Numerical simulation of the effect of heavy groundwater abstraction on groundwater-surface water interaction in Langat Basin, Selangor, Malaysia

被引:14
作者
May, Raksmey [1 ]
Mazlan, Nurhuda Shakhila Binti [1 ]
机构
[1] Univ Teknol MARA, Fac Civil Engn, Shah Alam 40450, Selangor, Malaysia
关键词
Groundwater-surface water interaction; Groundwater modeling; Langat River; Hyporheic flow; River conductance; FLOW;
D O I
10.1007/s12665-013-2527-4
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The paper aims at evaluating the interaction between ground and surface water along the Langat River in Malaysia through the development of a numerical simulation. Malaysia has been experiencing a rapid economic growth since the last few decades, driven by many factors such as agriculture, industry, and the like. The demand for water in these sectors has increased so tremendously that surface water has been utilized in conjunction to groundwater. Approximately 18,184 m(3) of water per day is obtained from the aquifer to supply to the steel factory. There are also workshops, petroleum stations, and houses in the area thus causing the water quantity and quality to degrade. In terms of quantity, the pumping activity has altered the interaction between the groundwater and surface water. Therefore, a numerical model was proposed and two aquifer layers were simulated, with the first layer being approximately > 20 m in depth and the second layer > 100 m. The recharge estimated from the tank model was input into the groundwater modeling. The effects of the surface water to the aquifer were included in the simulation by defining the river conductance, river bed, and river level. The calibrated model (error about 0.9 m) was achieved and applied to predict the flow pattern in its natural state without the pumping and with the pumping states. As a result, in the first scenario, the stream was in an effluent condition influenced by the groundwater from the northeast to the west. A hyporheic flow occurred and was observed from the contour map. The flow system was changed in the second scenario when the pumping activity was included in the simulation. The groundwater lost its original function but received leakage from the stream near the pumping sites. The findings of this study will help the local authorities and other researchers to understand the aquifer system in the area and assist in the preparation of a sustainable groundwater management.
引用
收藏
页码:1239 / 1248
页数:10
相关论文
共 11 条
[1]   Analysis and prediction of flow from local source in a river basin using a Neuro-fuzzy modeling tool [J].
Aqil, Muhammad ;
Kita, Ichiro ;
Yano, Akira ;
Nishlyama, Soichi .
JOURNAL OF ENVIRONMENTAL MANAGEMENT, 2007, 85 (01) :215-223
[2]  
Bencala KE, 2005, HYPORHEIC EXCHANGE F
[3]  
Damien L, 2010, HYPORHEIC HDB
[4]  
Department of Irrigation and Drainage (DID), 2012, ONL HYDR DAT
[5]  
DOE, 2006, ENV QUAL REP
[6]   Recharge sources and hydrogeological effects of irrigation and an influent river identified by stable isotopes in the Motril-Salobrena aquifer (Southern Spain) [J].
Duque, C. ;
Lopez-Chicano, M. ;
Calvache, M. L. ;
Martin-Rosales, W. ;
Gomez-Fontalva, J. M. .
HYDROLOGICAL PROCESSES, 2011, 25 (14) :2261-2274
[7]  
Fetter CW, 2001, APPL HYDROGEOLOGY, P128
[8]  
JICA and MGD, 2002, STUD SUST GROUNDW RE, V1
[9]  
Smith J.W.N, 2005, SC030155SR1 ENV AG
[10]   Surface and subsurface water balance estimation by the groundwater recharge model and a 3-D two-phase flow model [J].
Tsutsumi, A ;
Jinno, K .
HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES, 2004, 49 (02) :205-226