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首页> 外文期刊>Journal of hydrologic engineering >Coastal Aquifer Protection from Saltwater Intrusion Using Abstraction of Brackish Water and Recharge of Treated Wastewater: Case Study of the Gaza Aquifer
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Coastal Aquifer Protection from Saltwater Intrusion Using Abstraction of Brackish Water and Recharge of Treated Wastewater: Case Study of the Gaza Aquifer

机译:沿海含水层保护咸水侵入使用咸水抽象和治疗废水的充值:对加沙含水层的案例研究

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Coastal aquifers are threatened by saltwater intrusion (SWI), which leads to degradation of groundwater quality by raising salinity. SWI occurs due to human activities such as overabstraction or natural processes such as sea-level rise. SWI control can help in protecting coastal aquifers from deterioration. This paper presents a numerical study using the simulation of three-dimensional variable-density ground-water flow (SEAWAT) code to investigate and control SWI in Gaza aquifer, Palestine, considering overpumping due to population growth and sea-level rise. Application of different scenarios to investigate SWI in Gaza aquifer showed that the intrusion of the equi-concentration line at 35,000 ppm, which is the interface between freshwater and saline water that reached 3,177 m in 2010, were compared to the field investigation in 2010, and by 2055 it will increase to 3,186, 3,518, 5,619, and 6,523 m due to sea-level rise, reducing recharge, and overpumping (percentage changes of 0.29%, 10.74%, 76.87%, and 105.32%, respectively). The results reveal that the intrusion length will double in 2055, and overpumping is considered the main cause for such an increase. Three management scenarios were used to control SWI in Gaza aquifer, including the abstraction of brackish water, recharge of the aquifer using treated wastewater, and a combination of both. Brackish water abstraction led to retardation of SWI at 3.5 km; recharge using treated wastewater led to retardation of SWI at 3.6 km, but a combination of both scenarios led to a retardation of SWI at 3.7 km. The results revealed that recharging the aquifer using treated wastewater could retard intrusion of saline water more than abstraction of brackish water, while the combination of both scenarios gave a higher retardation rate for saline water toward the sea. Aquifer recharge using treated wastewater is considered an effective tool to control SWI and protect coastal aquifers from deterioration.
机译:沿海含水层受到咸水入侵(SWI)的威胁,这通过提高盐度导致地下水质量降低。由于人类的活动,如海平面上升等超级术或自然过程,发生了SWI。 SWI控制可以帮助保护沿海含水​​层免于恶化。本文介绍了使用三维可变密度地下水流量(SEAWAT)代码的模拟来调查和控制巴勒斯坦的SWI,考虑因人口增长和海平面升高而调查和控制SWI。不同情景在加沙含水层调查SWI的应用表明,平等浓度线的侵入量为35,000 ppm,这是2010年淡水和盐水达到3,177米的界面,与2010年的现场调查相比,和到2055年,由于海平面上升,减少充电和过度排斥(分别为0.29%,10.74%,76.87%和105.32%,将增加至3,186,3,518,5,619和6,523米,减少百分比(0.29%,10.74%,76.87%和105.32%)。结果表明,2055年的入侵长度将加倍,并被认为是这种增加的主要原因。三种管理情景用于控制加沙含水层的SWI,包括淡水的抽象,使用经过处理的废水的含水层的充电,以及两者的组合。咸水抽取导致3.5公里的SWI延迟;使用经过处理过的废水充电导致SWI延迟3.6公里,但这两种情况的组合导致了3.7公里的SWI延迟。结果表明,使用经过处理的废水再充电可能会使盐水的侵入咸水的抽象,而这两种情况的组合对海域的盐水产生了更高的延迟速率。使用经过处理过的废水充电的含水层被认为是控制SWI的有效工具,并保护沿海含水​​层免于恶化。

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