Hard Rock Aquifers of Trivandrum, Kerala, India: A Critical Analysis of Its Status and Prospects

P. Raveendran, E. Shaji
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Abstract

: Groundwater in the hard rock aquifers of Trivandrum district has been studied to characterize the groundwater potential and prospects. The study area is occupied by four watersheds (Ayirur, Vamanapuram, Karamana and Neyyar) and groundwater is one of the main sources of water for drinking and agricultural purpose. The groundwater scenario has been assessed by using the water table contour maps and groundwater level fluctuation maps based on the data obtained from 93 observation wells. The average water level in the region is 9 to 13 and 8 to 10 mbgl during pre and post monsoon seasons respectively. The deepest water level (20.21 mbgl to 26.67 mbgl) is recorded from places such as Chovvarapotta, Pazhayaucchakkada and Ozhukupara and shallowest water level (0.85 mbgl to 1.61 mbgl) is in places like Irumba, Punnamkarikkakam, Kathipara and Erattachira. Most of the deep dug wells go dry during summer months, though these wells show good water level fluctuation during rainy season. A detailed investigation has revealed that substantial quantity of groundwater is being lost as base flow. This base flow of groundwater makes the rivers and river lets, perennial in the area. The long term trend analysis shows that (ten years data), majority of the wells are showing declining trend (1.99 m/year) and this decline is attributed to the change in land use pattern in the area and less recharge from the rainfall. The rainfall analysis shows that there is not much variation in the rainfall pattern over the last few years. On the basis of mathematical projection the water level trends for the next ten years has been predicted. The analysis shows that the groundwater potential in the hard rock aquifer is depleting hence an immediate recharge measures have to be implemented in this region to arrest the decline trend and the base flow.
印度喀拉拉邦特里凡得琅的硬岩含水层:现状与前景的批判性分析
对Trivandrum地区硬岩含水层的地下水进行了研究,描述了地下水的潜力和前景。研究区有四个流域(Ayirur、Vamanapuram、Karamana和Neyyar),地下水是饮用水和农业用水的主要来源之一。利用93口观测井资料绘制的地下水位等高线图和地下水位涨落图,对地下水情景进行了评价。季风前和季风后的平均水位分别为9 ~ 13mbgl和8 ~ 10mbgl。最深的水位(20.21至26.67 mbgl)记录在Chovvarapotta, Pazhayaucchakkada和Ozhukupara等地,最浅的水位(0.85至1.61 mbgl)记录在Irumba, Punnamkarikkakam, Kathipara和Erattachira等地。大多数深挖井在夏季干涸,但这些井在雨季表现出良好的水位波动。一项详细的调查显示,大量的地下水作为基流正在流失。地下水的基础流使得河流和河川常年存在于该地区。长期趋势分析表明(10年数据),大部分井呈下降趋势(1.99 m/年),这种下降是由于该地区土地利用方式的变化和降雨补给的减少。降雨分析表明,过去几年的降雨模式没有太大变化。在数学推算的基础上,对未来十年的水位趋势进行了预测。分析表明,该地区硬岩含水层的地下水潜力正在枯竭,必须采取立即回灌措施,以遏制下降趋势和基底流。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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