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首页> 外文期刊>Journal of Hydrology >Three dimensional simulation of seawater intrusion in coastal aquifers: A case study in the Goksu Deltaic Plain
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Three dimensional simulation of seawater intrusion in coastal aquifers: A case study in the Goksu Deltaic Plain

机译:沿海含水层海水入侵的三维模拟:以五谷三角洲平原为例

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摘要

Unplanned exploitation of groundwater from coastal aquifers may cause salt water intrusion in coastal aquifers. Coastal areas are generally overpopulated with fertile agricultural lands and diversified irrigated farming activities. The objective of this study was to develop a model to control/prevent seawater intrusion into the coastal aquifer with a case study of the Silifke-Goksu Deltaic Plain. A computer program for the simulation of three-dimensional variable density groundwater flow, SEAWAT, is used to model the seawater intrusion mechanism of the Goksu Deltaic Plain along the Mediterranean coast of Turkey. The calibration analysis of the developed seawater intrusion model is performed using field measured data in the water-year of 2008 including static groundwater head, electrical conductivity, total dissolved solid (TDS), and chloride concentration values collected from 23 observation wells and the existing data which were compiled and reviewed. The main objectives for applying the seawater intrusion model to the Goksu Deltaic Plain were (1) to determine the hydraulic and hydrogeologic parameters of the aquifer, (2) to estimate the spatial variation of the salt concentration in the aquifer and (3) to investigate the impact of the increase and decrease in groundwater extractions. The simulation results show that the Goksu Deltaic Plain aquifer is especially sensitive to the increase in groundwater extraction.
机译:计划外开采沿海含水层的地下水可能会导致盐水侵入沿海含水层。沿海地区普遍人口稠密,农田肥沃,灌溉活动多样化。这项研究的目的是建立一个模型,以Silifke-Goksu三角洲平原为例,以控制/防止海水侵入沿海含水层。用于模拟三维可变密度地下水流SEAWAT的计算机程序用于模拟土耳其地中海沿岸Goksu三角洲平原的海水入侵机制。所开发的海水入侵模型的标定分析是使用2008年水域的现场测量数据进行的,包括从23个观测井收集的静态地下水压头,电导率,总溶解固体(TDS)和氯化物浓度值以及现有数据进行了汇编和审查。将海水入侵模型应用于Goksu三角洲平原的主要目标是(1)确定含水层的水力和水文地质参数,(2)估算含水层中盐浓度的空间变化,以及(3)研究地下水开采量增加和减少的影响。模拟结果表明,Goksu三角洲平原含水层对地下水开采量的增加特别敏感。

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