陕北红碱淖湖泊变化和生态需水初步研究

红碱淖位于陕北风沙区,是我国沙漠中最大的淡水湖,对当地生态环境保护具有重要作用。论文通过对陕北红碱淖湖泊的考察和调研,调查分析了湖泊近年来的变化趋势和流域的生态环境现状。在流域水资源开发利用分析和耗水计算基础上,初步定量评价了湖泊变化的主要影响因素。计算结果表明,红碱淖近年的萎缩主要是由于当地气候持续干旱的影响,目前该湖泊仍处于负均衡状态。根据湖泊对于当地生态环境的重要性,确定了湖泊保护的最小目标和适宜目标,根据水量平衡计算,确定了最小和适宜的生态需水量。通过对流域社会经济用水和生态建设用水研究,提出了湖泊保护的对策建议。     

Distribution, sources and potential toxicological significance of polycyclic aromatic hydrocarbons(PAHs) in Guanting Reservoir sediments, China

The Guanting Reservoir lost its function as the second biggest drinking water source for Beijing due to the pollutions from the upstream flow of Yongding River in 1997. From 1998, lots of studies were carryied out to renew the function of Guanting Reservoir as domestic drinking water source before 2008 Olympic Games. This is the first time that polycyclic aromatic hydrocarbon concentrations in the surface sediment of Guanting Reservoir have been analyzed. A distinctive spatial distribution of PAHs was observed. Sediments from four sites along Inlet of Yongding River to reservoir bam had PAHs concentrations of 1377--2855 μg/g dw in descending order. The composition of PAHs is investigated and used to assess patrogenic,combustion and naturally derived of the sediments samples of Guanting Reservoir. Special PAHs ratios, such as phenanthrene/anthracene(P/A) and fluoranthene/pyrene(Fl/Pyr) were calculated to assess the relative importance of different origins. The data confirmed a relatively high level of petrogenic contamination in four sites. These high PAHs levels were associated with the input of untreated and partially treated industrial sewage. In addition, the concentrations of PAHs compounds of samples indicated that sediments of reservoir were most likely to pose potential biological impairment.     

渤海表层沉积物中DDTs、PCBs及酞酸酯的空间分布特征

利用第2次全国海洋污染基线调查数据,研究渤海表层沉积物中DDTs、PCBs和酞酸酯的空间分布特征．结果表明：DDTs和PCBs的高值样点主要分布于秦皇岛近岸、辽东湾近岸和渤海湾近岸海区;酞酸酯的最高值和次高值样点分别出现在莱州湾近岸和辽东湾近岸,而秦皇岛近岸海区的平均水平高于其它海区．目前,渤海表层沉积物中PCBs和酞酸酯的含量相对较低,对周边底栖生物尚未构成威胁．另一方面,DDTs组成的比值关系显示秦皇岛近岸、渤海湾近岸和辽东湾近岸海区近期出现DDTs的输入,并且DDTs含量已超出相应的生态效应低值区间的标志水平,具有一定的生态风险．在渤海海区大多数样点,DDTs的主要代谢产物为厌氧条件下的DDD．     

武汉东湖风景名胜区可持续发展障碍与对策研究

武汉东湖风景名胜区可持续发展的主要障碍是湖泊水体的水质恶化,文章分析了城市污水的大量注入和湖泊水动力条件的改变是主因;提出了加快东湖截污与城市污水治理的工程建设、从单纯的点源治理转向综合治理、重新开启通江调节闸门恢复通江湖泊功能、实施环湖绿色生态保护工程建设意见。     

聚硅硫酸铝(PASS)的制备及其实际应用

以硅酸钠、硫酸铝及氢氧化钠等为原料,将硅酸钠在碱性条件下预聚,然后在快速搅拌下加到硫酸铝水溶液中,用氢氧化钠等碱性物质与混合液聚合而形成聚合铝硅混凝剂(PASS)。这种混凝剂在处理微污染饮用原水、富营养化湖水及再生纸生产废水时有较好的去除效果,具有广泛的应用前景。     

楚科奇海陆架区表层沉积物放射性核素的分布

对中国首次北极科学考察期间在楚科奇海采集的9个表层沉积物样品进行了γ谱分析。结果表明,2 1 0 Pb的比活度介于16.0～76.6Bq·kg 1 之间,平均为3 6.9Bq·kg 1 ,低于大多数中低纬度区表层沉积物的2 1 0 Pb比活度,反映出研究海域低的大气2 1 0 Pb输入通量。2 2 6 Ra、1 37Cs、2 38U的放射性比活度范围和平均值分别为11.4～2 0 .9、1.7～2 .9、3 2 .4～5 3 .4Bq·kg 1 和17.6、2 .2、44 .4Bq·kg 1 。研究海域表层沉积物中的2 2 6 Ra/2 38U ) A .R .介于0 .3 5～0 .47之间,低的2 2 6 Ra/2 38U) A .R .表明U、Ra的地球化学行为存在差异。2 1 0 Pb、2 1 0 Pbex、1 37Cs、4 0 K比活度和灼烧失重率均随离岸距离的增加逐渐减小,而2 2 6 Ra和2 38U则具有各自不同的分布特征,分别与研究海域表层沉积物Si和Ca的分布比较类似。对核素间相关关系的分析表明,研究海域表层沉积物中1 37Cs和2 1 0 Pbex含量与灼烧失重率之间存在良好的线性正相关关系,证实有机物质在2 1 0 Pb、1 37Cs的生物地球化学循环中起着重要作用。     

黄河中下游表层沉积物中多氯联苯的污染特征

对采自黄河中下游地区12个站点17个表层沉积物样品中的多氯联苯进行了定量分析测定,并讨论了多氯联苯在沉积物中的污染特征.结果表明:①黄河中下游表层沉积物中多氯联苯的浓度范围为ND—5·98μg·kg~(-1),受污染程度较轻;②沉积物样品中多氯联苯同族体的组成特征非常相似,都以含3—5个氯原子的PCB同族体为主,占多氯联苯总量的94·68%以上,且在大多数样品中含量顺序为:四氯联苯>三氯联苯>五氯联苯;③该地区表层沉积物中多氯联苯的含量与TOC和沉积物的机械组成无明显相关性,这可能与黄河中下游复杂的水利条件和沉积物自身的理化性质有关.     

湖泊流体动力学模型及实验

从二维浅水非恒定流的控制方程出发,建立了一个二维湖泊流体动力学模型.并根据天津于桥水库的实际情况,对该水库引水期和非引水期的湖水流场的不同情况进行了模拟试验.结果表明,在引水期水库的流场达到稳定状态时,水库流场有一个自东向西的水流主要通道.还对水库出口处有初始水体流速的情况进行了模拟.模拟的结果与于桥水库的实际污染物浓度分布基本一致.      

金坛市饮用水源地保护方案研究

钱资荡是金坛市目前直接饮用水源地,根据环境监测结果,它已处于中营养化后期。借鉴国内外先进的湖泊管理经验,运用系统工程的思想和方法提出了切实可行的金坛市饮用水源地保护方案。该方案由4个工程子系统组成,（1）截污工程：在岸丘桥和南州桥位置各筑一节制闸（而岸丘桥工程又是首选工程）,以封住湖泊两头入流,杜绝污染物进入水源地的截污工程;（2）引水工程：是截污工程的配套工程,利用一游长荡 湖来补充水量,并对3个引水工程设想进行了系统分析,推荐涵管方案,同时将长荡湖作为该市战略水源地一并纳入保护体系中;（3）湿地生态处理工程：对进入荡区前的芦苇区进行综合整治,发展以芦苇为主的湿地生态处理工程;（4）环湖绿色自然保护带工程：包括建设围湖芦苇荡、环湖林带、绿色食品基地以及污泥处置。最后还提出了三级水域保护区范围、水域行政管理体系建设以及工程方案分步实施计划。     

Sediment Parameters of Northwest Black Sea Shelf and Slope: Implications for Transport of Heavy Metals and Radionuclides

In June 1990, sediment cores were obtained from several locations in the Northwest Black Sea shelf and slope by a joint US/USSR scientific team aboard the survey vessel R/V VODYANITSKY. the goal of this investigation was to determine the distribution and levels of radioactivity resulting from the Chernobyl 1986 nuclear accident. the sediment was characterized for texture, mineral composition, redox state, heavy metals, and radionuclides. Correlations emerging from these data reveal paths of dispersal and transport of materials from river sources to deposition sites on the shelf and slope. Kaolinite in the clay mineral suite clearly reflects a dispersal pattern originating in the Danube River and progressing in an easterly direction across the shelf. Sand-size gypsum and the elemental heavy metals Zn, Cu, Cr, and Pb (probable industrial source) as well as the elements Al and Mg (probable terrigenous source) also show a dispersal pattern from the Danube station location in an easterly direction across the shelf. the dispersal direction indicated by these materials is not in conflict with recent existing notions concerning the hydrology of the Northwest Black Sea. Barium anomalies at a midshelf location may be related to operations in the Lebada oil fields situated updrift. Heavy mineral dispersal reflect the Danube and -Crimean Provinces established for the shelf and relate to terrestrial source areas. in addition, the heavy mineral monazite correlates with the radioactive Th 232 found most abundantly in the Crimean Province. Local anomalies of Mn, Fe and U in the sediment at station locations are related to redox (Eh) conditions and other factors. Cs^134/137 data, reported by Curtis and Broadway (1991), correspond to transport and dispersal patterns implicit in the mineralogic, anthropogenic indicators, and sediment characteristics of the study area.