鄱阳湖平原区农村门塘形态特征及底泥营养状况分析

通过在鄱阳湖平原选取典型农村门塘,对其形状、进出口布置、水下地形、水深、淤塞、水质和底泥营养盐含量等指标进行调查测定分析.结果表明,鄱阳湖平原农村门塘多呈长条形;进水口设置随意,多且分散;淤塞较为严重,淤积物主要以外源输入为主;水体总氮和总磷一定程度超标,污染程度总氮总体表现为冬季＞秋季＞夏季＞春季,总磷总体表现为夏季＞春季＞秋季＞冬季;底泥营养盐和有机质含量相对较高,呈现一定的污染状态;底泥中有机质、有机碳和总氮的同源性较高,主要以内源污染物为主;底泥中磷以陆源输入为主.     

绛溪河流域简阳段水环境调查与特征分析

采用单因子评价法、水质类别比例法、平均综合污染指数法、SPSS统计和相关性分析方法,调查分析绛溪河简阳段水环境特征,提出污染防治建议。本次调查结果表明:(1)监测断面氨氮、总磷、化学需氧量达到Ⅲ类水质标准的比例分别为72.2%、11.1%、22.2%,污染最重的因子是总磷;(2)部分断面指标不能完全达标,从上游至下游水质变差;(3)支流海螺河、赤水河对干流污染贡献大;(4)平均综合污染指数与总磷的相关性高于氨氮、化学需氧量,河流污染受磷元素影响最为显著;(5)氨氮与总磷显著相关,河流氨氮、总磷同源性较好。     

萍水河水质监测点的优化

城市内河流水质监测点位的优化,是全面掌握河流水质状况的关键。文章采用贴近度法对萍乡市萍水河2005—2015年水质及监测点位变化进行分析评价,并提出优化建议。根据萍水河水质污染特征,选择化学需氧量、五日生化需氧量、氨氮、总磷、总氮和高锰酸钾盐指数作为评价指标,结果表明:2005—2015年,萍水河水环境质量整体情况较好,但在2010年后呈下降趋势;监测点布设方案的调整有一定合理性,也有欠妥之处;对目前监测点位进行删减,得到了水质优化监测布点方案。     

徐州市地表水体底泥重金属污染特征研究

文章对徐州市地表水体底泥重金属的污染特征进行了研究。对流经徐州市的四条主要河流和云龙湖的55个底泥采样点的重金属含量进行了测试,并采用单因子污染指数法进行了评价。结果表明,徐州市地表水体除云龙湖之外均不同程度地受到了重金属元素的污染。荆马河污染最为严重,其次是奎河、故黄河、京杭大运河。云龙湖的第五个采样点也受到了Hg的污染。污染元素的种类及污染程度与徐州市的产业结构密切相关。     

河南省典型污染河流水环境现状评价及相关性分析

以河南省内典型污染河流贾鲁河、惠济河、卫河为研究对象,以氨氮、化学需氧量、总磷等污染物为评价因子,以2010—2014年间河流的水质监测数据为基础,基于SPSS的统计分析,重点研究河流中氨氮、化学需氧量、总磷等污染物的质量现状及演变趋势,在此基础上探索污染因子之间的相关性。     

河流底泥砷污染状况及分布特征研究

为了今年马鞍山市河湖整治重点工程中清淤工程环境安全需要,对该市城郊某河全流域不同断面底泥中砷含量进行了分析,评价了底泥砷污染状况并分析了该河流底泥中砷的沿程分布特征、横向分布特征和垂向分布特征。结果表明,该河流底泥砷含量范围为17.9~335mg/kg,均值为94.25mg/kg。参照土壤环境质量标准三级标准值对底泥中砷含量进行评价,平均砷污染指数2.69为中度污染;用土壤背景值标准参照评价,平均砷污染指数为9.72,超过当地背景值水平8.50倍,该河流从上游到下游,总体上沿程底泥砷含量未呈明显变化,但局部域段呈现一定变化趋势;断面横向分布上,河中间砷含量总体高于河岸边;垂向分布上,表层底泥砷含量最高。     

水磨河流域有机氯农药污染调查及防治对策

在对水磨河流域实地勘察的基础上,用GC-ECD定量测定了乌鲁木齐市水磨河底泥中有机氯农药HCHs和DDTs的含量,以此来了解水磨河有机氯农药污染情况。结果表明,样品中HCHs和DDTs含量分别为0.107~111.690和0.476~66.512ng/g,其检出率为100%,说明该流域已经普遍受到有机氯农药污染。针对目前的污染现状提出相应的治理措施,以减轻水磨河有机氯农药的污染。     

浙江省水体富营养化特征及防治对策

为研究浙江省水体富营养化特征,对全省历年省控断面地表水水质、污染源和重点藻华高发河流营养盐通量等数据进行了统计分析。结果表明:全省水体营养盐水平总体仍处于高位,重点流域富营养化问题突出,省控断面富营养、重富营养占比分别为78.7%和43.0%,营养盐已持续成为地表水首要污染超标因子。通过近年来的集中整治,浙江省水体营养盐浓度下降明显。但治理过程中也出现了总氮减排滞后,部分水域总磷浓度反弹等不利现象。特别是相应的藻类生长势能尚未进入下降敏感区间,对藻华防控贡献有限。同时,全省入河营养盐城镇生活源和农业面源占比突出,总氮合计占89.27%,总磷占95.45%。重点流域地表径流对营养盐入河通量贡献明显,汛期其对河流总磷浓度的贡献明显高于固定源排放。建议在营养盐总量控制、跨部门协调机制、水资源配置、农业面源管理、城镇雨污管网建设、雨污处理以及河流生态修复等方面加强应对。     

太原汾河景区跨桥断面水体污染的时空变化模式研究

选取太原汾河景区跨桥断面8个监测点,在2012年3月—2013年10月期间对河流8项水质参数进行监测,并结合派生的水体综合污染指数及主成分分析方法分析和评价景区水污染时空变化特征。结果表明,景区水质污染变化时空差异明显,上游污染相对较小,下游污染较重;春季溶解氧和p H值变化幅度最大,夏季除总氮和氨氮外,其他各污染物均有显著变化特征,秋季则以氨氮、总氮和总磷变化最为显著。主成分分析结果显示,虽然各监测点水体污染的关键影响因子不同,但总磷是太原市河流水体污染的共同解释因子。     

宿州市沱河沉积物氮磷和有机碳分布及评价

通过测定沱河宿州城区段沉积物中总氮(TN)、总磷(TP)和总有机碳(TOC)的含量,分析其分布特征,运用C/N和N/P比值法研究其可能来源,采用有机指数和折算后有机氮评价沱河沉积物污染状况。结果表明:沱河城区段沉积物中TN、TP和TOC平均质量比分别为1 343 mg/kg、608 mg/kg和30 201 mg/kg;C/N和N/P比值表明河流底泥沉积物中C、N和P污染可能是外源输入,且受煤炭工业发展影响较大;有机氮达到Ⅲ级,属于尚清洁程度,有机指数达到Ⅳ级,属于有机污染范畴,5号采样点需引起有关部门注意。     

An appraisal of changes in seasonal water quality during passage through a shallow reservoir in Western Poland

Following restoration changes in Antoninek Reservoir physico-chemical and biological processes in the water column and bottom sediments were measured to outline mechanisms of changes in nitrogen, phosphorus and organic matter concentrations during water flow through this reservoir. Intensive mineralisation of organic matter in the shallow sediments stimulated primary production and influenced increasing ammonia and nitrite nitrogen concentrations. Two main factors affected concentrations of phosphorus: (1) its presence in the external loads of river waters entering the reservoir, more important in the colder seasons as the water discharge was higher and (2) from the internal loads coming from bottom sediments. The quality of the river water during its flow through this reservoir improved for most parameters and seasons. However, concentrations of nutrients were still high in waters flowing out from the reservoir and in some months they were higher in the outflow than in waters entering the reservoir.     

Implication of two in-stream processes in the fate of nutrients discharged by sewage system into a temporary river

The aim of this study was to better understand the fate of nutrients discharged by sewage treatment plants into an intermittent Mediterranean river, during a low-flow period. Many pollutants stored in the riverbed during the low-flow period can be transferred to the downstream environments during flood events. The study focused on two processes that affect the fate and the transport of nutrients, a physical process (retention in the riverbed sediments) and a biological process (denitrification). A spatial campaign was carried out during a low-flow period to characterize the nutrient contents of both water and sediments in the Vène River. The results showed high nutrient concentrations in the water column downstream of the treated wastewater disposal (up to 13,315 μg N/L for ammonium and 2,901 μg P/L for total phosphorus). Nutrient concentrations decreased rapidly downstream of the disposal whereas nutrient contents in the sediments increased (up to 1,898 and 784 μg/g for total phosphorus and Kjeldahl nitrogen, respectively). According to an in situ experiment using sediment boxes placed in the riverbed for 85 days, we estimated that the proportion of nutrients trapped in the sediments represents 25% (respectively 10%) of phosphorus (respectively nitrogen) loads lost from the water column. In parallel, laboratory tests indicated that denitrification occurred in the Vène River, and we estimated that denitrification likely coupled to nitrification processes during the 85 days of the experiment was significantly involved in the removal of nitrogen loads (up to 38%) from the water column and was greater than accumulation processes.     

Study of phytopigments in river bed sediments: effects of the organic matter, nutrients and metal composition

Phytopigment estimation has a considerable interest in the evaluation of freshwater bodies' quality, because it takes into account the synergistic effect of nutrients like phosphorus or nitrogen on algal growth producing eutrophication. Furthermore, their increasing concentration constitutes the first step in the formation of biofilms on the surface sediments, adding a new and very important element to the dynamic nature of the surface sediments. In this study the distribution of phytoplankton--in terms of chlorophyll-a, chlorophyll-b, phaeophytin-a, phaeophytin-b, total carotenoids, total chlorophyll, and total phaeophytin--was evaluated in river bed sediments. Samples collected at sites with low levels of nutrients (P,N) and metal concentrations showed lower phytopigment concentrations than those collected at the sampling sites affected by sources of pollution. Phytoplankton concentrations were directly and highly related to the organic matter concentrations--in particular to the humic fraction--as well as to the total nitrogen (N), total phosphorus (P(T)) and available phosphorus (P(A)) concentrations in sediments. In addition, phytoplankton also correlates positively with Cu, Zn, Fe and Al extracted in oxalate, being Cu the variable that most influences the phytopigment growth. These are essential metals for the metabolism of the phytoplankton, so therefore the increase in metal concentrations can increase algal growth, unless they reach toxic levels.     

Hydrology, suspended sediment dynamics and nutrient loading in Lake Takkobu, a degrading lake ecosystem in Kushiro Mire, northern Japan

Suspended sediment and nutrient loadings from agricultural watersheds have lead to habitat degradation in Lake Takkobu. To examine their relationships with land-use activities, we monitored sediment, nutrient and water discharges into the lake for a 1-year sampling period. The Takkobu River contributed the largest portion of the annual water discharge into the lake, compared with the other tributaries. During dry conditions, lake water flowed into the Kushiro River, and conversely during flooding, Kushiro River water flowed into the lake. Inflows from the Kushiro River had a high proportion of inorganic matter, with high concentrations of total nitrogen and total phosphorus, attributed to agricultural land-use development and stream channelization practiced since the 1960s in the Kushiro Mire. Nutrient loadings from these two rivers were significantly higher during flooding than in dry conditions. However, there was no clear correlation between river discharge and nutrient concentrations. Since land-use activities in the Kushiro River and Takkobu River watersheds were concentrated near rivers, nutrients easily entered the drainage system under low flow conditions. In contrast, water discharged from small, forest-dominated watersheds contained a low proportion of inorganic matter, and low nutrient concentrations. The suspended sediment delivered to the lake during the sample period was estimated as approximately 607 tons, while the total nitrogen and total phosphorus inflows were about 10,466 and 1,433 kg, respectively. Suspended sediment input into the lake was 65%, and total nitrogen and total phosphorus were 40% and 48%, respectively, being delivered by the Kushiro River.     

Comparative study of fluvial lakes in floodplains of the Elbe,Lužnice and Svratka Rivers based on hydrochemical and biological approach

The aim of the thesis was to specify key differences in chemistry and biota (zooplankton communities) among fluvial lakes in three regions of the Czech Republic: the central part of the Elbe River, the upper part of the Lu?nice River and the upper part of the Svratka River. The ten studied lakes of the three regions differ in size, geology, shading, connection with the river and the level of anthropogenic impact. The following hypotheses were tested: (1) The water chemistry of fluvial lakes significantly differs in different floodplains. In the central Elbe River floodplain, there are the highest values of conductivity and concentrations of organic matter and nutrients. Fluvial lakes of the Svratka River floodplain show the lowest level of these parameters, and fluvial lakes of the upper Lu?nice River have levels intermediate between the two previous regions. (2) The chemistry of fluvial lakes that have contact with the river through surface connection is significantly influenced by the river. (3) The structure of zooplankton differs in different lakes due to the geographical distance between locations, their different altitude and water chemistry. The PCA analysis of selected parameters of the water chemistry revealed a close relationship of locations in the central Elbe River floodplain on the one side and close relationship of the locations in the upper Lu?nice River and Svratka River on the other. However, the amount of organic matter, nitrogen (with the exception of nitrates) and phosphorus was independent of the region. The relationship between the extent of the lake-river connection and the water chemistry was not significant. The hypothesis that the zooplankton differ in different lakes was not proved—the species composition was similar in all the lakes.     

Physical and chemical characteristics of water from the hydrographic basin of the Poxim River, Sergipe State, Brazil

The Poxim River is one of Sergipe State’s major waterways. It supplies water to the State capital, Aracaju, but is threatened by urban and agricultural developments that compromise both the quantity and the quality of the water. This has direct impacts on the daily lives of the region’s population. In this work, a multivariate analytical approach was used to investigate the physical and chemical characteristics of the water in the river basin. Four sampling campaigns were undertaken, in November 2005, and in February, May, and September 2006, at 15 sites distributed along the Poxim. The parameters analyzed were conductivity, turbidity, color, total dissolved solids, dissolved oxygen, alkalinity, hardness, chlorophyll-a, and nutrients (total phosphorus, dissolved orthophosphate, nitrite, nitrate, ammoniacal nitrogen, and total nitrogen). Dissolved oxygen contents were very low in the Poxim-Açu River (1.0–2.8), the Poxim River (1.6–4.6), and the estuarine region (1.7–5.1), due to the dumping of wastes and discharges of domestic and industrial effluents containing organic matter into fluvial and estuarine regions of the Poxim. Factor analysis identified five components that were indicative of the quality of the water, and that explained 81.73 % of the total variance.     

黑臭河道底泥特征分析及处理工艺筛选

以深圳市前海片区代表性河道黑臭底泥为研究对象,对其p H值、含水率、有机质、氮磷含量、重金属含量及粒径进行分析。结果表明,黑臭底泥主要为呈碱性的无机砂质成分,有机质含量低,重金属含量虽高但分布稳定。根据其特性,最终确定其主要处置方式为疏浚后机械脱水。     

Longitudinal heterogeneity of sediment characteristics during southwest monsoon season in hyper-eutrophic Krishnagiri reservoir,India

Krishnagiri reservoir is a hyper-eutrophicated reservoir located in Krishnagiri district which is one of the drought-prone districts in Tamil Nadu, India. The reservoir water is being used for various purposes such as irrigation, drinking, fish rearing, livestock rearing, and recreation. Since there is no an evidence of investigation on bottom sediments in Krishnagiri reservoir, the present study was carried out during southwest monsoon season in 2008. This study examined the physical and chemical characteristics of the bottom sediments such as composition, redox potential, moisture content, organic carbon, organic matter, total phosphorus, and total iron at 15 locations in the reservoir. Phosphorus fractionation study was carried out to find out different fractions such as loosely adsorbed phosphorous, iron and aluminium-bound phosphorus, calcium-bound phosphorous, and organic phosphorous. Results indicated that there was spatial variation in the composition of sediments and low values of redox potential. The significant positive correlation exists between the organic carbon and organic phosphorus concentration. The lacustrine zone of the reservoir showed high accumulation of total phosphorus and total iron when compared to riverine and transition zones. This study concludes an allogenic origin of majority of inorganic phosphorus in the reservoir during the study period and this might have been derived from the catchment during the erosion process. The high concentration of surface sediment phosphorus clearly indicates a greater threat of eutrophication in Krishnagiri reservoir.     

季节性Kendall检验分析湘江长沙段水质变化趋势

季节性Kendall检验是一种广泛应用于河流水质变化趋势分析的非参数检验。以湘江长沙段三汊矶断面2001—2011年水质监测结果为样本,运用季节性Kendall检验分析湘江长沙段水质变化趋势及影响因素,结果表明:氨氮浓度呈显著上升趋势,总磷浓度呈高度显著上升趋势,总镉、总砷浓度呈高度显著下降趋势,湘江长沙段水质主要受城市生活、工业和农业面源污染物排放的影响,河水流量对水质的影响相对较小。     

A 100-year sedimentary record of natural and anthropogenic impacts on a shallow eutrophic lake, Lake Chaohu, China

In this study, the sediment profiles of total organic carbon, total nitrogen, C/N ratios, total phosphorus, N/P ratios, C/P ratios, particle sizes, and stable carbon and nitrogen isotopes (δ(13)C and δ(15)N) were used to investigate natural and anthropogenic impacts on Lake Chaohu over the past 100 years. Before 1960, Lake Chaohu experienced low productivity and a relatively steady and low nutrient input. The increasing concentration and fluxes of total organic carbon, total nitrogen, total phosphorus, together with changes in the δ(13)C and δ(15)N of organic material in the sediment cores, suggested that the anthropogenic effects on trophic status first started because of an increase in nutrient input caused by a population increase in the drainage area. With the construction of the Chaohu Dam, an increase in the utilization of fertilizer and the population growth which occurred since 1960, stable depositional conditions and increasing nutrient input resulted in a dominantly algae-derived organic matter source and high productivity. Nutrient input increased most significantly around 1980 following the rapidly growing population, with concomitant urbanization, industrial and agricultural development. This study also revealed that the concentration and distribution of nutrients varied between different areas of sediment within Lake Chaohu because of the influence of different drainage basins and pollution sources.