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Evaluating the impact of percolated reclaimed water from river-channel reservoir on groundwater using tracers in Beijing, Northern China

机译:中国北方北京北京地下水中河流储层从河流储层中渗透渗流的影响

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As an increasingly important aspect of water management, historical dry river-channels, ponds or lakes are operated for the storage of reclaimed water as a landscape with the need for reuse of water. However, the percolated reclaimed water may have an adverse effect on groundwater quality. The aims of this work are to evaluate the potential for using various groundwater constituents or characteristics as tracers of percolated reclaimed water, to clarify the groundwater hydrochemical process with the effect of the reclaimed water recharge, and to estimate the degree to which the infiltrated reclaimed water has mixed with the native groundwater. Results obtained by comparing analysis between the dry season and wet season are presented based on multivariate statistics analysis, correlation of hydrochemical elements, and stable isotopes. The groundwater with the impact of reclaimed water was clustered together with higher Cl, K and NH4-N concentrations, lower Ca concentrations and more enriched heavy isotopes using unprecedentedly 3D-biplot; The water types of the groundwater change from Ca-Mg-HCO3-Cl, via Ca-Na-Mg-HCO3-Cl to Na-Ca-Mg-Cl-HCO3 with increasing reclaimed water percolated into the groundwater; the most useful tracers for evaluation of the fate and mixing of reclaimed water are chloride ion and oxygen-18 and chloride ion is more accurate than oxygen-18 to quantify the recharge source of the groundwater from the reclaimed water; using a two-end-member mixing model to calculate the reclaimed water discharged into the groundwater, the proportion of reclaimed water in groundwater is up to 94% near the unlined riverbed and up to 43% far from it. These results demonstrate the potential of the combined application of multivariate statistics analysis, traditional hydrochemical analysis and isotopes to assess the percolated reclaimed water in the groundwater, especially using 3D-biplot to determine the spatial water quality changes defined by the different factors.
机译:作为水管理的越来越重要的方面,历史干燥的河流通道,池塘或湖泊被运作用于存储再生水作为一种景观,需要再利用水。然而,渗透的再生水可能对地下水质量产生不利影响。这项工作的目的是评估利用各种地下水成分或特征作为渗透再生水的示踪剂的可能性,以阐明地下水的水化工程具有再生水充电的影响,并估计渗透的再生水的程度与本土地下水混合。基于多元统计分析,水化学元素的相关性和稳定同位素,提出了通过比较干燥季节和湿季分析获得的结果。具有再生水的影响的地下水与更高的Cl,K和NH 4-N浓度,低于Ca浓度和更富集的重同位素使用前所未有的3D-Plot;通过Ca-Na-Mg-HCO3-Cl至Na-Ca-Mg-Cl-HCO3从Ca-Mg-HCO3-CL转化的地下水的水类型随着渗透到地下水中的再生水;用于评价的命运和再生水混合的最有用的示踪剂是氯离子和氧-18和氯离子比氧气-18更精确,以量化地下水的再生水源;使用双端构件混合模型来计算排放到地下水的再生水,地下水中再生水的比例靠近无衬里河床附近的94%,远远超过43%。这些结果表明了多元统计分析,传统水化学分析和同位素的组合应用的潜力,以评估地下水中的渗透再生水,特别是使用3D-PLOT来确定不同因素定义的空间水质变化。

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