The ability of subsurface dams to protect freshwater abstraction wells against seawater intrusion in heterogeneous aquifers

Antoifi Abdoulhalik , Ismail Abd-Elaty , Ashraf A. Ahmed
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Abstract

The main purpose of this study was to examine the ability of subsurface dams to protect freshwater abstraction against seawater intrusion in both homogeneous and layered aquifers. Laboratory experiments were conducted in a synthetic aquifer where a subsurface dam was simulated in a homogeneous scenario (case H), and in another scenario where a top low-permeability (low-K) layer was placed in the upper part of the aquifer (case LH). We then conducted numerical simulations using the SEAWAT model to validate the experimental results. We also examined other numerical cases where a low-K layer existed at the middle (case HLH) and the bottom of the aquifer (case HL). The existence of a low-K layer has generally delayed the upconing, and it took longer for the SWI to contaminate the abstraction well. The top low-K layer case needed 52 % more pumping than the homogeneous aquifer for the wedge to spill over the dam into the landward side. The clean-up time varied substantially from one case to another, with the case HL taking longer than the other cases for SWI removal. The cleanup time was reduced by 23 % in the presence of a top low-K layer compared to the homogeneous aquifer. The study demonstrates that a low-K layer on the top of the aquifer contributed positively to improving the ability of the subsurface dams to obstruct SWI, limit saltwater upconing and, therefore, allow more optimal freshwater abstraction. A feature of this study was that it examined the ability of dams to prevent seawater intrusion in the presence of freshwater pumping, which has not been investigated in previous studies, at least in laboratory experiments.
在非均质含水层中,地下水坝保护淡水抽取井免受海水入侵的能力
本研究的主要目的是检查地下水坝在均匀和分层含水层中保护淡水抽取免受海水入侵的能力。在一个合成含水层中进行了实验室实验,其中在均匀情景(案例H)中模拟了地下大坝,在另一个场景中,在含水层的上部放置了一个顶部低渗透(低钾)层(案例LH)。然后利用SEAWAT模型进行数值模拟,验证实验结果。我们还研究了在含水层中部(案例HLH)和底部(案例HL)存在低钾层的其他数值情况。低k层的存在通常会延迟上行,并且SWI需要更长的时间才能污染抽象井。顶部低钾层的情况需要比均匀含水层多抽52% %的水才能使楔块从大坝溢出到陆地侧。清除时间因病例而异,HL病例比其他病例清除SWI所需的时间更长。与均匀含水层相比,存在顶部低钾层时,清理时间缩短了23% %。研究表明,含水层顶部的低钾层有助于提高地下坝阻碍SWI、限制盐水上涌的能力,从而实现更优的淡水提取。这项研究的一个特点是,它检验了在抽取淡水的情况下大坝防止海水入侵的能力,这在以前的研究中没有被调查过,至少在实验室实验中没有。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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