Identifikasi Zona Akuifer Air Tanah Menggunakan Metode Geolistrik Resistivitas Konfigurasi Wenner dan Schlumberger di Megal Kabupaten Blora

Riko Fadla, Muhamad Syaugi Arif Nugraha, Erni Erni, Gunawan Gunawan
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引用次数: 0

Abstract

− Geoelectric research has been carried out in Megal, Blora Regency with the Wenner and Schlumberger configuration resistivity geoelectric method. The purpose of this research is to provide information about the subsurface layer as a potential point for groundwater drilling which has variations in rock lithology. The geoelectric method works by utilizing the propagation of electric current located below the surface so that data is obtained which is processed using Res2dinv software with the inversion method, and interpreted to identify groundwater aquifer zones in Megal, Blora Regency. The results of the Wenner configuration show up to a depth of 17.2 meters but the data does not find groundwater sources. Meanwhile, the results of the Schlumberger configuration showed up to a depth of 31.5 meters and an anomaly was found so that drilling was carried out to obtain soil layer data.
确定土壤含水层区域使用温纳和斯伦贝格尔地区的配置电阻波和斯伦贝佐的方法
−利用Wenner和斯伦贝谢配置电阻率地电方法,在Blora Regency的Megal进行了地电研究。本研究的目的是提供地下地层作为地下水钻探的潜在点的信息,这些地下地层具有不同的岩石岩性。地电法的工作原理是利用位于地表以下的电流传播,从而获得数据,并使用Res2dinv软件与反演方法进行处理,并进行解释,以确定Blora Regency Megal地区的地下水含水层。温纳构造的结果显示了17.2米的深度,但数据没有发现地下水来源。同时,斯伦贝谢配置的结果显示深度为31.5米,发现了一个异常,因此进行了钻井以获得土层数据。
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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