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首页> 外文期刊>Journal of Hydrology >Interaction between shallow groundwater, saline surface water and contaminant discharge at a seasonally and tidally forced estuarine boundary
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Interaction between shallow groundwater, saline surface water and contaminant discharge at a seasonally and tidally forced estuarine boundary

机译:季节性和潮汐作用河口边界处浅层地下水,盐分地表水和污染物排放之间的相互作用

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This paper presents findings from a 2-year field investigation of a dissolved hydrocarbon groundwater plume flowing towards a tidally and seasonally forced estuarine river system in Perth, Western Australia. Samples collected from transects of multiport wells along the riverbank and into the river, enabled mapping of the fine scale (0.5 m) vertical definition of the hydrocarbon plume and its longitudinal extent. Spear probing beneath the river sediments and water table, and transient monitoring of multiport wells (electrical conductivity) was also carried out to define the zone of mixing between river water and groundwater (the hyporheic zone) and its variability. The results showed that groundwater seepage into the estuarine surface sediments occurred in a zone less than 10 m from the high tide mark, and that this distance and the hyporheic transition zone were influenced by tidal fluctuations and infiltration of river water into the sediments. The dissolved BTEXN (benzene, toluene, ethylbenzene, the xylene isomers and naphthalene) distributions indicated the behaviour of the hydrocarbon plume at the groundwater/surface water transition zone to be strongly influenced by edge-focussed discharge. Monitoring programs and risk assessment studies at similar contaminated sites should therefore focus efforts within the intertidal zone where contaminants are likely to impact the surface water and shallow sediment environments. Crown Copyright (C) 2004 Published by Elsevier B.V. All rights reserved.
机译:本文介绍了一项为期2年的野外调查结果,该研究对西澳大利亚珀斯的潮汐和季节性强迫河口河水系统中溶解的碳氢化合物地下水羽流进行了研究。从沿河岸并进入河中的多口井样带收集的样本能够绘制出碳氢化合物羽流的精细尺度(0.5 m)垂直定义及其纵向范围。对河底沉积物和地下水位下方的矛进行探测,并对多口井进行瞬态监测(电导率),以定义河水与地下水之间的混合区(低渗区)及其变化性。结果表明,地下水从河口表层沉积物渗入的区域发生在距高潮标记不到10 m的区域,并且该距离和流变过渡区受到潮汐波动和河水向沉积物中的渗透的影响。溶解的BTEXN(苯,甲苯,乙苯,二甲苯异构体和萘)的分布表明,烃类羽流在地下水/地表水过渡区的行为受到边缘集中排放的强烈影响。因此,在类似污染场地的监测计划和风险评估研究应集中在潮间带内,污染物可能会影响地表水和浅层沉积物环境。官方版权(C)2004,Elsevier B.V.保留所有权利。

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