Groundwater Exploration using 2D Electrical Resistivity Imaging (ERI) at Kulim, Kedah, Malaysia

A. Suryadi, M. Habibi, Batara, D. B. E. Putra, H. Kausarian
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引用次数: 2

Abstract

Water demand in the study area has been increasing by time but surface water is not sufficient to fulfil the demands. 2D Electrical Resistivity Imaging (ERI) survey was conducted in order to looking for groundwater potential as freshwater alternative resources at Kulim, Kedah, Malaysia. The data acquisition was carried out using 5 meters multi-electrodes spacing with pole-dipole configuration array. The geophysical survey involved both resistivity and chargeability at the same time. The result of 2D Electrical Resistivity Imaging indicated that the groundwater potential area has low resistivity value with range 10 – 100 Ωm. Groundwater potential zone divided into 2 characteristics which is shallow groundwater zone (>75m in depth) and deep groundwater zone (>100m in depth). The groundwater potential zone covered by high to very high resistivity value. Those high resistivity value 200 – 1000 Ωm interpreted as dry top soil at near surface while at deep zone is interpreted as fresh bedrock. Chargeability value of groundwater potential area ranging from 0 up to 8 msec. All interpretation later confirmed by drilling data.
利用二维电阻率成像(ERI)在马来西亚吉打州的Kulim进行地下水勘探
随着时间的推移,研究区需水量不断增加,但地表水不足以满足研究区需水量的需求。在马来西亚吉打州的Kulim进行了二维电阻率成像(ERI)调查,以寻找地下水作为淡水替代资源的潜力。数据采集采用5米多电极间距,采用极-偶极配置阵列。地球物理调查同时涉及电阻率和电荷率。二维电阻率成像结果表明,地下水潜势区具有低电阻率值,范围为10 ~ 100 Ωm。地下水潜力带分为浅埋区(>75m)和深埋区(>100m) 2个特征。地下水电位区为高至极高电阻率值所覆盖。高电阻率值200 ~ 1000 Ωm在近地表解释为干表土,在深部解释为新鲜基岩。地下水潜在区域的可充电性值范围从0到8毫秒。所有解释后来都得到了钻井数据的证实。
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