山废水以及酸雨沉降都会对水体造成不同程度的污染。     

混合电镀废水处理工艺

物化法是处理混合电镀废水的一种有效方法,对COD、Pb离子、Ni离子尤其是Pb离子、Ni离子的处理效果非常理想。COD的去除率达到80.1%,Pb离子的去除率达到97.2%,Ni离子的去除率达到98.1%,中间产出的污泥也可得到较好处理。     

富勒烯甘氨酸铜盐的制备及表征

以富勒烯和甘氨酸为原料合成富勒烯甘氨酸,再与硝酸铜反应得到富勒烯甘氨酸铜盐。通过单因素方法探讨了反应温度、反应时间、反应物物料比对目标物富勒烯甘氨酸铜盐中铜质量分数的影响。获得最佳工艺条件为:富勒烯甘氨酸和硝酸铜的摩尔比1∶5,反应时间2.0 h,反应温度35℃。此时富勒烯甘氨酸铜盐中铜质量分数为17.8%。同时用FT-IR、MS、元素分析及原子吸收等方法表征了产物的结构。用差热仪测试了富勒烯甘氨酸铜盐的热稳定性,表明产物具有良好的热稳定性。     

不同物质对铬价态测定结果的影响

采用单波长法和双波长法,分别考察了KH2PO4、H3PO4、H2SO4、KNO3、牛肉膏和蛋白胨对Cr(III)和Cr(VI)质量浓度测定的影响。结果显示,Cr(III)和Cr(VI)在测量中是相互影响的,并且Cr(III)对Cr(VI)影响较显著。在单波长法测定中,牛肉膏、蛋白胨及2种酸对Cr(III)和Cr(VI)的影响较钾盐对其影响更为显著,H3PO4和H2SO4对Cr(III)和Cr(VI)的特征吸收峰值影响最大,降低幅度在20%～50%。这些物质对双波长法测定Cr(VI)几乎没有影响;但对Cr(III)测定中,H2SO4和H3PO4的影响较大,其相对误差分别为14.57%和8.87%,其余物质产生的相对误差均小于1.6%。因此,双波长法可用于生物样品中Cr(III)和Cr(VI)的测定,线性范围分别为0～160 mg/L和0～80mg/L。     

环境分析化学发展战略研究

环境分析化学是环境化学的一个重要分支.本文报导环境分析化学的研究领域,对象,国内外研究工作的发展趋势以及环境分析方法和环境监测仪器等。近年来,在污染物的超痕量分析、环境标准参考物的制备以及环境分析监测技术自动化方面都有较大的进展,对推动研究污染物的来源、毒性和含量,为最终控制和改造环境起到了推动作用,环境科学的发展在一定程度上依赖于环境分析化学所取得的成就。 在研究国内外工作动向的基础上,我们提出了环境分析化学的中近期研究方向,其中包括有机污染物和元素化学形态定值的环境标准参考物质、无机毒物的形态分析、分析技术的联用,有毒污染物的系统分析、我国优先监测污染物名单的制定、新型采样器,以及监测技术自动化研究等方面,以供从事这方面工作的领导和科研人员参考。     

天然水体中有机酸当量浓度的确定方法

本文根据天然水体中溶解有机在碳与化学需氧量和生化需氧量之间的相关性，以及有机酸当量和水体溶解有机碳之间的近似定量关系，提出了由化学需氧量或生化需氧量得到溶解有机碳或总有机碳浓度，最终得到有机酸和有机酸根当量浓度的转换方法，为大区域天然水体有机酸碱缓冲作用的评估提供了一个实用的转换途径。     

Heavy Metals in the Bed and Suspended Sediments of Anyang River, Korea: Implications for Water Quality

The objective of this study is to compare Anyang River bed sediments with water chemical composition and to assess the anthropogenic chemical inputs into the river system. Eight sampling locations were chosen along the river channel. Bed and suspended river sediments and water samples were collected, and analyzed for their chemical and physical composition. Data revealed that trace element concentrations in the river water were generally below world average, except for As, Mn, Ni and Cr. Among the three phases: water, bed and suspended sediment, more than 99% of the trace elements was associated with the bed sediment. Concentrations of trace elements in the sediment were a function a particle size distribution and organic content. The calculated degrees of enrichment based on the least influenced sample (ASD 1) indicated the river sediments were enriched with respect to background. The enrichment factors for Pb, Zn and As were relatively lower than for Cr, Co, Ni and Zn. The difference in the enrichment seems to reflect the human activities influence in the basin, and specially for Cd. Speciation of the elements in the five different chemical forms in the sediment by sequential extraction indicated that the reducible fraction was predominant for Fe, Zinc and Cu showed an irregular variation among the different fractions; whereas, Cd and Pb were more regular. Zinc and Cu highly existed mostly in exchangeable forms. Acid soluble and reducible forms were also important for most metals. The speciation implies that the metals associated with the sediment are subject to release into water bodies as goechemical variables (pH and Eh) change. Currently, the introduced metals are deposited near the source area and are mostly associated with the sediment, implying that the river bed sediment acts mainly as a sink, rather than a pool. The accumulated and enriched toxic trace elements can pose a potential pollution of river water.     

Application of a coupled ecosystem-chemical equilibrium model, DayCent-Chem, to stream and soil chemistry in a Rocky Mountain watershed

Atmospheric deposition of sulfur and nitrogen species have the potential to acidify terrestrial and aquatic ecosystems, but nitrate and ammonium are also critical nutrients for plant and microbial productivity. Both the ecological response and the hydrochemical response to atmospheric deposition are of interest to regulatory and land management agencies. We developed a non-spatial biogeochemical model to simulate soil and surface water chemistry by linking the daily version of the CENTURY ecosystem model (DayCent) with a low temperature aqueous geochemical model, PHREEQC. The coupled model, DayCent-Chem, simulates the daily dynamics of plant production, soil organic matter, cation exchange, mineral weathering, elution, stream discharge, and solute concentrations in soil water and stream flow. By aerially weighting the contributions of separate bedrock/talus and tundra simulations, the model was able to replicate the measured seasonal and annual stream chemistry for most solutes for Andrews Creek in Loch Vale watershed, Rocky Mountain National Park. Simulated soil chemistry, net primary production, live biomass, and soil organic matter for forest and tundra matched well with measurements. This model is appropriate for accurately describing ecosystem and surface water chemical response to atmospheric deposition and climate change.     

西江流域中部的洪涝特征及防洪减灾对策

对广西西江流域中部的洪涝特征进行了较全面的论述,并对西江流域防洪减灾提出了有效的对策。