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Experimental Study of Tidal Effects on Coastal Groundwater and Pollutant Migration

机译:潮汐对沿海地下水和污染物迁移影响的试验研究。

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摘要

The problem of current urban groundwater pollution is very serious, which has influenced social development and people's daily life. Around the land-sea interface, tide obviously changes nearshore the groundwater flow regime and makes the pollutant migration process become more complex. In the present study, the effect of tide-induced groundwater table fluctuations and on the pollutants migration in beach aquifers is investigated by constructing a two-dimensional sand trough physical experimental model. The model considered brackish-water density differences and the tide by controlling experimental medium properties and boundary conditions. The results showed that the groundwater table fluctuation cycle is the same as the tidal cycle and the fluctuation lag time increases linearly with the increase of the offshore distance. Tidal fluctuation flattens brackish-freshwater interface, widens the dispersion zone, and generates the upper saline and the freshwater belt. Time lag corresponding relationships between saline water and tidal fluctuation was observed. With the pollutant approaching the saline water area, the profile of the pollutant migration is gradually developed into a spindle shape until the strip shape, and the pollutant enters the saline water body along the curved edge of the upper part of the saline water. The transverse dispersion of pollutants is larger than the longitudinal dispersion in a tidal cycle and its outline presents a strip shape development. No mixing or exchange between the pollutants and the saline water body happened during the whole process. This study can provide scientific references for nearshore groundwater pollution prevention and control in the future.
机译:当前城市地下水污染问题十分严重,影响了社会发展和人们的日常生活。在陆地-海洋界面附近,潮汐在地下水流态附近发生明显变化,并使污染物迁移过程变得更加复杂。在本研究中,通过建立二维砂槽物理实验模型,研究了潮汐引起的地下水位波动以及对海滩含水层中污染物迁移的影响。该模型通过控制实验介质的性质和边界条件来考虑微咸水密度差和潮汐。结果表明,地下水位波动周期与潮汐周期相同,波动滞后时间随离岸距离的增加而线性增加。潮汐波动使微咸水-淡水界面变平,扩大了分散区,并产生了上层盐水和淡水带。观察到盐水和潮汐波动之间存在时滞对应关系。随着污染物接近盐水区域,污染物迁移的轮廓逐渐发展成纺锤形直至条状,污染物沿着盐水上部的弯曲边缘进入盐水体。在一个潮汐循环中,污染物的横向扩散大于纵向扩散,其轮廓呈现出条形发展。在整个过程中,污染物与盐水水体之间没有混合或交换。该研究可为今后近岸地下水污染的防治提供科学参考。

著录项

  • 来源
    《Water, Air, and Soil Pollution》 |2017年第4期|163.1-163.15|共15页
  • 作者单位

    Tongji Univ, Coll Civil Engn, Shanghai, Peoples R China|Tongji Univ, Minist Educ, Key Lab Yangtze River Water Environm, 1239 Siping Rd, Shanghai 200092, Peoples R China;

    Power China HuaDong Engn Corp Ltd, Hangzhou, Zhejiang, Peoples R China;

    Tongji Univ, Coll Civil Engn, Shanghai, Peoples R China;

    Tongji Univ, Coll Civil Engn, Shanghai, Peoples R China;

    Tongji Univ, Coll Civil Engn, Shanghai, Peoples R China;

    Tongji Univ, Coll Civil Engn, Shanghai, Peoples R China;

    Tongji Univ, Coll Civil Engn, Shanghai, Peoples R China;

    Lomonosov Moscow State Univ, Fac Geog, GSP-1,1 Leninskiye Gory, Moscow 119991, Russia;

    Lomonosov Moscow State Univ, Fac Geog, GSP-1,1 Leninskiye Gory, Moscow 119991, Russia;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Tidal effect; Seawater intrusion; Coastal groundwater; Pollutant migration; Model simulation;

    机译:潮汐效应海水入侵沿海地下水污染物迁移模型模拟;
  • 入库时间 2022-08-17 13:37:49

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