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印度深层城市地下水脆弱性通过新兴有机污染物和停留时间示踪剂揭示。

Deep urban groundwater vulnerability in India revealed through the use of emerging organic contaminants and residence time tracers.

机构信息

British Geological Survey, Maclean Building, Wallingford, OX10 8BB, UK.

Department of Geology and Geophysics, IIT-Kharagpur, Kharagpur, 721302, West Bengal, India.

出版信息

Environ Pollut. 2018 Sep;240:938-949. doi: 10.1016/j.envpol.2018.04.053. Epub 2018 Jun 18.

Abstract

Demand for groundwater in urban centres across Asia continues to rise with ever deeper wells being drilled to avoid shallow contamination. The vulnerability of deep alluvial aquifers to contaminant migration is assessed in the ancient city of Varanasi, India, using a novel combination of emerging organic contaminants (EOCs) and groundwater residence time tracers (CFC and SF). Both shallow and intermediate depth private sources (<100 m) and deep (>100 m) municipal groundwater supplies were found to be contaminated with a range of EOCs including pharmaceuticals (e.g. sulfamethoxazole, 77% detection frequency, range <0.0001-0.034 μg L), perfluoroalkyl substances (e.g. PFOS, range <0.0001-0.033 μg L) as well as a number of pesticides (e.g. phenoxyacetic acid, range <0.02-0.21 μg L). The profile of EOCs found in groundwater mirror those found in surface waters, albeit at lower concentrations, and reflect common waste water sources with attenuation in the subsurface. Mean groundwater residence times were found to be comparable between some deep groundwater and shallow groundwater sources with residence times ranging from >70 to 30 years. Local variations in aquifer geology influence the extent of modern recharge at depth. Both tracers provide compelling evidence of significant inputs of younger groundwater to depth >100 m within the aquifer system.

摘要

亚洲城市中心对地下水的需求持续上升,为了避免浅层污染,人们不断钻探更深的井。本研究采用新兴有机污染物(EOCs)和地下水滞留时间示踪剂(CFC 和 SF)的新组合,评估了印度古城瓦拉纳西深层冲积含水层对污染物迁移的脆弱性。浅层和中层私人水源(<100 m)和深层(>100 m)市政地下水均受到各种 EOCs 的污染,包括药物(如磺胺甲恶唑,检出频率为 77%,范围为<0.0001-0.034μg/L)、全氟烷基物质(如 PFOS,范围为<0.0001-0.033μg/L)以及一些农药(如苯氧乙酸,范围为<0.02-0.21μg/L)。地下水中发现的 EOCs 特征与地表水中发现的特征相似,尽管浓度较低,但反映了常见的废水来源,并在地下发生了衰减。一些深层地下水和浅层地下水的平均地下水滞留时间被发现具有可比性,范围从>70 年到 30 年不等。含水层地质的局部变化影响着深部现代补给的程度。两种示踪剂都提供了令人信服的证据,表明在含水层系统中,深度>100 m 的地下水有大量的年轻地下水输入。

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