北大港水库调蓄“引江水”水质变化

通过模拟实验研究了北大港水库底泥释放氯离子的规律,建立了数学模型。采用2 0 0 3年第8次“引黄济津”水质监测数据,验证了模型的有效性。最后,利用该数学模型,预测了南水北调“引江水”在水库中调蓄时的水质变化。认为在合理调度运用的情况下,根据工程规划,北大港水库可以满足作为南水北调调蓄水库的水质要求     

阜阳电厂灰水氟化物浓度的确定及对地下饮用水源污染预测

目前在火电厂环境影响评价中，主要利用类比法和实验法确定灰水中氟化物的浓度。文章提出了一种新的方法－－计算法。该方法以氟的迁移转化规律为基础，以物料平衡原理为依据，充分考虑煤源、煤质、除尘方式、除灰方式、排灰方式及冲灰水水质等影响因素。与类比法和实验法相比，该法简便、可靠、实用、经济。鉴于阜场附近地区地下水饮用水源污染的可能性，影响程度及发生时间。     

Impact of drought on the ecological and chemical status of surface water and on the content of arsenic and fluoride pollutants of groundwater in the province of Salamanca (Western Spain)

The impact of drought on the ecological and chemical status of surface and groundwaters of the River Tormes (River Duero basin, northwestern Iberian Peninsula) was studied to evaluate the evolution of the quality of the river during its passage through the city of Salamanca (Spain). The Water Quality Index (WQI) of the river revealed that the drought period of 2005 did not significantly affect water chemical quality. However, during the study period differences were found in surface water ecological quality, using phytoplankton quality as AN indicator. These differences may be accentuated as a result of regulation of the River Tormes by the Santa Teresa reservoir. Arsenic and fluoride concentrations were measured in water wells, finding higher arsenic concentrations after the drought period and no correlation between the arsenic and fluoride contents. The results are useful for an overall understanding of potential impact of climate change on the ecological and chemical status of water in regional systems.     

Ground water pollution by pesticides at the watershed‐soil catena scale: Lindane at the lower Colorado river basin (Argentina)

The movement of Lindane from application points at the surface soil towards the underground water and further transport within this compartment at the watershed‐soil catena scale, was inspected by measurements of the pesticide concentration in soil water at a controlled experiment where it was applied at a usual label dose. The concentrations of Lindane in soil water and the upper phreatic level were also measured at successive dates in samples obtained from a net of phreatimeter probes distributed over the area (1,500 km²) of the lower Colorado River basin (Bs. Aires, Argentina). The location of cultivated‐irrigated areas within the watershed was inferred from NDVI (Normalized Difference Vegetation Index)‐1 km‐10 day AVHRR images obtained at successive dates during the irrigation season. Feasible paths of underground gravitational water flows were computed by means of a GIS‐simulation model on the basis of local terrain slopes and aspects. The pattern of Lindane distribution over the basin was explained on the basis of the distribution of diffuse sources, the patterns of percolation and groundwater flows and the thermodynamic characteristics of the pesticide.     

运用主成分分析法评价北京市代表性河流的水质与毒性状况

以北京市3条具有不同功能的代表性河流(清河:纳污排洪;京密引水渠:供水水源;小月河:景观用水)作为研究对象,分析测定了33个水质指标,采用内梅罗指数法与大型蚤急性毒性测试法对3条河流的水质与毒性状况进行了评价,同时运用主成分分析法对毒性产生的原因和影响水质的因素进行了初步探讨.结果表明,1)3条河流已受到不同程度的污染,水质和毒性状况均不容乐观.作为纳污排洪的清河大部分采样点水质较差,生物毒性极高;作为景观用水的小月河水质一般,具有一定的生物毒性;作为供水水源的京密引水渠水质一般,但毒性较低.2)水样生物毒性与Cl-、Ca、K、Li、Mn、Na、Cr、Ni等指标有关;内梅罗水质指数与NO2-、Cl-、K、Na、Ni等指标有关.3)某些指标(如NO2-)超标会对水质分级产生较大影响,但对生物毒性贡献不大,而低浓度的重金属,不会对水质分级产生贡献,却会对生物的生理活动产生影响,综合化学指标和毒性指标共同评价水质更为合理.     

再生水回灌地下水环境安全风险评价技术方法研究

再生水回灌是水资源管理的一条有效途径,也是污水再生利用的重要发展方向。然而,当再生水以农灌、土壤含水层处理（SAT）、河湖入渗和井灌等方式进行地下水回灌时,不可避免的会在回补地下水的过程中造成对地下水环境的污染风险。针对不同回灌方式建立适用于我国的再生水回灌地下水环境安全风险评价技术体系至关重要。借鉴国内外地下水污染风险评价方法,综合分析再生水回灌对地下水产生风险的关键环节,采用层析分析法,从回灌水特征污染物特性、回灌区地下水固有脆弱性以及回灌工程布设方式3个方面,针对地表灌溉、河湖入渗和井灌3种回灌方式,建立了包含污染物浓度水平、分配系数、溶解度、半衰期、半致死剂量、地下水埋深、降雨入渗补给量、地形坡度、土壤介质、包气带介质、含水层介质、含水层厚度、回灌强度、回灌周期、回灌水停留时间以及取水点与回灌点水平距离16个指标在内的风险评价指标体系。在此基础上,结合地下水使用功能,以20个典型再生水回灌场地调研结果和160种再生水回灌地下水污染风险因子物化特性为数据基础,对各指标进行了风险水平的划分,基于聚类分析法,采用各指标风险指数相乘的风险表征方法计算总风险指数,构建了再生水回灌地下水环境安全风险评价技术方法。该方法有效的避免了指标权重计算的主观性,并且能够直观的找出导致风险的主要因素。结果表明：利用建立的风险评价技术方法可将我国再生水回灌地下水环境安全风险划分为3级,风险值〈5为一级,风险值在5-15之间为二级,风险值〉15为三级。在某再生水回灌场地的应用表明,该回灌区地下水环境安全风险为二级,同时得出回灌水特征污染物特性指标是造成该回灌区地下水环境风险的主要因素。     

Integrating wetlands and riparian zones in river basin modelling

Wetlands, and in particular riparian wetlands, represent an interface between the catchment area and the aquatic environment. They control the exchange of water and related chemical fluxes from the upper catchment area to surface waters like streams and lakes. Their influence on water and nutrient balances has been investigated mainly at the patch scale. In this study an attempt was made (a) to integrate riparian zones and wetlands into eco-hydrological river basin modelling, and (b) to quantify the impacts of riparian wetland processes on water and nutrient fluxes in a meso-scale catchment located in the northeastern German lowland. The investigation was performed by analysing hydro-chemical field data and applying the eco-hydrological model SWIM (Soil and Water Integrated Model), which was extended to reproduce the relevant water and nutrient flows and retention processes at the catchment scale in general, and in riparian zones and wetlands in particular. The main extensions introduced in the model were: (1) implementation of daily groundwater table dynamics at the hydrotope level, (2) implementation of water and nutrient uptake by plants from groundwater in riparian zones and wetlands, and (3) assessment of nutrient retention in groundwater and interflow. The simulation results indicate that wetlands, though they represent relatively small parts of the total catchment area, may have a significant impact on the overall water and nutrient balances of the catchment. The uncertainty of the simulation results is considerably high, with the main sources of uncertainty being the model parameters representing the geo-hydrology and the input data for land use management.     

北京部分地区地下水中全氟化合物的污染水平初探

全氟化合物(perfluorinated compounds,PFCs)因具有持久性、生物蓄积性和毒性,近年来得到全世界的广泛关注。我国对PFCs环境污染水平的研究主要集中在污水、河水、湖水等浓度较高的水体,针对地下水中PFCs的存在情况研究较为缺乏。为了解北京市地下水中PFCs的污染水平,采集和分析了6个采样地段26眼监测井中的地下水。结果表明:18种目标PFCs中有11种存在不同程度的检出,以C4~C9的全氟羧酸(MQLs~42.9 ng·L-1)和C4~C8的全氟磺酸(MQLs~23.2 ng·L-1)为主。风险评价结果显示,地下水中PFCs未达到对生态环境和人体健康具有风险的水平。本研究提供了北京地区地下水中PFCs污染水平的初步数据,有利于后续开展地下水中PFCs监测和风险评估等研究。     

高效液相色谱-串联质谱法同时检测水体中26种药物及个人护理品

通过优化固相萃取条件和高效液相色谱-串联质谱参数,建立了可以同时检测地表水和地下水中26种典型药物及个人护理品(pharmaceuticals and personal care products,PPCPs),包括磺胺类、大环内酯类、喹诺酮类、酰胺醇类、精神类、消炎止痛类以及个人护理品的检测方法.通过将水样pH值调节至7,利用HLB固相萃取柱对水样中PPCPs进行富集,以甲醇和含0.005%甲酸的水溶液作为正离子模式流动相,甲醇和含0.5 mmol·L^-1乙酸铵的水溶液作为负离子模式流动相进行梯度洗脱,采用多反应监测的质谱扫描模式(MRM)分析测定.26种PPCPs的检出限为0.007—1.78 ng·L^-1,定量限为0.02—5.68 ng·L^-1,回收率为52.28%—115.24%.利用该方法检测北京潮白河地表水和地下水中PPCPs的浓度,结果表明,地表水中PPCPs的含量普遍高于地下水,磺胺甲恶唑、舒必利、咖啡因、卡马西平和布洛芬在地表水和地下水中的含量相对较高,检测浓度分别高达147.83、52.48、78.35、166.58、30.63 ng·L^-1.     

A modeling system for drinking water sources and its application to Jiangdong Reservoir in Xiamen city

Drinking water sources are highly valued by authorities for safeguarding the life of a city. Models are widely applied as important and effective tools in the management of water sources. However, it is difficult to apply models in water source management because water managers are often not equipped with the professional knowledge and operational skills necessary for making use of the models. This paper introduces a drinking water source simulation and prediction system that consists of a watershed model, a hydrological model and a water quality model. This system provides methods and technical guidance for the conventional management of water sources and emergency water event response. In this study, the sub-models of the system were developed based on the data of the Jiangdong Reservoir in Xiamen, and the model validation was based on local monitoring data. The hydrological model and water quality model were integrated by computer programming, and the watershed model was indirectly integrated into the system through a network platform. Furthermore, three applications for Jiangdong Reservoir water protection utilizing the system were introduced in this paper, including a conventional simulation, an emergency simulation, and an emergency measures evaluation.     

Modelling the impacts of land-use and drainage density on the water balance of a lowland–floodplain landscape in northeast Germany

This study presents the modelling approach and impact assessment of different strategies for managing wetland water resources and groundwater dynamics of landscapes which are characterised by the hydrological interactions of floodplains and the adjacent lowlands. The assessment of such impacts is based on the analysis of simulation results of complex scenarios of land-use changes and changes of the density of the drainage-network. The method has been applied to the 198 km² Lower Havel River catchment as a typical example of a lowland–floodplain landscape. The model used consists of a coupled soil water and groundwater model, where the latter one is additionally coupled to the surface channel network. Thus, the hydrological processes of the variable saturated soil zone as well as lateral groundwater flow and the interactions between surface water and groundwater are simulated in an integrated manner. The model was validated for several years of significantly different meteorological conditions. The comparison of lateral and vertical water balance components showed the dominance of lateral flow processes and the importance of the interactions between surface water and groundwater for the overall water balance and the hydrological state of that type of landscape.The simulation of land-use change scenarios showed only minor effects of land-use change on the water balance and groundwater recharge. Changes of groundwater recharge were particularly small within the wetland areas being part of the floodplain where interactions between surface water and groundwater are most pronounced. Alterations in vertical groundwater recharge were counter-balanced by the lateral interaction between groundwater and surface water. More significant deviations in groundwater recharge and storage were observed in the more peripheral areas towards the catchment boundaries which are characterised by greater groundwater distance from the surface and less intense of ground water–surface water interactions.However, the simulation results assuming a coarsening of the drainage network density showed the importance of drainage structure and geometry for the water balance: The removal of the artificial draining ditches in the floodplain would result in significant alterations of total groundwater recharge, i.e., less recharge from winter to early summer and an increase of groundwater recharge during summer and autumn. Furthermore the different effects of groundwater recharge alterations on the dynamics of groundwater stages within the wetland areas close to the floodplains compared to the more peripheral areas could be quantified. Finally, it will be discussed that a well-adjusted co-ordination of different management measures is required to reach a sustainable water resources management of such lowland–floodplain landscapes.     

基于BP神经网络算法的密云水库水质参数反演研究

密云水库是北京市重要的地表饮用水源地,在保障首都水源安全方面起着重要作用,而密云水库水质参数的区域监测已成为当前亟待解决的问题。为了实现密云水库水质参数大范围、实时获取,该文基于遥感和GIS技术,采用BP神经网络算法,结合地面监测数据和Landsat 8遥感影像,分别建立了反演总磷、总氮、氨氮和COD(化学需氧量)4个水质参数的BP神经网络模型,并反演了密云水库2013-2018年非结冰期主要水质参数,分析了密云水库主要水质参数的年际变化特征、季节变化特征和空间分异特征。结果表明,(1)水质参数的Landsat 8敏感波段分别为:总氮为1、4波段,氨氮为1-7波段,总磷为1、3-7波段,COD为2-5波段。(2)密云水库主要水质参数在2013-2018年总体呈下降趋势,氨氮和COD为Ⅰ类水质,总磷为Ⅱ类水质,总氮为Ⅲ类水质。(3)4个水质参数指标春季最高、秋季次之、夏季最低,总氮、总磷、氨氮和COD的春季值分别是夏季值的1.08、1.36、1.6、1.45倍。(4)密云水库不同水质参数的空间差异性较大,总体来看,水库北部和东部的4个水质参数含量相对较高,这种分布与北部和东部村庄密集以及密云水库两大入库河流有关。综上所述,基于BP神经网络算法的密云水库水质反演研究是可行的,且得到了较为可信的研究结果,该研究可为密云水库水质管理与政策制定提供重要的科学依据。     

广花盆地地下水化学特征及其演化分析

粤港澳大湾区(简称大湾区)建设已经上升为中国国家重大发展战略,水资源保障能力提升是大湾区建设的重点内容。城市应急备用水源建设是解决区内供水风险、保障特殊时期供水安全的重要手段,查明水环境质量状况及其演化对于备用水源地的科学建设意义重大。以粤港澳大湾区应急备用水源地-广花盆地为研究对象,采集并测试了41口监测井水样的常规化学组分,利用主成分分析、元素比值和Gibbs模型等多种方法,探讨了地下水主要离子来源及控制因子,评估了水质状况。结果表明:地下水的TDS变化范围为51.42-1 293.36 mg·L-1,Cl-为1.81-858.65 mg·L-1,淡水样占比95.1%,微咸水占比4.9%,反映地下水化学具有较大的空间差异;地下水阳离子以Ca2+和Na+为主,阴离子以HCO3-和Cl-为主,为HCO3-Ca、HCO3-Na·Ca、HCO3·SO4-Na·Ca和HCO3·Cl-Na·Ca型水;地下水的ρ(Na+)/ρ(Na++Ca2+)值为0.02-0.59,ρ(Cl-)/(Cl-+HCO3-)值为0.03-0.88,Ca/Na值为0.69-52.66,HCO3/Na值为1.28-41.64,据Gibbs模型和元素化学计量分析表明,其化学组成主要受含水层碳酸盐岩和硅酸盐岩风化控制;Na/Cl系数为0.31-6.39,局部地下水盐化明显,在北部高Cl-质量浓度区,其主要受古咸水与现代淡水混合影响,并有Na+与Ca2+离子交换,在南部的高Cl-质量浓度区,可能是海水沿流溪河咸潮上溯和河流侧向补给地下水所致;氨氮为0.05-7.50mg·L-1,有75.6%的样品超过Ⅲ类水标准,其主要来源为农业施肥、人畜粪便。由此,氨氮污染威胁地下水安全,作为应急备用水源应引起高度重视。     

北方城市干涸河流生态环境治理途径

以滹沱河石家庄市区段为例,针对目前我国北方城市干涸河流治理和改造存在的问题,提出"以绿代水"的生态恢复与重建模式。在对河流进行生态输水、水资源合理管理与调度的同时,选择适宜的研究尺度,恢复流域内自然植被,实现河道中心区草本滞洪补潜、缓冲区灌木束水导流、杨柳护堤造岸、过渡区林果防风固沙的"绿色滹沱",为北方城市干涸河流的生态环境治理提出新的理念和途径。     

盐渍土系统土壤水-地下水转化规律研究

通过野外定位观测和室内分析,探讨了苏打盐渍土微域特征(32m长的横截面)及其水分和地下水之间的转化规律。结果表明:土壤特征以及微地貌格局是制约土壤表层水分迁移的主要因素,并由此形成了大汽降水-土壤水-地下水转化的特殊模式。盐化草甸土分布在相对低洼的部位,苏打碱土分布在微坡地和高平地。苏打碱土质地为粉砂质亚粘土-粘土-粉砂-砂砾垂直结构,盐化草甸土以粉砂和砂砾结构为主。地表径流为水分迁移的关键环节,盐化草甸土成为地表水和地下水转化的通道。承接微坡地和高平地的径流,盐化草甸土在雨季含水率较多(甚至大到饱和)且迅速补给地下水,使地下水位逐渐上升。坡地土壤(苏打盐渍土)整个土层的含水率变化不显著。运用Vensim对盐渍土系统的土壤水-地下水的转化过程进行了模拟,结果与观测数据基本一致。在现代盐渍化过程研究中,以坡面系统为研究单元并考虑坡面径流,才能认识到盐渍化地区土壤水-地下水之间转化的实质。     

种间关系预测(ICE)模型在水质基准研究中的应用

水质基准研究主要是基于物种的实验室测试的毒性数据开展的。对于一些毒性数据相对缺乏的化学品,水质基准研究就会受到一定的影响。本文从水质基准研究方法的角度,阐述了种间关系预测(ICE)的基本原理和基本方法,系统介绍了ICE模型的毒性预测方法在水质基准研究中的应用,并通过锌的ICE案例研究证明了模型在中国的可利用性。同时,对ICE模型的不确定性和适用性进行了分析。最后,对ICE模型存在的问题和未来的发展方向进行了探索和展望。     

北京市郊再生水灌区土壤有机氯农药垂向分布特征

在北京市郊再生水灌区采用正三角型布点法进行了3个钻孔的采样工作,钻孔间隔为1m,从表层开始每隔0.5m取一个样,3个钻孔共36组样品,同时采集钻孔附近的灌溉水及地下水,分别测试了土壤的理化参数及其土壤、灌溉水及地下水中9种有机氯农药的质量分数。测试结果表明：表层土壤是有机氯农药的主要残留层,表层土壤中检出的DDTs和BHCs质量分数较高,分别为2814.21ng·kg^-1和1130.41ng·kg^-1,但均符合土壤环境质量一级标准,残留污染程度较轻;其他层位以七氯和艾氏剂为主要检出物,最高质量分数分别为1286.19ng·kg^-1和781.23ng·kg^-1;其中艾氏剂未在表层土壤中检出;灌区内未检出的γ-BHC和（DDE＋DDD）/DDT的计算值为1.80,都说明近期内没有新污染源的输入;检出的有机氯农药在土壤剖面上的迁移能力有HEP〉ALD〉BHCs〉DDTs〉HCB,与地下水中检出的规律一致。     

太行山山前平原区地下水下降对该区土壤性质的影响

太行山山前平原区的地下水持续下降,对土壤成土条件产生了重大影响。通过对太行山山前平原区地下水及地下25 m内土层的土壤含水量进行研究,发现由于该区地下水下降引起饱和含水量土壤层由原来的地下1-2米,演变成现在的30-40米以下,土壤水库储水量显著降低;通过毛管水上升模拟试验,证实地下水已经不再参与土壤的形成过程,该区土壤的成土条件已经发生变化,土壤由潮土向褐土的方向发展。     

北京和上海市居民冬夏两季饮用水消费习惯

饮用水是人体暴露于有毒物质的重要暴露源,为了定量描述饮用水中污染物对暴露人群所造成的危害,世界各国的科学家们对饮用水的健康风险评价做了大量的研究.通常,健康风险评价需要污染物毒理学数据和暴露人群的暴露剂量数据.目前,针对很多的有毒污染物,国际上已经建立了应用于健康风险评价的毒理学数据库,同时积累了大量可用的有效数据.而对于暴露人群的暴露剂量数据,则是健康风险评价所要研究的重点.正确估计暴露人群的暴露剂量需要消费者提供大量的消费信息.例如,暴露人群每天消费的饮用水水量.美国环保局(EPA)认为成人每天消耗的饮用水水量为2L·d-1,此外,饮用水的消耗量会随着暴露人群的身体活动状况和所处环境状况(温度,湿度等)的改变而改变.目前,许多研究都是关于饮用水消费信息的,总体来讲这些研究结果基本上与美国环保局所采用的饮水消耗数据相一致.需要说明的是中国居民有完全不同于西方人的饮用水消费方式,如果在进行中国居民饮用水健康风险评价过程中应用美国环保局的假设会带来较大的不确定性.饮用水健康风险评价工作在我国开展并不多,尤其缺少中国居民饮用水消费习惯的数据库.这些客观条件使得在我国进行饮用水健康风险评价时只能从基础做起,积累有效的数据.本研究以北京和上海两座城市居民为研究对象,2002年到2004年分冬夏两季分别进行了4次饮用水消费习惯调查.研究采用随机入户方式(2004年至2005年),与中央电视台-索福瑞联合调查有限公司合作进行.参加调查的家庭从中央电视台入户收视率调查的基础数据库中随机抽取,在抽取过程中兼顾了不同城区、年龄结构、知识结构、收入水平等因素.研究表明,北京和上海居民冬夏两季的日均饮水量分别为2.2L·d-1、1.7L·d-1、2.0L·d-1和1.8L·d-1,这一结果和美国环保局的假设基本一致.同时本研究考察了性别、年龄、职业和季节对应用水消费习惯的影响.研究表明,日均饮水量随年龄的增加有增加的趋势,这一趋势在北京的夏季调查中趋势明显(p=0.01);男性的日均饮用水量大于女性,在上海冬季和夏季调查中均存在显著的差异(冬季:p=0.01;夏季:p=0.04);季节也同样影响被访者的日均饮水量,但是在4次调查中均未发现显著性差异.在北京冬季和夏季的调查中均发现了工作地点对饮用水消费习惯的显著影响(夏季p=0.01和冬季p=0.00).研究同样考察了居民饮用水消费类型,调查结果表明,煮沸后的自来水是中国居民最主要的日常饮品(上海夏季:58.3%;上海冬季67.9%;北京夏季:42.7%;北京冬季:60.0%).同时消费桶装纯净水的被访者也占有相当的比重(上海夏季:36.2%;上海冬季:24.7%;北京夏季:30.7%;北京冬季:60.0%).研究同时表明,在中国居民的日常生活中牛奶和豆奶已经成为重要的日常饮品.极少量的居民(北京夏季:10.7%;北京冬季5.7%;上海夏季1.2%;上海冬季0.6%)有直接饮用自来水的习惯.研究表明滞留水(在自来水水管中滞留6h以上的自来水)是对人体健康影响最大的水,而在我们的调查中,中国居民几乎不直接饮用滞留水.当前,饮用水健康风险评价在世界范围内蓬勃展开,但是这一技术在我国还处于起步阶段.本研究作为饮用水健康风险评价的前期工作,为其在中国的进一步发展提供了基础性的数据.