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首页> 外文期刊>Water Research >Dynamics of dissolved organic carbon (DOC) through stormwater basins designed for groundwater recharge in urban area: Assessment of retention efficiency
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Dynamics of dissolved organic carbon (DOC) through stormwater basins designed for groundwater recharge in urban area: Assessment of retention efficiency

机译:通过用于市区补给的雨水盆地中的溶解有机碳(DOC)的动力学:保留效率的评估

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Managed aquifer recharge (MAR) has been developed in many countries to limit the risk of urban flooding and compensate for reduced groundwater recharge in urban areas. The environmental performances of MAR systems like infiltration basins depend on the efficiency of soil and vadose zone to retain stormwater-derived contaminants. However, these performances need to be finely evaluated for stormwater-derived dissolved organic matter (DOM) that can affect groundwater quality. Therefore, this study examined the performance of MAR systems to process DOM during its transfer from infiltration basins to an urban aquifer. DOM characteristics (fluorescent spectroscopic properties, biodegradable and refractory fractions of dissolved organic carbon -DOC-, consumption by micro-organisms during incubation in slow filtration sediment columns) were measured in stormwater during its transfer through three infiltration basins during a stormwater event. DOC concentrations sharply decreased from surface to the aquifer for the three MAR sites. This pattern was largely due to the retention of biodegradable DOC which was more than 75% for the three MAR sites, whereas the retention of refractory DOC was more variable and globally less important (from 18% to 61% depending on MAR site). Slow filtration column experiments also showed that DOC retention during stormwater infiltration through soil and vadose zone was mainly due to aerobic microbial consumption of the biodegradable fraction of DOC. In parallel, measurements of DOM characteristics from groundwaters influenced or not by MAR demonstrated that stormwater infiltration increased DOC quantity without affecting its quality (% of biodegradable DOC and relative aromatic carbon content estimated by SUVA(254)-). The present study demonstrated that processes occurring in soil and vadose zone of MAR sites were enough efficient to limit DOC fluxes to the aquifer. Nevertheless, the enrichments of DOC concentrations measured in groundwater below infiltration basins need to be considered in future studies to especially assess their impact on groundwater quality. (C) 2015 Elsevier Ltd. All rights reserved.
机译:许多国家已经开发了有管理的含水层补给(MAR),以限制城市洪灾的风险并补偿城市地区地下水补给的减少。 MAR系统(如浸润池)的环境性能取决于土壤和渗流带保留雨水衍生污染物的效率。但是,对于可能影响地下水质量的源自雨水的溶解有机物(DOM),需要对这些性能进行精细评估。因此,本研究研究了MAR系统在DOM从渗透盆地转移到城市含水层过程中处理DOM的性能。在暴雨过程中,通过雨水将DOM的特征通过三个渗透盆地转移时,测量了DOM的特征(荧光光谱特性,溶解的有机碳的可降解部分和难降解部分-DOC-,在缓慢过滤的沉淀柱中温育期间微生物的消耗)。三个MAR站点的DOC浓度从地表到含水层急剧下降。这种模式主要是由于三个MAR位点的可生物降解DOC保留率超过75%,而难治性DOC的保留率变化更大,并且在全球范围内不那么重要(取决于MAR位点,从18%到61%)。慢速过滤柱实验还表明,雨水通过土壤和渗流带渗透过程中的DOC保留主要是由于DOC可生物降解级分的好氧微生物消耗。同时,对MAR影响或不影响的地下水中DOM特性的测量表明,雨水的渗透增加了DOC的数量而不影响其质量(可降解DOC的百分比和SUVA(254)-估算的相对芳烃含量)。本研究表明,在MAR站点的土壤和渗流带中发生的过程足以将DOC通量限制到含水层。然而,在未来的研究中需要考虑在渗透盆地以下的地下水中测得的DOC浓度的增加,以特别评估它们对地下水质量的影响。 (C)2015 Elsevier Ltd.保留所有权利。

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