骆马湖富营养化调查

骆马湖为一浅水湖泊,具有典型的过水性特征,其已经处于中—富营养化阶段。通过对骆马湖富营养化发生机制的研究,发现入湖河道携入大量营养物质入湖和水生植物的破坏是骆马湖富营养化进程加快的主要原因。并提出了控制骆马湖富营养化的一些措施:控制外源污染物入湖、加强湖滨湿地建设和水生植物的保护、合理的水库调度以及湖泊内部的生物治理。     

滇池流域水资源与水污染问题

滇池水质污染与流域水资源紧缺二者相互影响，相互制约，存在人口机械增长过快，沿岸开发过度，面山水土流失严重和水资源未能优化配置等问题，应从水土保持综合治理，优化配置水资源，控制入湖污染物总量等方面着手，监管，科研，生态恢复并重，逐步解决滇池流域水资源与水污染问题。     

城市水资源社会再生能力评价模型研究

为了在城市水资源评价过程中充分考虑城市水资源的社会循环，更好地揭示城市水资源开发利用的潜力，提出了城市水资源社会再生能力概念，并分别建立了城市水资源社会绝对再生能力与相对再生能力的评价指标体系；在此基础上，建立了一种全新的城市水资源评价模型——基于人工神经网络的城市水资源社会再生能力评价模型．该模型在构造评价标准的过程中，通过“虚拟城市”构造模型训练样本；由此将评价问题转化成人工神经网络所擅长的分类问题，并赋予评价结果实际的内涵，使得评价结果更直观且更易于理解．最后，以黄河流域的主要城市为研究对象，对其绝对水资源再生能力与相对水资源再生能力分别进行评价；并与传统的灰色关联方法进行对比；评价结果与实际相吻合。     

固城湖生物资源现状及近20年间的变化趋势

1999年对固城湖渔业生物资源进行了周年调查,结合1981年4月至1982年3月、1987年6月至1988年5月的2次调查资料,比较分析了固城湖生物资源的动态。研究结果表明,从1981年至1999年近20a间,固城湖浮游植物数量增加44.8倍,生物量增加40.6倍,生物多样性减少。浮游动物数量较20世纪80年代下降约50%,生物量高于80年代初期,低于80年代后期。底栖动物生物量下降,其中瓣鳃类、腹足类生物量下降明显,而寡毛类和摇蚊幼虫等数量与生物量增长显著。固城湖水生植物演替剧烈,水生植物群落结构发生了重大变化,已由苦草、轮叶黑藻群落演变为微齿眼子菜、菹草群落,渔业利用价值下降。每年大量水草腐烂沉积,使固城湖水质呈现不断下降趋势。指出加强对固城湖生物资源的调控和综合利用,是固城湖生态保护和建设的关键。     

太湖流域近地表大气二氧化碳本底体积分数观测研究

基于2003年1月至2005年6月用气相色谱法对太湖流域近地表大气中二氧化碳本底体积分数的监测资料,对太湖流域近地表大气二氧化碳体积分数的变化特征进行了分析研究。结果表明:在观测时段内,太湖流域近地表大气二氧化碳体积分数平均值为(413.7±19.2)×10-6,且呈上升的趋势,主要受人类活动、工农业生产和交通运输业发展的影响;二氧化碳体积分数季节变化明显,冬春季高,夏秋季低,冬季出现峰值,平均体积分数为(417.8±3.7)×10-6,夏季出现谷值,平均体积分数为(400.8±14.7)×10-6,一年中最高值(424.0±1.1)×10-6出现在12月份,最低值(387.7±1.4)×10-6出现在8月份,主要受源汇强度变化影响;二氧化碳体积分数日变化基本呈双峰态,这是源汇强度变化和边界层稳定程度相互作用的结果。     

农业生产活动对鄱阳湖区生态环境的影响

鄱阳湖区是江西省重要商品粮基地，但其生态环境也有较为脆弱的一面。某些违反生态规律的农业生产活动导致该区生态环境的恶化。本文从围湖造田、湖区传统耕作制度、乡镇企业发展及农民环境意识淡薄等方面分析了它们对湖区生态环境的影响，并提出几点治理意见。     

日本琵琶湖流域的生活污水治理对策

介绍了日本滋贺县为了保护琵琶湖水环境而实施的生活污水综合治理对策。其基本思路是：将市区和人口稠密地区划为下水道整备规划区，积极实施下水道建设工程，推行污水处理；在下水道整备区外推广使用合并净化槽和地域粪便处理设施；在有条件的农村村落建设农村下水道；鼓励和资助各种处理设施实行除氮除磷的高级处理方式，以防止琵琶湖富营养化；积极实施多种多样的生活杂排水对策。     

里杜湖富营养化综合评价及预测

根据里杜湖水库的水质监测及水文资料，选择评分法结合生物优势种评价法以及“源－效应”预测模型对里杜湖水库水质的营养状态进行综合评价及预测。结果表明：里杜湖水库水质已轻度富营养化，并有逐年加重的趋势。旨在正确评价和预测里杜湖水库营养状态，并为同类水库的营养状态评价及预测提供参考和借鉴，从而为水库水质管理及富营养化的控制提供科学依据。     

Phytoplankton Community and Chlorophyll a as Trophic State Indices of Lake Skadar (Montenegro,Balkan) (7 pp)

Background, Aims and Scope Phytoplankton, as a first step in trophic cascades of lakes, can be a good indicator of trophic states, considering that every environmental change affects this community and many species of this community are sensitive to changes, and that they response very quickly. In this study, we tried to assess and predict the trophic state of Lake Skadar according to phytoplankton data.Methods Water samples were collected using Ruttner sampling bottle. Temperature, dissolved oxygen, ph, conductivity and transparence were measured in situ using portable equipment. Nutrients and chlorophyll a were measured using standard spectrophotometric methods. A determination of phytoplankton species was performed using relevant keys and the counting of cells was performed using sedimentation methods.Results and Discussion The species composition of Lake Skadar revealed 95 taxa, with Chlorophyceae and Bacillariophyceae being represented best. According to an average chlorophyll a concentration of 5.9 µg/l, Lake Skadar belongs to the mesotrophic level of the trophic scale. Developed prediction equation for chlorophyll a revealed a good prediction (R2=0.71) and the parameter Secchi depth was primarily correlated with chlorophyll a concentration. Trophic state indices derived from chlorophyll a and transparency, were close together, but both were below the phosphorous index. Values of trophic state indices rank the Lake Skadar as being mesotrophic. This study also showed that indices of diversity based on phytoplankton are weak indicators of trophic status and that they can well characterize only differences between assemblages and associations. According to calculated saprobic indices (ranging from 1.5 to 2.15), Lake Skadar is on betamesosaprobic level of saprobity, which means that it is moderately polluted with organic compounds. Conclusions Total phosphorus is not the main limiting factor for the phytoplankton community in Lake Skadar. Disagreements between chlorophyll and the transparency index, on the one hand, and the total phosphorus index, on the other, suggest that the phytoplankton in Lake Skadar is probably limited by other factors than phosphorus, such as nitrogen, toxic substances or intense zooplankton grazing. According to the majority of investigated parameters and indices derived from phytoplankton data, Lake Skadar is mesotrophic, with tendencies toward eutrophic levels during the summer period. Recommendations and Outlook Long-term monitoring is required for a better estimation of state and the conditions of Lake Skadar. Further studies on factors influencing the phytoplankton community, especially zooplankton grazing and toxic substances, which were not included in this study, should be continued in the future to improve the efficiency of phytoplankton usage in estimating the ecological and trophic conditions of Lake Skadar.     

S–O–C isotopic picture of sulphate–methane–carbonate system in freshwater lakes from Poland. A review

Microbial oxidation of organic compounds (including methane), in freshwater sediments, may result in precipitation of carbonates, which may become an important geochemical archive of paleoenvironmental variations. Most probably low δ¹³C value in calcite in eutrophic systems results from an advanced oxidation of organic compounds in turbulent or/and sulphate-rich conditions. Likewise, high δ¹³C value in calcite from organic-rich sediments may evidence low redox potential of the freshwater system. Oxidation of methane and organic matter results in significant isotope effects in sulphates dissolved in water. Therefore, to better understand the origin of carbon isotope signal in carbonates, concentration and stable isotope measurements in dissolved sulphate (water column), bubble methane and calcite (freshwater sediments) have been carried out in 24 lakes, 2 ponds and 4 rivers in Poland. The highest concentration of sulphate has been detected in rivers (85.47 SO₄ ²⁻ mg/l) and an artificial lake (70.30 SO₄ ²⁻ mg/l) located in the extremely SO₄ ²⁻-polluted region called the “Black Triangle”. The lowest concentration of sulphate is found in dystrophic and mountain lakes (from 0.5 SO₄ ²⁻ to about 3 mg/l). The lowest δ³⁴S(SO₄ ²⁻) and δ¹⁸O(SO₄ ²⁻) values occur in unpolluted lakes in eastern Poland (−0.94 and 1.38‰, respectively). The highest S and O isotopic ratios are found in a polluted lake in western Poland (δ¹⁴S(SO₄ ²)=12.95‰) and in a dystrophic lake in eastern Poland (δ¹⁸O(SO₄ ²) = 16.15‰) respectively. It is proposed that δ³⁴SO₄ ²⁻ and (¹⁸O(SO₄ ²⁻) values in lakes represent a good tool to assess and quantify anthropogenic impact by acid precipitation and to monitor variations in the trophic state and redox processes controlled by biodegradation of organic compounds in sediments and water column. In general, increasing depth (up to 12 m) of the water column is associated with decreasing trend the δ¹³C(CH₄) value from about –35 to about –78‰. However, δ¹³C value in sedimentary calcite (δ¹³C vary from –10 to 0.5‰) shows opposite trends as compared to the corresponding methane. This is probably due to redox processes and distribution of heavy isotopes between methane and calcite. Likewise, turbulent water (river) show high δ¹³C value in methane and low δ¹³C value in calcite—this is probably due to an enhanced oxidation of methane producing ¹³C-depleted CO₂. In contrast to clean lakes, it is observed that an increase of the δ¹³C(CH₄) value occurs with increasing depth of the water column in a strongly SO₄ ²⁻-contaminated lake. This is probably due to a loss of biological buffering potential of the lake accompanied by an active oxidation of methane precursors.