四川省马边磷矿区水环境中典型重金属污染分析

马边磷矿区磷矿资源丰富,区内磷矿开采企业较多。在开采的过程中难免会对当地的河水造成一定的影响。为了进一步了解马边磷矿区的环境影响问题,本文通过对磷矿区采集的水体样品和同一地点的水系沉积物样品进行分析测试,共检测了Cd、As、Cu、Cr、Pb、Zn六种重金属元素的含量,采用潜在生态危害指数法对沉积物中的重金属污染程度进行了综合评价。结果如下:马边磷矿区河水中的重金属元素的浓度较低,6种重金属元素含量均低于国家标准(GB3838-2002)。水系沉积物中的重金属元素含量较高,其中:Cd、Pb、Zn分别为2. 06mg/kg、182. 39mg/kg、479. 13 mg/kg。与四川省土壤元素背景值相比:Cd元素超标25. 7倍,Pb元素超标5. 9倍,Zn元素超标5. 5倍,其余元素未超标。与马边地区1∶20万区域水系沉积物背景值相比:Cd元素超标3. 12倍,Pb元素超标3. 3倍,Zn元素超标2. 5倍,As元素超标1. 6倍,Cu、Cr元素含量在背景值以内。与“中国土壤元素背景值”相比:Cd元素超标29. 4倍,Pb元素超标7. 7倍,Zn元素超标7. 1倍。潜在生态危害指数法评价结果表明:Cd的生态危害指数最大,其次为Pb和As,其余Cu、Cr、Zn等元素属于轻微生态风险。     

拉萨河流域拉萨市段农业面源污染情况浅析

通过对拉萨河流域拉萨市段农业面源污染现状和成因进行分析,提出了改善拉萨河流域拉萨市段农业面源污染的对策。研究指出,化肥、农膜、农药的广泛使用,禽畜粪便的随意排放等是造成拉萨河流域拉萨市段农业面源污染的主要原因。针对这些问题,首先要加强流域人们环境意识,以可持续发展为前提,同时配合经济手段和农业面源污染防治对策,有效控制拉萨河流域农业面源污染,为保护拉萨河流域水体资源提供技术支撑。     

凡河榛子岭水库上游河段水质现状及污染防治对策

以2012年4月至10月的水质监测数据为基础,分析了凡河榛子岭水库上游河段水体的水质状况。结果表明：仅夹河厂断面9月监测的水质符合Ⅲ类水质要求,其余各月3个断面监测的水质均超出Ⅴ类水质标准,超标项目主要是总氮、氨氮和总磷;各监测断面水质除总氮、氨氮和总磷超标外,其他项目基本达到Ⅲ类水质标准。凡河榛子岭水库上游河段丰水期各监测项目的浓度值明显大于平水期和枯水期时期。导致水质超标的原因主要是农村面源污染。     

嘉陵江南充段水质监测分析与综合评价

本文依据南充市2011年~2013年嘉陵江流域水环境监测统计资料,采用单因子评价法和综合污染指数法分析与综合评价嘉陵江南充段水质污染特征和现状。结果表明,研究河段内的清泉寺、小渡口和李渡断面总氮含量超标属于地表水Ⅳ类水体,超标倍数年均值分别0.21、0.35、0.37,其他监测项目符合Ⅲ类水质标准,均属于轻度污染。彩虹桥断面总氮、总磷、氨氮、CODMn和BOD5含量超过Ⅲ类标准,均在Ⅳ~Ⅴ类范围,属于中度污染。综合分析嘉陵江南充段,水质主要污染指标为总氮,综合污染指数为0.38,水质综合评价结果属轻度污染。该评价结果能为嘉陵江流域的水环境保护和科学治理提供依据。     

宁波市主要流域农用水质量调查与评价

通过对宁波市两大主要流域姚江、奉化江农用水质环境质量的监测和综合分析评价,结果表明：两流域上游水质较好,没有监测指标超标,达到1级水质标准;中下游水质较差,有多项指标超标,水质以3级为主,部分地段水质达到2级,其主要超标物为粪大肠菌群数、悬浮物、石油类、六价铬和化学需氧量等,其中粪大肠菌群数、悬浮物是影响两流域水体质量的主要污染因子。姚江流域水质要明显好于奉化江流域。在水质的具体农业应用上应先考虑粮油作物和其他旱作作物的灌溉,若使用在对水质要求较严的蔬菜灌溉或渔业养殖上,建议对水质进行治理后再应用,以防影响农产品的产量和品质。     

西藏掠影

<正>西藏遵循‘‘保护中开发,开发中保护"的原则,大部分区域仍保持着原生态,西藏仍然是世界上环境质量最好的地区之一。但是,近年来,拉萨河谷高寒湿地—拉鲁湿地生态系统健康程度处于快速下降状态。人为侵占、乱占湿地,盲目开发、过度放牧的现象十分严重;加上人们毫无顾及地向湿地倾倒生活生产垃圾,排放未经任何处理的生活、生产污水,拉鲁湿地的生态环境系统遭了严重的破坏。图为拉萨河现状。     

郪江流域遂宁段水环境质量调查和评价

为研究郪江流域遂宁段水环境质量，对郪江干流和8条支流开展了现场调查和定期监测。采用内梅罗综合污染指数、断面类别比例法和水环境质量指数对流域水质进行了综合分析。利用综合营养状态指数对水源地水体富营养化进行了评价。结果表明：郪江流域遂宁段水质不能够达到《地表水环境质量标准》(GB3838-2002)Ⅲ类标准要求，水质为轻度污染，枯、平水期水质优于丰水期。支流水质较差，加重了干流水体负荷。流域部分饮用水源地为Ⅳ类水质，同时表现为轻度富营养化。研究成果为水质改善提供理论依据和水生态环境质量稳定达标提供技术支撑。     

太白山自然保护区湖泊水质状况及季节差异

通过对太白山山顶大爷海、二爷海、三爷海与玉皇池等4个湖泊解冻期与冰冻期水体17项常规指标监测,分别利用单项污染指数与综合污染指数对太白山山顶湖泊水质现状进行评价,并对不同时期水质差异进行分析。结果表明太白山山顶湖泊总氮超标严重,总磷、氨氮与汞含量也出现超标现象,其他指标均符合我国地表水环境质量Ⅰ类标准。综合污染指数显示4个湖泊均属于清洁水体,清洁度排序为玉皇池三爷海二爷海大爷海。冰冻期湖泊水质优于解冻期。     

涪江流域遂宁段生态环境监测与水质污染现状评价

为研究涪江遂宁段河流水环境质量和污染现状,对水体中基本理化指标和细菌总数、粪大肠茵群数、浮游藻类组成等生物指标进行了监测和综合分析,并采用了单因子评价法和综合污染指数法对其进行水质污染现状进行了评价。结果表明,该流域境内香山和郭江属地表水Ⅳ类中度污染,污染指标总氮、总磷和BOD;超标倍数分别为0．76、0．26、0．02和0．39、0．24、0．03;跑马滩属地表水Ⅳ类中度污染,总氮和BOD,超标倍数为0．08、0．13;米家桥和老池属于Ⅲ类轻度污染;总氮、总磷和BOD,断面超标率分别为60％、40％、60％。此外,各监测断面水体中细菌总数、大肠菌群数及藻类组成均差异明显,变化趋势与水质理化指标基本吻合。细菌总数变化趋势为郭江〉跑马滩〉香山〉米家桥〉老池,郭江细菌总数2．36×10^7cfu／mL,比跑马滩、香山高、米家桥和老池分别高23.7％和41．5％．56．25倍和65．5倍。     

城镇景观水体水质控制技术分析

本文针对上海城镇小型景观水体水质污染特征，分析了充氧曝气、人工湿地、曝气生物滤池等工艺技术在小型景观水体水质净化中的应用，提出各种小型景观水体水质控制技术的特点和适用范围，为2010年上海世博会园区内景观水体水质控制方法提供参考，也为其他小型景观水体的建设和运行提供借鉴。     

Human Influences on Water Quality in Great Lakes Coastal Wetlands

A better understanding of relationships between human activities and water chemistry is needed to identify and manage sources of anthropogenic stress in Great Lakes coastal wetlands. The objective of the study described in this article was to characterize relationships between water chemistry and multiple classes of human activity (agriculture, population and development, point source pollution, and atmospheric deposition). We also evaluated the influence of geomorphology and biogeographic factors on stressor-water quality relationships. We collected water chemistry data from 98 coastal wetlands distributed along the United States shoreline of the Laurentian Great Lakes and GIS-based stressor data from the associated drainage basin to examine stressor-water quality relationships. The sampling captured broad ranges (1.5–2 orders of magnitude) in total phosphorus (TP), total nitrogen (TN), dissolved inorganic nitrogen (DIN), total suspended solids (TSS), chlorophyll a (Chl a), and chloride; concentrations were strongly correlated with stressor metrics. Hierarchical partitioning and all-subsets regression analyses were used to evaluate the independent influence of different stressor classes on water quality and to identify best predictive models. Results showed that all categories of stress influenced water quality and that the relative influence of different classes of disturbance varied among water quality parameters. Chloride exhibited the strongest relationships with stressors followed in order by TN, Chl a, TP, TSS, and DIN. In general, coarse scale classification of wetlands by morphology (three wetland classes: riverine, protected, open coastal) and biogeography (two ecoprovinces: Eastern Broadleaf Forest [EBF] and Laurentian Mixed Forest [LMF]) did not improve predictive models. This study provides strong evidence of the link between water chemistry and human stress in Great Lakes coastal wetlands and can be used to inform management efforts to improve water quality in Great Lakes coastal ecosystems.     

Wetland Flowpaths Mediate Nitrogen and Phosphorus Concentrations across the Upper Mississippi River Basin

Eutrophication, harmful algal blooms, and human health impacts are critical environmental challenges resulting from excess nitrogen and phosphorus in surface waters. Yet we have limited information regarding how wetland characteristics mediate water quality across watershed scales. We developed a large, novel set of spatial variables characterizing hydrological flowpaths from wetlands to streams, that is, “wetland hydrological transport variables,” to explore how wetlands statistically explain the variability in total nitrogen (TN) and total phosphorus (TP) concentrations across the Upper Mississippi River Basin (UMRB) in the United States. We found that wetland flowpath variables improved landscape-to-aquatic nutrient multilinear regression models (from R² = 0.89 to 0.91 for TN; R² = 0.53 to 0.84 for TP) and provided insights into potential processes governing how wetlands influence watershed-scale TN and TP concentrations. Specifically, flowpath variables describing flow-attenuating environments, for example, subsurface transport compared to overland flowpaths, were related to lower TN and TP concentrations. Frequent hydrological connections from wetlands to streams were also linked to low TP concentrations, which likely suggests a nutrient source limitation in some areas of the UMRB. Consideration of wetland flowpaths could inform management and conservation activities designed to reduce nutrient export to downstream waters.     

尼洋河流域水环境质量现状评价研究——基于模糊综合评价法

尼洋河流域水资源十分丰富,水能蕴藏量巨大,生态环境良好。随着西藏经济的发展,必将出现大规模开发利用水资源的趋势,探讨流域水资源和环境的现状及可持续发展具有十分重要的现实意义。本文对尼洋河流域基础资料的收集与整理,分析尼洋河流域的特点与现存的问题,根据收集的水质监测资料,分析了流域污染源概况和构成,以未进行水环境功能区划为前提,选择模糊综合评价法对尼洋河流域水环境质量进行现状评价,并对超标断面进行了原因分析,通过对2012年尼洋河流域14个监测断面监测成果的评价,得出尼洋河流域水质现状良好的结论,为以后的水功能区划分、水质目标的确定以及水环境功能区划分提供依据。     

人工湿地控制非点源污染的应用

随着点源污染的有效管理和控制，非点源污染已成为水环境污染的主要原因。人工湿地作为一种控制水环境非点源污染的有效工具，已被世界上很多国家所认可。本文首先简述了非点源污染的危害，其次对人工湿地的概念和类型进行了介绍，论述了人工湿地对非点源污染中氮、磷、重金属和农药等主要污染物的去除机理，最后对人工湿地处理系统的附属设施、水力因素、表土层以及植物收割等应用问题进行了探讨。     

河长制背景下流域协同治理问题探讨——基于共容利益理论

河长制是中国水环境治理的重大创新实践,其明确的责任、针对性的治理模式有效实现了水环境质量的大步提升。然而,以行政区划为基础的河长制与流域整体性治理之间依然存在着操作上的缝隙亟待解决。以流域水污染为典型对象,从共容利益的角度,讨论了上、下游河长协同治理的利益博弈结构,明确影响上、下游合作的因素,进而提出河长制背景下促进流域协同治理要从强化协同治理收益、降低交易风险、构建多方联动的协同治理网络三方面展开。     

Simulated wetland conservation-restoration effects on water quantity and quality at watershed scale

Wetlands are one of the most important watershed microtopographic features that affect hydrologic processes (e.g., routing) and the fate and transport of constituents (e.g., sediment and nutrients). Efforts to conserve existing wetlands and/or to restore lost wetlands require that watershed-level effects of wetlands on water quantity and water quality be quantified. Because monitoring approaches are usually cost or logistics prohibitive at watershed scale, distributed watershed models such as the Soil and Water Assessment Tool (SWAT), enhanced by the hydrologic equivalent wetland (HEW) concept developed by Wang [Wang, X., Yang, W., Melesse, A.M., 2008. Using hydrologic equivalent wetland concept within SWAT to estimate streamflow in watersheds with numerous wetlands. Trans. ASABE 51 (1), 55–72.], can be a best resort. However, there is a serious lack of information about simulated effects using this kind of integrated modeling approach. The objective of this study was to use the HEW concept in SWAT to assess effects of wetland restoration within the Broughton's Creek watershed located in southwestern Manitoba, and of wetland conservation within the upper portion of the Otter Tail River watershed located in northwestern Minnesota. The results indicated that the HEW concept allows the nonlinear functional relations between watershed processes and wetland characteristics (e.g., size and morphology) to be accurately represented in the models. The loss of the first 10–20% of the wetlands in the Minnesota study area would drastically increase the peak discharge and loadings of sediment, total phosphorus (TP), and total nitrogen (TN). On the other hand, the justifiable reductions of the peak discharge and loadings of sediment, TP, and TN in the Manitoba study area may require that 50–80% of the lost wetlands be restored. Further, the comparison between the predicted restoration and conservation effects revealed that wetland conservation seems to deserve a higher priority while both wetland conservation and restoration may be equally important.     

基于水质目标的流域排放管控模式与案例研究

改善流域水质是目前我国生态环境治理的重要议题,然而我国目前的流域水污染排放管控体系和手段还存在诸多不足,在流域尺度还未形成一套系统性的水污染管控体系。本研究提出了一种基于水环境质量目标的流域排放管控体系,构建了三种具有一定普适性的排放管控模式,并以成都江安河流域为案例开展实证研究,对比了三种模式在固定源排放管控方面的差异性和适用性。结果表明,本研究提出的管控模式能很好地实现水质达标目的,并能够不同程度地提高不同时段水环境容量的利用率。在相同的边界条件下,流域标准管控模式的方案和流域精细管控模式的方案对于固定源的逐月允许排放量分别为流域简化管控模式的1.3~1.6倍和1.5~2.0倍。     

Strategies for assessing the cumulative effects of wetland alteration on water quality

Assessment of cumulative impacts on wetlands can benefit by recognizing three fundamental wetland categories: basin, riverine, and fringe. The geomorphological settings of these categories have relevance for water quality.Basin, or depressional, wetlands are located in headwater areas, and capture runoff from small areas. Thus, they are normally sources of water with low elemental concentration. Although basin wetlands normally possess a high capacity for assimilating nutrients, there may be little opportunity for this to happen if the catchment area is small and little water flows through them.Riverine wetlands, in contrast, interface extensively with uplands. It has been demonstrated that both the capacity and the opportunity for altering water quality are high in riverine wetlands.Fringe wetlands are very small in comparison with the large bodies of water that flush them. Biogeochemical influences tend to be local, rather than having a measurable effect on the larger body of water. Consequently, the function of these wetlands for critical habitat may warrant protection from high nutrient levels and toxins, rather than expecting them to assume an assimilatory role.The relative proportion of these wetland types within a watershed, and their status relative to past impacts can be used to develop strategies for wetland protection. Past impacts on wetlands, however, are not likely to be clearly revealed in water quality records from monitoring studies, either because records are too short or because too many variables other than wetland impacts affect water quality. It is suggested that hydrologic records be used to reconstruct historical hydroperiods in wetlands for comparison with current, altered conditions. Changes in hydroperiod imply changes in wetland function, especially for biogeochemical processes in sediments. Hydroperiod is potentially a more sensitive index of wetland function than surface areas obtained from aerial photographs. Identification of forested wetlands through photointerpretation relies on vegetation that may remain intact for decades after drainage. Finally, the depositional environment of wetlands is a landscape characteristic that has not been carefully evaluated nor fully appreciated. Impacts that reverse depositional tendencies also may accelerate rates of change, causing wetlands to be large net exporters rather than modest net importers. Increases in rates as well as direction can cause stocks of materials, accumulated over centuries in wetland sediments, to be lost within decades, resulting in nutrient loading to downstream aquatic ecosystems.     

HYDROGEOLOGIC EVALUATION OF WETLAND BASINS FOR LAND USE PLANNING1

ABSTRACT: Wetlands occur in a variety of geologic, hydrologic, and topographic settings and exhibit diverse hydrogeologic characteristics. A wetland is more than an organic mat - it is an element in a larger hydrogeologic system. Three distinct but related effects of wetlands are: modifying the character of runoff from a basin, influencing the discharge/recharge relationship with the underlying aquifer, and effecting the potential for ground water development in a wetland dominated basin. An important goal of wetland research is to define the diverse roles that wetlands play in the regional hydrology and to define the geologic, hydrologic, and topographic factors that will allow meaningful distinctions among wetlands. Geologic and hydrologic factors include character and thickness of surficial materials; bedrock type; hydrologic position; permeability of organic layer; transmissivity, quality, and hydrologic connection of wetland related aquifers; ground water outflow; and depth of standing water. Topographic factors are position in the drainage basin, relative size, and absolute size of wetlands. A wetland classification to aid hydrologists and land use planners is proposed using selected factors involving hydrologic position, topographic position, and geologic type.