考虑补给变化的斯里兰卡东海岸海岸砂质含水层脆弱性分析

M. Vithanage, K. Villholth, P. Engesgaard, K. Jensen
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引用次数: 4

摘要

地下水是斯里兰卡东部典型的海水和泻湖之间的沙质含水层中家庭和农业用水的唯一来源。本研究旨在评估斯里兰卡东部沿海地区沙质含水层在快速城市化、农业和气候变化的影响下的安全产量和脆弱性。一个典型的含水层系统作为一项综合研究的一部分进行了建模,以了解这些沿海含水层的可持续性,该研究基于在斯里兰卡东部沿海沙带的一个试验田进行的观察。分别代表2000 m长、22 m深和2 m宽的模型域进行了二维模型模拟。据估计,在平均水文年,含水层的安全产量为0.37立方米/立方米,在干旱水文年,安全产量为0.18立方米/立方米。含水层系统中的水平衡与目前的补给处于平衡状态。然而,重要的是要将井分别放置在离海和泻湖至少750米的内陆,以避免咸水和微咸水的入侵。根据模拟结果,目前含水层系统没有出现枯竭或海水入侵的迹象。然而,由于气候变化,人口的增加、抽水的增加和补给的减少会增加含水层对盐和微咸水污染的脆弱性。
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Vulnerability analysis of the coastal sandy aquifers in the east coast of Sri Lanka with recharge change consideration.
Groundwater is the only source of water for domestic as well as agricultural purposes in the sand aquifer in be- tween sea and lagoon configuration typically found in the eastern Sri Lanka. This study was carried out to estimate the safe yield and assess the vulnerability of the sandy aquifer on the eastern coastal belt of Sri Lanka by rapid urbanization, agriculture and as well as climate change. A typical aquifer system was modeled as a part of a synthetic study to under- stand the sustainability of these coastal aquifers based on the observations made through a pilot field site in the eastern coastal sand stretch in Sri Lanka. Two dimensional model simulations were carried out representing 2000 m length, 22 m deep and 2 m wide model domain respectively. The safe yield of the aquifer is estimated to be 0.37 m 3 /m 2 for an average hydrological year and 0.18 m 3 /m 2 for a dry hydrological year. Water balance in the aquifer system is in equilibrium with the present recharge. However, it is important that the wells to be placed at least 750 m inland from the sea and lagoon re- spectively to avoid salt and brackish water intrusion. According to the modeling results, currently the aquifer system shows no signs of depletion or sea water intrusion. However, increase of population, increase of pumping, and reduction of recharge due to climate change can increase the aquifer vulnerability for contamination by salt and brackish water.
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