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首页> 外文期刊>Journal of earth system science >Numerical modelling of seawater intrusion in Shenzhen (China) using a 3D densitydependent model including tidal effects
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Numerical modelling of seawater intrusion in Shenzhen (China) using a 3D densitydependent model including tidal effects

机译:使用包含潮汐效应的3D密度相关模型对深圳(中国)的海水入侵进行数值模拟

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摘要

During the 1990s, groundwater overexploitation has resulted in seawater intrusion in the coastal aquifer of the Shenzhen city, China. Although water supply facilities have been improved and alleviated seawater intrusion in recent years, groundwater overexploitation is still of great concern in some local areas. In this work we present a three-dimensional density-dependent numerical model developed with the FEFLOW code, which is aimed at simulating the extent of seawater intrusion while including tidal effects and different groundwater pumping scenarios. Model calibration, using waterheads and reported chloride concentration, has been performed based on the data from 14 boreholes, which were monitored from May 2008 to December 2009. A fairly good fitness between the observed and computed values was obtained by a manual trial-and-error method. Model prediction has been carried out forward 3 years with the calibrated model taking into account high, medium and low tide levels and different groundwater exploitation schemes. The model results show that tide-induced seawater intrusion significantly affects the groundwater levels and concentrations near the estuarine of the Dasha river, which implies that an important hydraulic connection exists between this river and groundwater, even considering that some anti-seepage measures were taken in the river bed. Two pumping scenarios were considered in the calibrated model in order to predict the future changes in the water levels and chloride concentration. The numerical results reveal a decreased tendency of seawater intrusion if groundwater exploitation does not reach an upper bound of about 1.32 ?— 104 m3/d. The model results provide also insights for controlling seawater intrusion in such coastal aquifer systems.
机译:在1990年代,地下水的过度开采导致了中国深圳沿海含水层的海水入侵。尽管近年来供水设施得到了改善并减轻了海水的入侵,但是在某些地方,地下水的过度开发仍然引起人们的极大关注。在这项工作中,我们提出了一个用FEFLOW代码开发的三维密度相关数值模型,该模型旨在模拟海水入侵的程度,同时包括潮汐影响和不同的地下水抽运情况。根据2008年5月至2009年12月监测的14个钻孔的数据,使用水位和报告的氯化物浓度进行了模型校准。通过手动试验获得了观测值和计算值之间的良好适应性。错误方法。考虑到高,中,低潮水位以及不同的地下水开采方案,已经使用校准模型对模型进行了三年的预测。模型结果表明,潮汐引起的海水入侵显着影响了大沙河河口附近的地下水位和浓度,这意味着即使考虑到采取了一些防渗措施,该河流与地下水之间也存在重要的水力联系。河床。在校准模型中考虑了两种抽水方案,以预测水位和氯化物浓度的未来变化。数值结果表明,如果地下水开采量未达到约1.32?-104 m3 / d的上限,则海水入侵的趋势会降低。模型结果还为控制此类沿海含水层系统中的海水入侵提供了见识。

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