The Delineation of the Langat Basin Aquifer Based on Geological and Hydrogeological Characterization of Three Urban Areas of Malaysia

Syed Haque, N. Roslan
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Abstract

Aims: The aim of this study is to find out the hydrogeological settings and aquifer properties of Kajang, Bangi, and Semenyih urban areas to overcome the mismanagement of groundwater. Study Design: The scarcity of groundwater is one of the major concerns of urbanization in growing populated countries like Malaysia. Lack of knowledge of subsurface geology, hydrogeology and aquifer properties is the main reason for the groundwater mismanagement of the Langat Basin. Place and Duration of Study: The study targeted three growing urban areas Kajang, Bangi and Semenyih of Malaysia. Data were collected from the Mineral and Geosciences Department, Malaysia. Borehole logs, pumping tests and groundwater level monitoring data have been analysed and interpreted for this study. Methodology: Subsurface logs have been produced by the Strater Demo4 software; Water level analyses have been done by the groundwater level monitoring data, the contour map was plotted by using ArcGIS software with calculated groundwater head values and the Pumping test curve has been prepared by using Excel 2007. Results: Study areas are situated in Kenny Hill formation. Water is pumped from four types of formations they are; hard rock, weathered sedimentary, shallow sedimentary and a combination of alluvium and hard rock. Groundwater flow direction is controlled by the topography, from the hilly north-eastern side to the low elevated south-western side. The identified aquifer condition of the Kajang area is confined, boundary and consolidated fractured. Water is pumped from the confined fractured aquifer in Bangi town and from the leaky, consolidated fractured and unconfined aquifer in Semenyih town. Transmissivity and Specific capacity of all types of aquifers show a range of 2.35m2/day to 25.92m2/day and 2.64 m2/day to 41.28m2/day respectively. Conclusion: This study will help to establish robust policies for the sustainable development of groundwater.
基于马来西亚三个城区地质和水文地质特征的Langat盆地含水层圈定
目的:本研究的目的是了解加江、班吉和色门义市区的水文地质环境和含水层性质,以克服地下水管理不善的问题。研究设计:在像马来西亚这样人口不断增长的国家,地下水短缺是城市化的主要问题之一。缺乏对地下地质、水文地质和含水层性质的认识是导致Langat盆地地下水管理不善的主要原因。研究地点和时间:该研究针对马来西亚的加江、邦吉和Semenyih三个发展中的城市地区。数据收集自马来西亚矿产和地球科学部。本研究对钻孔测井、抽水试验和地下水位监测数据进行了分析和解释。方法:地下测井由Strater Demo4软件生成;利用地下水位监测资料进行了水位分析,利用ArcGIS软件绘制了等高线图,计算了地下水头值,并利用Excel 2007绘制了抽水试验曲线。结果:研究区位于肯尼山组。水从四种不同的地层中抽取;硬岩,风化沉积,浅沉积和冲积层和硬岩的组合。地下水的流向受地形控制,从丘陵的东北侧到低洼的西南侧。确定的加藏地区含水层条件为封闭、边界、固结断裂。从Bangi镇的承压裂缝含水层和Semenyih镇的渗漏、固结裂缝和无承压含水层抽水。各类型含水层的透光率和比容分别为2.35 ~ 25.92m2/d和2.64 ~ 41.28m2/d。结论:本研究将有助于制定地下水可持续发展的有力政策。
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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