基于水质污染风险识别的人工湖需水研究

人工湖需水量是指维持湖区水量平衡、满足人工湖水质目标的供水量,人工湖需水量确定是人工湖水体工程设计的主要内容之一。以上虞滨海新城建设的人工湖为例,分析了人工湖建成后的可能污染源,采用TP质量守恒模型,预测了不同生活污水截污率、生态措施作用前后的人工湖需水量及水质要求。结果表明,当生活污水截污率为100%时,若供水TP≤0.10mg/L,则人工湖需水量为240万t/a;当生活污水截污率为95%时,若供水TP=0.05mg/L,不考虑生态措施作用,则人工湖需水量为1 600万t/a;当生活污水截污率为95%时,若供水TP=0.05mg/L,在生态措施作用下人工湖需水量为730万t/a。     

鄱阳湖区人地关系转变及其驱动力分析

通过综述鄱阳湖区人地关系史3个重要时期“围湖造田”、“退田还湖”及“鄱阳湖生态经济区”人类活动对湖区生态环境的影响及三者的转变过程,探讨了湖区人地关系的转变及其驱动力。结果表明“围湖造田”降低了湖泊、湿地的诸多功能（如调蓄洪水、维持生物多样性、碳汇等）,促生了人地之间的紧张关系;“退田还湖”则使湖泊、湿地功能得以逐步恢复,缓和了湖区人地关系,而“鄱阳湖生态经济区”的提出与建设将产生良好的社会、经济与生态效益,把湖区人地关系推向和谐阶段。鄱阳湖区人类活动由“围湖造田”到“退田还湖”的转变是在当地人民对自然灾害的深刻反省与国家政策的双重驱动下实现的,而“鄱阳湖生态经济区”的提出与建设则是人与自然和谐相处的价值观在社会、经济发展中的体现,是当地人民主动建设生态文明和实践科学发展观的典型案例。     

湖泊富营养化模型的研究进展

湖泊的富营养化是全球普遍关注的环境问题之一.湖泊的富营养化模型是防治、修复和治理湖泊富营养化的重要决策工具.按研究的侧重点不同,将湖泊富营养化模型分为简单回归模型、水质模型、生态模型和生态-水动力水质模型,并分别回顾了四类模型的研究进展.最后指出湖泊富营养化模型的发展趋势,强调不确定理论、3S技术、耦合模型是今后湖泊富营养化模型研究的重点,应在此基础上建立通用的模拟、预测、评价和优化模型,为湖泊富营养化管理提供科学依据.     

环保疏浚的技术要求与环保绞刀的设计

湖泊底泥环保疏浚是消除内源性污染最快捷、最有效的方法,并为生态恢复创造条件,而环保绞刀是湖泊底泥环保疏浚的必要条件.阐述了环保疏浚的技术要求,设计了绞吸式挖泥船用环保绞刀,满足了湖泊底泥环保疏浚的需要.     

属性识别理论模型在湖泊水质富营养化评价中的应用

近年来提出的属性识别理论模型已在环境质量评价中有所应用。现将该模型引用到湖泊水质富营养化评价中来 ,并用此模型对福州市山仔水库的水质进行评价 ,其评价结果与运用模糊隶属函数法得到的结果进行比较 ,其结果令人满意。此模型为湖泊水质的富营养化评价提供一种简便实用的评价方法     

Measuring Water Storage Fluctuations in Lake Dongting, China, by Topex/Poseidon Satellite Altimetry

Although satellite radar altimetry was developed and optimized for open oceans, it has been used to monitor variations in the level of inland water-bodies such as lakes and rivers. Here, for the first time, we have further used the altimetry-derived variation of water level for estimating the fluctuation of water storage as an addition to the present in situ water storage estimation systems to be used in remote areas and in emergency situation such as in the events flooding monitoring and for studying the effect of climate change. Lake Dongting, the second largest lake in China, influenced frequently by flooding, was, therefore, chosen to demonstrate the potential of the technique. By using the concept of an “assumed reference point”, we converted Topex/Poseidon satellite altimetry data on water level variations in Lake Dongting to “water level” data. The “water level” time-series data and in situ water storage were used to establish a rating curve. From the rating curve, we converted data on “water level” derived from seven years (1993–1999) of Topex/Poseidon data to actual water storage in Lake Dongting. The result reveals that the seasonal and annual fluctuations of water storage occurred during the 1990s with a more frequent flooding at the late 1990s' especially the flooding in whole catchment level in 1998 and 1999. The study supports the usefulness of satellite altimetry for dense and continuous monitoring of the temporal variations in water dynamic in moderate to large lakes.     

基于GIS的湖泊区域地表水环境影响评价方法

对地理信息系统（Geographic Information System,GIS）技术在地表水环境影响评价中的应用进行了系统分析,指出了应用GIS的技术优势。通过实例研究,提出了基于GIS的区域地表水环境影响评价的方法步骤。在环境监测数据的基础上,利用计算机软件ArcView对BOD5和COD两个评价参数的监测值在水域中的空间分布进行分析,绘制区域等值线,结合地表水评价标准,进行水质评价,确定不同等级水质的空间分布区域。最后对应用GIS应注意的问题进行了分析。     

Spatial Heterogeneity of Water Quality in a Highly Degraded Tropical Freshwater Ecosystem

Awareness of environmental heterogeneity in ecosystems is critical for management and conservation. We used the Xochimilco freshwater system to describe the relationship between heterogeneity and human activities. This tropical aquatic ecosystem south of Mexico City is comprised of a network of interconnected canals and lakes that are influenced by agricultural and urban activities. Environmental heterogeneity was characterized by spatially extensive surveys within four regions of Xochimilco during rainy and dry seasons over 2 years. These surveys revealed a heterogeneous system that was shallow (1.1 m, SD = 0.4 ), warm (17°C, SD = 2.9), well oxygenated (5.0 mg l⁻¹, SD = 3), turbid (45.7 NTU SD = 26.96), and extremely nutrient-rich (NO₃–N = 15.9 mg l⁻¹, SD=13.7; NH₄–N = 2.88 mg l⁻¹, SD = 4.24; and PO₄–P =  8.3 mg l⁻¹, SD = 2.4). Most of the variables were not significantly different between years, but did differ between seasons, suggesting a dynamic system within a span of a year but with a high resilience over longer periods of time. Maps were produced using interpolations to describe distributions of all variables. There was no correlation between individual variables and land use. Consequently, we searched for relationships using all variables together by generating a combined water quality index. Significant differences in the index were apparent among the four regions. Index values also differed within individual region and individual water bodies (e.g., within canals), indicating that Xochimilco has high local heterogeneity. Using this index on a map helped to relate water quality to human activities and provides a simple and clear tool for managers and policymakers.     

艾比湖湿地生态效应能值评价

湿地是地球上具有多功能的独特生态系统,是自然界最富生物多样性的生态景观和人类最重要的生存环境之一。内陆干旱区的湿地则因其所处地理环境的特殊性更具有巨大保护价值。艾比湖湿地在我国内陆荒漠自然生态系统中具有一定典型性。其生态系统极不稳定,具有很强的敏感性和脆弱性。人类社会经济的迅猛发展,引起一系列以土地荒漠化为代表的生态逆向演替,严重的水土流失和锐减的生物多样性使其不可更新资源的能值投入远远超过其可更新资源,同时,肆虐的盐尘严重危害着天山北坡经济带甚至更远地区工、农、牧业生产和人们的生活环境。从能值角度评价环境的贡献,注重其生态效应,以期引起人们警醒,加强湿地资源的保护和管理,维护其可持续发展。     

长江流域生态环境对洪涝影响的评价

长江流域的生态环境问题近年来变得越来越严重,其集中表现为：人口急剧增长的情况下,土地资源过度利用和不合理的开发,使生态环境的脆弱性增强,造成生态环境的恶化,结果导致洪水威胁加剧。本文通过对长江流域生态环境问题的分析,提出目前存在的问题是上游森林的过度开发、毁林开荒、陡坡开荒造成水土流失,增加了中下游河湖的泥沙淤积;中下游地区盲目围湖造田,占用行洪洲滩,湿地生态环境遭到破坏,造成水调蓄面积减少。最后就生态环境问题对洪涝的影响进行了评价。