Effects of intensive urbanization on the intrusion of shallow groundwater into deep groundwater: Examples from Bangkok and Jakarta

被引:49
作者
Onodera, Shin-ichi [1 ]
Saito, Mitsuyo [2 ]
Sawano, Misa
Hosono, Takahiro [3 ]
Taniguchi, Makoto
Shimada, Jun [4 ]
Umezawa, Yu [5 ]
Lubis, Rachmat Fajar
Buapeng, Somkid
Delinom, Robert
机构
[1] Hiroshima Univ, Grad Sch Integrated Arts & Sci, Hiroshima 7398521, Japan
[2] Ehime Univ, Ctr Marine Environm Studies, Matsuyama, Ehime 790, Japan
[3] Akita Univ, Dept Earth Sci & Technol, Akita 010, Japan
[4] Kumamoto Univ, Grad Sch Sci, Kumamoto 860, Japan
[5] Nagasaki Univ, Fac Fisheries, Nagasaki, Japan
关键词
Asia; Groundwater; Pollution; Urbanization;
D O I
10.1016/j.scitotenv.2008.08.003
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Asian megacities have severe pollution problems in both coastal and urban areas. In addition, the groundwater potential has decreased and land subsidence has occurred because of intensive groundwater pumping in urban areas. To prevent the adverse effects of urbanization on groundwater quality, it is necessary to confirm the changes in groundwater flow and contaminant transport caused by urbanization. We examined the effects of urbanization on contaminant transport in groundwater. The research areas were located around Bangkok, Thailand, and akarta, Indonesia, cities with populations of approximately 8 and 12 million, respectively. Each metropolitan city is located on a river delta and is adjacent to a bay. We measured the water level and collected water samples at boreholes at multiple depths (100 to 200 m) in 2004 and 2006 in Bangkok and Jakarta, respectively. The current hydraulic potential is below sea level in both cities because of prior excess abstraction of groundwater. As a result, the direction of groundwater flow is now downward in the coastal area. The Cl- concentration and delta O-18 distributions in groundwater suggest that the decline in hydraulic potential has caused the intrusion of seawater and shallow groundwater into deep groundwater. Concentrations of Mn and NO3(-)-N in groundwater suggest the intrusion of these contaminants from shallow to deep aquifers with downward groundwater flow and implies an accumulation of contaminants in deep aquifers. Therefore, it is important to recognize the possibility of future contaminant transport with the discharge of deep groundwater into the sea after the recovery of groundwater potential in the coastal areas. (C) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:401 / 410
页数:10
相关论文
共 35 条
[1]   Land subsidence characteristics of Jakarta between 1997 and 2005, as estimated using GPS surveys [J].
Abidin, Hasanuddin Z. ;
Andreas, H. ;
Djaja, Rochman ;
Darmawan, Dudy ;
Gamal, M. .
GPS SOLUTIONS, 2008, 12 (01) :23-32
[2]  
*AIT, 1981, INV LAND SUBS CAUS D, P91
[3]  
[Anonymous], GLOBAL ENV MEGACITIE
[4]  
[Anonymous], 1978, GROUNDWATER
[5]  
[Anonymous], WORLD DEV IND CD ROM
[6]  
[Anonymous], 2004, P 3 FIG REG C JAK IN
[7]  
[Anonymous], WHIT PAP QUAL ENV JA
[8]  
[Anonymous], WHIT PAP QUAL ENV JA
[9]  
Appelo CAJ, 2005, GEOCHEMISTRY GROUNDW, P415, DOI [10.1007/s00027-013-0327-2, DOI 10.1007/S00027-013-0327-2]
[10]  
BOHLKE JK, 1995, WATER RESOUR RES, V31, P2319, DOI 10.1029/95WR01584