SEBARAN AIR TANAH MENGGUNAKAN METODE GEOLISTRIK RESISTIVITAS KONFIGURASI DIPOLE-DIPOLE

Resma Silvia, Usman Malik
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引用次数: 1

Abstract

This research has been worked in the Graha Mustamindo Permai 3 Housing area, Rimba Panjang Village, Tambang District. This research been thorough to calculate the value of measured rock resistivity in Graha Mustamindo Permai 3 Housing and analyze rock layer types through rock resistivity values at Sepakat street, Rimba Panjang, Riau. The method using in this research is geoelectric resistivity of the Dipole-dipole configuration, two lanes with the same length of 100 meters are used and spacing between electrodes is 7 meters. The data obtained were processed using Res2Dinv software version 3.54.44. The data result that obtained show two differences trajectories in Rimba Panjang Village has varying resistivity, namely in the first lane around 1.595 Ωm to 2,762 Ωm and in the second lane 1.594 Ωm to 5,879 Ωm. Groundwater potential in the first and second lanes is quite large and is thought to be in a free aquifer so that it is easy to drill.
地下水的排泄方法是协同对流
这项研究是在坦邦区Rimba Panjang村Graha Mustamindo Permai 3住宅区进行的。本研究深入计算Graha Mustamindo Permai 3 Housing的实测岩石电阻率值,并通过riba Panjang Sepakat street的岩石电阻率值分析岩层类型。本研究采用的方法为偶极-偶极配置地电阻率法,采用长度为100米的两条车道,电极间距为7米。使用Res2Dinv 3.54.44版软件对所得数据进行处理。结果表明,在riba Panjang村,1巷1.595 Ωm ~ 2762 Ωm附近和2巷1.594 Ωm ~ 5879 Ωm附近有两条不同的电阻率轨迹。第一和第二通道的地下水潜力相当大,被认为处于自由含水层中,因此很容易钻探。
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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