Potential Aquifer Exploration using Electrical Resistivity Imaging at Rumbio Jaya, Kampar, Riau

A. Suryadi, D. B. E. Putra, H. Kausarian, Abdul Rahman Sholeh, Malik Tauladani, Adriyadhi Adriyadhi
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引用次数: 0

Abstract

Groundwater sustainability has become a serious issue as a water resource needed by society. Therefore, electrical Resistivity Imaging was carried out at Rumbio Jaya, Kampar, and Riau to study groundwater aquifer's electrical characteristics. The equipment used is a Geocis resistivity meter with (32) multi-electrodes alignment. Wenner configuration electrode was applied in this survey. The 2-D Electrical Resistivity inversion results indicate there are three resistivity zones; (1) Low resistivity value (0.0093 – 4.84 Ωm) representing conductive clay; (2) intermediate resistivity value (1.07 – 171 Ωm) indicate as potential aquifer layer; and (3) a high resistivity value (61 – 4000 Ωm) occupying as bolder of rock. All the zones have different thicknesses and depths, but mostly clay layers dan boulders are shown as lenses in the aquifer of the study area. Meanwhile, the aquifer layer is found easily at a depth of 1 meter up to 30 meters.
利用电阻率成像技术在廖内省的Rumbio Jaya进行潜在含水层勘探
地下水作为社会所需的水资源,其可持续性已成为一个严重的问题。因此,在Rumbio Jaya、Kampar和Riau进行了电阻率成像,以研究地下水含水层的电学特性。使用的设备是Geocis电阻率计,具有(32)多电极排列。文纳配置电极应用于本次调查。二维电阻率反演结果表明,存在三个电阻率带;(1) 代表导电粘土的低电阻率值(0.0093–4.84Ωm);(2) 中间电阻率值(1.07~171Ωm)表示为潜在含水层;和(3)高电阻率值(61–4000Ωm)占据了岩石中较粗的部分。所有区域的厚度和深度不同,但在研究区域的含水层中,大部分粘土层和漂石显示为透镜体。同时,在1米至30米的深度很容易发现含水层。
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