T. Fitrianto, S. Supriyadi, Ulil Albab Taufiq, T. M. Mukromin, Anggit Pranatya Wardana
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引用次数: 1

摘要

本研究旨在确定巴彭萨里、巴格伦和普沃雷霍的地下水位置和分布。本研究采用斯伦贝谢配置的垂直电测深(VES)方法。研究数据采用IPMGEO电阻率计。本研究在两个线路长度为180米的位置进行。数据使用Microsoft Excel和IP2WIN软件进行处理。基于研究结果。在第一个位置,地下水深度为32.2m,厚度为3,3m。在第一个位置,地下水深度为34.6m,厚度为9.58m。第一位置的地下水比第二位置浅。然而,在第一个地点有负担过重。过载具有足够大的电阻率值(高于100欧姆-米)。该值已用于识别实体层。该层为安山岩角砾岩。当在第二位置时,过载具有足够小的电阻率值(50欧姆-米)。该值已被用于识别沉积层。该层为风化角砾岩和砾石。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Identifikasi Potensi Air Tanah Menggunakan Metode Geolistrik Resistivitas Konfigurasi Schlumberger di Kelurahan Bapangsari Kecamatan Bagelen Kabupaten Purworejo
This research aimed to determine location and distribution of groundwater in Bapangsari, Bagelen, Purworejo. This research used Vertical Electrical Sounding (VES) method with Schlumberger configuration. Research data were taken by using resistivity meter IPMGEO. This research did on 2 locations with length of line is 180 m. The data were processed using software Microsoft Excel and IP2WIN. Based on result of the research. On the first location, groundwater is at 32,2 m depth with 3,3 m thick. On the first location, groundwater is at 34,6 m depth with 9,58 m thick. Groundwater on the first location is shallower than second location. However, on the first location have over burden. The over burden has big enough resistivity value (higher than 100 ohm m). This value has been identifying of a solid layer. The layer is andesitic breccia. While on second location, the over burden has small enough resistivity value (50 ohm m). This value has been identifying of a sedimentary layer. The layer is weathered breccia and gravel.
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