Effect of seasonal variations in sea level on residual saltwater removal upstream of subsurface dam in coastal layered heterogeneity aquifers.

IF 8 2区 环境科学与生态学 Q1 ENVIRONMENTAL SCIENCES Journal of Environmental Management Pub Date : 2024-08-01 Epub Date: 2024-07-03 DOI:10.1016/j.jenvman.2024.121589
Jun Wang, Jun Kong, Chao Gao, Li Jing, Weilun Chen
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Abstract

Subsurface dams have been recognized as one of the most effective measures for preventing saltwater intrusion. However, it may result in large amounts of residual saltwater being trapped upstream of the dam and take years to decades to remove, which may limit the utilization of fresh groundwater in coastal areas. In this study, field-scale numerical simulations were used to investigate the mechanisms of residual saltwater removal from a typical stratified aquifer, where an intermediate low-permeability layer (LPL) exists between two high-permeability layers, under the effect of seasonal sea level fluctuations. The study quantifies and compares the time of residual saltwater removal (Tre) for constant sea level (CSL) and seasonally varying sea level (FSL) scenarios. The modelling results indicate that, in most cases, seasonal fluctuations in sea level facilitate the dilution of residual saltwater and thus accelerate residual saltwater removal compared to a static sea level scenario. However, accounting for seasonal sea level variations may increase the required critical dam height (the minimum dam height required to achieve complete residual saltwater removal). Sensitivity analyses show that Tre decreases with increasing height of subsurface dam (Hd) under CSL or weaker sea level fluctuation scenarios; however, when the magnitude of sea level fluctuation is large, Tre changes non-monotonically with Hd. Tre decreases with increasing distance between subsurface dam and ocean for both CSL and FSL scenarios. We also found that stratification model had a significant effect on Tre. The increase in LPL thickness for both CSL and FSL scenarios leads to a decrease in Tre and critical dam height. Tre generally shows a non-monotonically decreasing trend as LPL elevation increases. These quantitative analyses provide valuable insights into the design of subsurface dams in complex situations.

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海平面季节性变化对沿海分层异质含水层地下水坝上游残余盐水排除的影响。
地下水坝被认为是防止海水入侵的最有效措施之一。然而,这可能会导致大量残余盐水滞留在大坝上游,需要数年至数十年的时间才能清除,这可能会限制沿海地区对地下淡水的利用。在这项研究中,采用了野外尺度的数值模拟来研究在季节性海平面波动的影响下,一个典型的分层含水层(在两个高渗透层之间存在一个中间低渗透层(LPL))的残余盐水排除机制。研究量化并比较了恒定海平面(CSL)和季节性海平面变化(FSL)情况下的残余盐水去除(Tre)时间。建模结果表明,在大多数情况下,海平面的季节性波动会促进残余海水的稀释,从而加快残余海水的清除速度。不过,考虑季节性海平面变化可能会增加所需的临界坝高(实现完全去除残余盐水所需的最低坝高)。敏感性分析表明,在 CSL 或海平面波动较弱的情况下,Tre 随地下坝高度(Hd)的增加而减小;但当海平面波动幅度较大时,Tre 随 Hd 的变化呈非单调变化。在 CSL 和 FSL 情景下,Tre 随地下水坝与海洋距离的增加而减小。我们还发现分层模型对 Tre 有显著影响。在 CSL 和 FSL 方案中,LPL 厚度的增加都会导致 Tre 和临界坝高的降低。随着 LPL 高度的增加,Tre 一般呈非单调递减趋势。这些定量分析为复杂情况下的地下大坝设计提供了宝贵的见解。
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来源期刊
Journal of Environmental Management
Journal of Environmental Management 环境科学-环境科学
CiteScore
13.70
自引率
5.70%
发文量
2477
审稿时长
84 days
期刊介绍: The Journal of Environmental Management is a journal for the publication of peer reviewed, original research for all aspects of management and the managed use of the environment, both natural and man-made.Critical review articles are also welcome; submission of these is strongly encouraged.
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