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

机译:集约化城市化对浅层地下水渗入深层地下水的影响:以曼谷和雅加达为例

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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 δ~(18)O 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.
机译:亚洲大城市在沿海和城市地区都存在严重的污染问题。此外,由于城市地区大量抽水,地下水潜力下降,地面沉降发生。为了防止城市化对地下水质量的不利影响,有必要确认城市化引起的地下水流量和污染物迁移的变化。我们研究了城市化对地下水中污染物迁移的影响。研究区域分别位于泰国曼谷和印度尼西亚阿卡塔附近,这两个城市的人口分别约为800万和1200万。每个大都会城市都位于三角洲上,并且与海湾相邻。我们分别在2004年和2006年在曼谷和雅加达测量了水位并在多个深度(100至200 m)的钻孔中收集了水样。由于先前过度抽取地下水,两个城市的当前水力潜力均低于海平面。结果,在沿海地区,地下水的流动方向现在向下。地下水中Cl〜-的浓度和δ〜(18)O的分布表明水力势的下降导致海水和浅层地下水侵入深层地下水。地下水中Mn和NO3-〜N的浓度表明这些污染物随着地下水流量的下降而从浅水层向深水层侵入,并暗示了深水层中污染物的积累。因此,重要的是要认识到沿海地区地下水潜力恢复后,随着深层地下水排入海中,未来污染物可能会迁移。

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