阿图什城市地下水饮用水源地水质状况评价

由于水质评价中存在的不确定性和模糊性,本文采用模糊数学综合评价法对新疆阿图什市水源地地下水中总硬度、溶解性总固体、高锰酸盐指数、氯化物、氟化物、硝酸盐、硫酸盐、氨氮8个水质指标的监测结果进行了数据处理,对地下水的水质进行综合评价。结果表明,6个取水井和市水厂的水质符合地下水质量标准Ⅱ级及以上水质标准。该方法反映出水环境系统的模糊性,评价的结果更具有说服性。     

饮用水源水质评价指数法探讨

对水利部水环境监测评价研究中心定期向社会发布的部分重点城市主要供水水源地水资源质量旬报所采用的评价方法——水质指数法进行了分析,针对该方法存在的缺陷提出了改进的水质指数法。     

东营市地下水碘化物的空间分布特征及影响分析

为研究东营市地下水碘化物的空间分布特征以及对环境和饮用水安全的影响,对域内的山前平原区和黄泛平原区分别布设了48个和47个调查点位。结果表明:东营市地下水碘化物质量浓度均值达到(0.247±0.263) mg/L,其环境质量呈现由南向北逐步恶化的变化趋势,超过90%的国土面积处于地下水环境质量标准Ⅳ类。山前平原区南部是东营市唯一具备可饮用地下水的区域,域内以适碘地区为主,缺碘地区和高碘地区分别位于区域东南部和第二次海侵古海岸线附近。总体上,可饮用地下水处于中等缺碘水平,海(咸)水入侵已成为影响可饮用地下水适碘地区范围的关键因素,需引起高度关注。地下水所处的环境地质概况、海(咸)水入侵和大气降水是影响碘化物空间分布的重要因素。     

长江口北支湿地资源和环境现状调查

调查了长江口支湿地环境现状，分析了评价长江口北支湿地的环境质量。指出，长江口北支湿地有着得天独厚的地理位置和自然条件，是世界范围内极具代表性十分重要的湿地，拥有丰富的水资源，动植物资源，滩涂资源等。近年来，由于长江上游河水质量下降，启东和海门经内河流向长江的城市生活污水，启东沿江建设的工业带，对北支口湿地环境质量产生了较大的影响。调查结果表明，长江口北支口水域主要污染物为COD，氨氮等，其污染程度呈现出以下规律：平水期（污染）＞丰水期（污染）＞枯水期（污染）。长江口北支区域陆地土壤中主要污染物为重金属元素镉，铅，锌以及滴滴涕，其中镉与滴滴涕达《土壤环境质量标准》（GB15618－1995）中三级标准，其他指标达一级标准。     

乌鲁木齐河地表水化学组成及时空分布特征

乌鲁木齐河作为乌鲁木齐市的主要水源地,在生态保护和城市供水中均具有重要的战略意义。为了研究乌鲁木齐河水化学特征及水环境质量,于2016年4—10月逐月对乌鲁木齐河6个采样断面进行地表水样采集,获取水样41个,对主要离子(K~+、Na~+、Ca~(2+)、Mg~(2+)、Cl~-、HCO_3~-、SO_4~(2-))浓度及pH、DO、TDS、CODMn、TN、TP、NH3-N进行监测分析,探讨了水化学组成的时空差异及影响因素,研究了乌鲁木齐河的水环境质量状况。结果显示,乌鲁木齐河水域年离子总量平均值为213.27 mg/L,属弱矿化度水,年离子总量在空间上表现出沿主河道由南向北逐步增加的趋势。主要阴离子为HCO_3~-和SO_4~(2-),主要阳离子为Ca~(2+),水质类型为Ca~(2+)-HCO_3~--SO_4~(2-)型。2016年河水年内不同时期TDS平均浓度排序为:9月10月4月5月6月8月7月。对水化学离子含量基于时间序列分析,结果显示除Ca~(2+)、HCO_3~-外,其他离子含量在各月份间均存在显著差异。SO_4~(2-)浓度在年内变化最为明显,呈现先减少后增加的趋势。对主要离子含量基于空间序列进行分析,结果显示,仅Na+含量存在显著差异。现阶段乌鲁木齐河的水环境质量为轻度污染。     

因子分析法在金泉工业园区地下水水质评价中的应用

根据金泉工业园水源地8个不同监测断面的地下水水质监测数据,采用R型因子分析法对园区水源地地下水水质进行综合评价,在研究地下水中13种化学成分间相关关系的基础上,提取4个主因子进行分析计算。结果表明,Cl-、SO24-、总硬度和可溶性固体对第一主因子贡献明显;第二主因子代表指标是Zn;第三主因子代表指标是As;NO3-、氨氮、NO2-对第四主因子贡献显著。对水质进行综合评价后发现,人民渠、海流图河和乌拉壕监测断面处水质类别为V类,其他断面均为IV类。因子分析法从整体上评价了园区水源地地下水的水质现状,分析结果清晰明确,为日后地下水资源的管理与保护提供科学依据。     

某碱渣堆放场对岩溶地下水的影响分析

结合某碱渣堆放场的水文地质状况,通过模拟试验,探讨了碱渣堆放场对岩溶地下水的影响。结果表明,碱渣场在冲灰水和大气降水的浸泡、淋滤作用下,其中的氯化物和钙镁盐类大量析出并随碱渣废液一起下渗,石灰岩碎石对氯化物有一定的吸附作用,但能力微弱。据试验数据分析认为,该渣场是焦作市北中部岩溶地下水中氯化物浓度和总硬度持续升高的主要原因。     

无锡市地下水环境质量调查与评价

为了解无锡市地下水水质状况,于2010年10—12月对无锡地区145口地下水井进行采样分析。以地理信息系统为技术手段,对不同土地利用类型和地下水类型的水污染物监测结果进行综合评价。结果表明,无锡全市地下水达标率为45.52%,整体水质情况处于"较好"级别;NH3-N、Mn和Fe为无锡市地下水的主要污染物;无锡市农业和建设用地区域地下水的污染程度整体要高于水体和林地区域;承压层的地下水污染较为严重。提出,无锡市管理部门应根据地下水污染现状,对地下水资源进行动态监测(包括水量和水质监测),并采取强有力的保护与治理措施,以实现区域水资源的持续利用。     

长江南京段不同径流 潮汐动力作用下突发污染事故对饮用水水源地的影响研究

长江南京段水动力条件复杂,突发污染事故对下游饮用水水源地影响难以预测。基于构建的长江南京段二维水动力水质耦合数学模型,对不同径流潮汐动力作用下的突发污染事故进行模拟,分析其对长江水源地的影响。结果表明:洪季径流作用较强,污染团扩散速度受潮汐影响较弱,各水源地受污染团的影响时长基本接近,约为2.5~3.5 h。枯季径流作用减弱,污染团扩散速度受潮汐影响增强,越下游处受潮汐影响越大,各水源地受污染团的影响时长依次为:长江江浦水源地<燕子矶水源地<龙潭水源地。枯季污染物传播时的浓度大于洪季,洪季污染物传播浓度呈现随距离增大浓度减小的趋势。枯季流速受到潮汐影响,径流稀释作用减弱,使得污染物经八卦洲分流后的浓度略小于传播向下游的浓度。     

宜昌城区地下水总硬度升高与污染物相关多元分析

水质硬度增高对人体健康、对城市工业生产成本及能源的消耗,均具有很大的影响.本文针对宜昌城区地下潜水总硬度升高的水环境问题,运用多元回归分析方法,寻找出导致地下潜水总硬度升高主要原因及污染物主要“贡献者”,为保护地下水资源质量,提出了切实可行的研究治理办法.     

Influence of changes in hydrodynamic conditions on cadmium transport in tidal river network of the Pearl River Delta, China

With rapid economic development, the Pearl River Delta (PRD) of China has experienced a series of serious heavy metal pollution events. Considering complex hydrodynamic and pollutants transport process, one-dimensional hydrodynamic model and heavy metal transport model were developed for tidal river network of the PRD. Then, several pollution emergency scenarios were designed by combining with the upper inflow, water quality and the lower tide level boundary conditions. Using this set of models, the temporal and spatial change process of cadmium (Cd) concentration was simulated. The influence of change in hydrodynamic conditions on Cd transport in tidal river network was assessed, and its transport laws were summarized. The result showed the following: Flow changes in the tidal river network were influenced remarkably by tidal backwater action, which further influenced the transport process of heavy metals; Cd concentrations in most sections while encountering high tide were far greater than those while encountering middle or low tides; and increased inflows from upper reaches could intensify water pollution in the West River (while encountering high tide) or the North River (while encountering middle or low tides).     

长江源区河流及典型湖泊丰水期水质与鱼类群落分析

为加强长江源区水生态研究,于2017年丰水期调查了长江源区5个湖泊、5条河流的水质和鱼类资源状况,并研究了其空间格局.水质综合指数(WQI)计算结果显示,长江源区WQI范围为41～87,评价等级介于差到良好之间,大部分采样点的水质评价等级为一般,其中,班德湖的水质评价等级为良好.主成分分析结果显示,长江源区河流、淡水湖...     

泰东河疏浚工程对通榆河水质的影响

为了解泰东河疏浚工程对通榆河水质的影响,于2012年6月8日、9月12日、12月6日,对泰东河沿线以及通榆河东台段进行调查取样,分析施工期间河体水质变化。结果表明,施工期间水质参数基本保持在Ⅱ~Ⅲ类。根据江苏省水环境监测中心盐城分中心2011年、2013年监测资料评价分析,泰东河河道疏浚后,清理了河床淤泥,提高了泰东河的行洪、抗洪以及通航能力,其水质的好转有效地改善了下游通榆河的水质,确保了饮水安全。     

The influences of weir construction on salt water intrusion and water quality in a tidal estuary—assessment with modeling study

A three-dimensional hydrodynamic and water quality model was developed and applied to predict the changes in physical and biochemical processes that would result from the proposed Dadu Weir construction in the Wu River estuary, located in central Taiwan. A high-resolution unstructured grid was constructed to represent the narrow channels in the tidal estuary. The model was calibrated and verified with available hydrographic and water quality data measured in 2011. The overall performance of the model is in reasonable agreement with the measured water level, salinity, and water quality state variables. The model was then used to investigate the changes in salt water intrusion and water quality as a result of weir construction under low-flow conditions. The model simulations indicate that more tidal energy will propagate into the estuary after weir construction because of decreased freshwater discharges. The limits of salt water intrusion before and after weir construction coincide at a distance of 11.6 km from the mouth of the Wu River. This salt water intrusion limit is the reason that the Dadu Weir will be constructed at a distance of 12 km from the mouth of the Wu River. The weir will become a barrier to salt water intrusion. The simulation results indicate that the concentrations of dissolved oxygen and nutrients will decrease slightly after weir construction, while the chlorophyll a concentration in the middle reach will increase after weir construction. However, construction of the weir is predicted to have little influence on water quality conditions downstream of the Wu River estuary. The results of this case study provide quantitative estimates of the physical and biochemical changes expected to occur in this nature system due to human action.     

Water pollution of Sabarmati River—a Harbinger to potential disaster

River Sabarmati is one of the biggest and major river of Gujarat that runs through two major cities of Gujarat, Gandhinagar and Ahmedabad and finally meets the Gulf of Khambhat (GoK) in the Arabian Sea. A study was conducted to evaluate the water quality of this river, as it could possibly be one of the major sources for filling up Kalpasar, the proposed man-made freshwater reservoir supposed to be the biggest one in the world. A total of nine sampling stations were established covering 163 km stretch of the river from upstream of Gandhinagar city to Vataman near Sabarmati estuary. Physicochemical (temprature, pH, salinity, chloride, total dissolved solids, turbidity, dissolved oxygen, biochemical oxygen demand, phenol, and petroleum hydrocarbons), biological (phytoplankton), and microbiological (total and selective bacterial count) analyses indicated that the river stretch from Ahmedabad-Vasana barriage to Vataman was highly polluted due to perennial waste discharges mainly from municipal drainage and industries. An implementation of sustainable management plan with proper treatment of both municipal and industrial effluents is essential to prevent further deterioration of the water quality of this river.     

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。     

基于在线自动监测的钦州湾海域水质参数周年时空变化特征

通过分析位于钦州湾的2个海水水质自动监测站2009-2010年的自动监测数据，发现钦州湾水温、盐度、溶解氧季节变化明显，海水表层水温变化是引起钦州湾溶解氧含量变动的主要原因；钦州湾海水表层盐度及pH值主要受钦江、茅岭江径流及潮汐涨落的影响；处于河口区域，受大陆径流影响显著的海域使用海水水质标准来评价有欠妥当。     

Fluoride in groundwater, Varaha River Basin, Visakhapatnam District, Andhra Pradesh, India

Excess intake of fluoride through drinking water causes fluorosis on human beings in many States of the country (India), including Andhra Pradesh. Groundwater quality in the Varaha River Basin located in the Visakhapatnam District of Andhra Pradesh has been studied, with reference to fluoride content, for its possible sources for implementing appropriate management measures, according to the controlling mechanism of fluoride concentration in the groundwater. The area occupied by the river basin is underlain by the Precambrian Eastern Ghats, over which the Recent sediments occur. Results of the chemical data of the groundwater suggest that the considerable number of groundwater samples show fluoride content greater than that of the safe limit prescribed for drinking purpose. Statistical analysis shows that the fluoride has a good positive relation, with pH and bicarbonate. This indicates an alkaline environment, as a dominant controlling mechanism for leaching of fluoride from the source material. Other supplementary factors responsible for the occurrence of fluoride in the groundwater are evapotranspiration, long contact time of water with the aquifer material, and agricultural fertilizers. A lack of correlation between fluoride and chloride, and a high positive correlation between fluoride and bicarbonate indicate recharge of the aquifer by the river water. However, the higher concentration of fluoride observed in the groundwater in some locations indicates insufficient dilution by the river water. That means the natural dilution did not perform more effectively. Hence, the study emphasizes the need for surface water management structures, with people's participation, for getting more effective results.     

Environmental impact assessment and seasonal variation study of the groundwater in the vicinity of River Adyar, Chennai, India

Hydrochemical investigations of the groundwater and the seasonal effect on the chemical budget of ions along the course of the polluted river Adyar were carried out. From the geochemical results, it has been found that the seasonal effect does not change the order of abundance of both cations and anions, but it does change the concentration of various ions present in the groundwater. Among the chemical budget of ions, sodium and chloride were found to be the most predominant ions. The nitrate concentration in the groundwater ranges from 4.21 to 45.93 mg/l in pre-monsoon and in post-monsoon it ranges from 1.02 to 75.91 mg/l. The nitrate concentrations in the post-monsoon are high in some places especially in the upper stretch of the river. The intense agricultural activities near the upper stretch of the river may be an important factor for the higher concentration of nitrates in these aquifers. In order to determine the geochemical nature of water, the data was interpreted using the piper diagram wherein the results show the predominance of NaCl and CaMgCl types. Equiline diagrams, 1:1, were applied to evaluate the affinity ion relationship between various ions present in these waters. The quality of the groundwater was assessed with regard to its suitability to drinking and irrigation. A comparison of the groundwater quality in relation to drinking water quality standards shows that most of the water samples are not suitable for drinking, especially in post-monsoon period. US Salinity Laboratory's, Wilcox's diagrams, Kellys ratio and magnesium ratio were used for evaluating the water quality for irrigation which suggest that the majority of the groundwater samples are not good for irrigation in post-monsoon compared to that in pre-monsoon. Moreover the source of the ions in the water was examined and classified accordingly using Gibb's diagram. The analytical results reveals that the TDS values of the pre-monsoon samples were found to be lower than the post-monsoon reflecting that leaching predominates over that of the dilution factor.     

Water Environmental Degradation of the Heihe River Basin in Arid Northwestern China

Water environmental degradation is a major issue in the Heihe River Basin belonging to the inland river basin of temperate arid zone in northwestern China. Mankind’s activities, such as dense population and heavy dependence on irrigated agriculture, place immense pressure on available and limited water resources during the last century, especially the recent five decades. An investigation on the water environmental degradation in the Heihe River Basin and analysis of its causation were conducted. The results indicated that water environmental changes in the whole basin were tremendous mostly in the middle reaches, which reflected in surface water runoff change, decline of groundwater table and degeneration of surface water and groundwater quality. Some new forms of management based on traditional and scientific knowledge must be introduced to solve problems of water environmental degradation in the Heihe River Basin.