Three-Dimensional Numerical Simulation of Saltwater Extraction Schemes to Mitigate Seawater Intrusion due to Groundwater Pumping in a Coastal Aquifer System

被引:30
作者
Park, Sang-Uk [1 ]
Kim, Jun-Mo [1 ]
Yum, Byoung-Woo [2 ]
Yeh, Gour-Tsyh [3 ,4 ]
机构
[1] Seoul Natl Univ, Sch Earth & Environm Sci, Seoul 151742, South Korea
[2] Korea Inst Geosci & Mineral Resources, Div Geol & Environm Res, Taejon 305350, South Korea
[3] Natl Cent Univ, Grad Inst Appl Geol, Jhongli 32001, Taoyuan, Taiwan
[4] Univ Cent Florida, Dept Civil & Environm Engn, Orlando, FL 32816 USA
关键词
Coastal aquifer system; Groundwater pumping; Seawater intrusion; Saltwater extraction; Hydrodynamic dispersion; Numerical simulation; WATER-INTRUSION;
D O I
10.1061/(ASCE)HE.1943-5584.0000412
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
A series of three-dimensional numerical simulations using a multidimensional hydrodynamic dispersion numerical model was performed to analyze various saltwater extraction schemes for mitigating seawater intrusion attributed to groundwater pumping in a coastal aquifer system. A steady-state numerical simulation was performed first to obtain initial (i.e., pregroundwater pumping) steady-state conditions before groundwater pumping, and then a transient-state numerical simulation was performed to obtain intermediate (i.e., postgroundwater pumping) steady-state conditions during groundwater pumping. In the subsequent series of transient-state numerical simulations as scenario and sensitivity analyses, four different saltwater extraction factors such as the amount of saltwater extraction, the number of extraction wells, the horizontal location of extraction wells, and the vertical interval of saltwater extraction were considered to determine an optimal saltwater extraction scheme for the coastal aquifer system threatened with seawater intrusion. The numerical simulation results show that seawater intrusion may be better mitigated when saltwater is extracted at 30% (up to 50%) of the groundwater pumping rate from a single extraction well, which is located horizontally midway between the pumping well and the coastline and is screened through the whole sand aquifer. DOI: 10.1061/(ASCE)HE.1943-5584.0000412. (C) 2012 American Society of Civil Engineers.
引用
收藏
页码:10 / 22
页数:13
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