Schlumberger地电法识别松巴哇省Telu Orong Strength Gunwang村的Akuifer地表水

Muhammad Faizal Zakaria, I. Suyanto
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引用次数: 2

摘要

森那旺区是松巴哇省的一个干旱程度很高的地区。本研究旨在提供更多关于地下水的信息,以支持塞纳旺区清洁水的可用性。本研究采用地电斯伦贝谢方法作为地表识别的主要方法。采集采用10个点采集,点间距为200 m,线长度为250 m。数据处理的结果是每个点测量的垂直电阻率随深度的变化。这一结果将被解释为岩石类型和地下水的存在。解释表明,地下水含水层的电阻率为12.54–26.28m,厚度为4.59–7.95m,深度(层上部)为23.29–50.56m。研究区域的地下水含水层类型为承压含水层。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Identifikasi Akuifer Air Tanah di Desa Senawang, Kecamatan Orong Telu, Kabupaten Sumbawa Menggunakan Metode Geolistrik Schlumberger
Senawang District is an area in Sumbawa Province with a high level of drought. This study aims to provide additional information about groundwater to support the availability of clean water in Senawang District. The study used Geoelectric-Schlumberger Method as main method of subsurface identification. The acquisition was conducted with 10 points acquisition, with spacing between points is 200 m and the line stretch of 250 m. The results of data processing are a vertical resistivity variation in depth at each point measurement. This result will be interpreted into the type of rock and the presence of groundwater. The interpretation shows that the presence of groundwater aquifer with resistivity of 12.54 – 26.28 m, thickness 4.59 – 7.95 m, depth (upper part of the layer) 23.29 – 50.56 m. The type of groundwaters aquifer in the study area are confined aquifers.
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