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Study on the influence of seawater density variation on sea water intrusion in confined coastal aquifers

机译:密闭沿海含水层中海水密度变化对海水入侵的影响研究

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The coupled influence of seawater density and groundwater level variation plays an import role in seawater intrusion in confined coastal aquifers. In this study, the effects of seawater density variations along with changing hydraulic gradients were investigated by conducting laboratory experiments and numerical simulations. Parameters of salinty and density in the experiments are based on the references related Bohai sea of China. The results indicate that the higher density of saltwater facilitates the seawater intrusion into the aquifers at the bottom and accelerates the circulation at the changing hydraulic gradient. Even slight variations in saltwater density can change the steady-state conditions in a confined aquifer, which should be considered when attempting to control the intrusion of seawater. Moreover, the influence of seawater density variations on transient salt-wedge dynamics was also examined in these experiments. Numerical modelling was simultaneously performed to mimic the behaviour of SW using the TOUGH2/EOS7 package. The simulated results were generally consistent with those obtained from the experiments. This study is conducive to further understand the mechanism of seawater intrusion, thereby leading to effective management of the problem in coastal areas.
机译:海水密度和地下水位变化的耦合影响在受限沿海含水层的海水入侵中起重要作用。在这项研究中,通过进行实验室实验和数值模拟研究了海水密度变化以及水力梯度变化的影响。实验中的盐度和密度参数基于与中国渤海有关的参考资料。结果表明,较高的盐水密度有利于海水侵入底部的含水层,并在不断变化的水力梯度下加速循环。盐水密度的微小变化都会改变密闭含水层的稳态条件,在尝试控制海水入侵时应考虑到这一点。此外,在这些实验中还检查了海水密度变化对瞬态盐楔动力学的影响。使用TOUGH2 / EOS7软件包同时进行了数值建模,以模拟SW的行为。模拟结果总体上与从实验中获得的结果一致。这项研究有利于进一步了解海水入侵的机制,从而导致对沿海地区问题的有效管理。

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