Sudarwin Kamur
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引用次数: 0

摘要

摘要这项研究的动机是发展和人口的日益增长。人口增长的影响是住宅用地的增加。住宅用地的增加有时并没有伴随着PDAM提供的清洁水,因此人们使用挖井或钻井。在Kolaka地区,特别是Kolaka地区,这是一个研究地点,也是一个很难找到淡水的地方,所以地电法在确定哪些地方含有淡水方面起着非常重要的作用。本研究采用温纳和斯伦贝谢配置的电阻率地电法。利用Res2Dinv处理数据,绘制二维等电阻率图。利用Microsoft Excel、Surfer 10.2应用程序和ArcGIS对井深数据进行处理,绘制地下水网络图。测量轨迹使用7米、20米和40米的空间。研究结果表明,不同岩石的电阻率值不同。得到的电阻率变化从0.453 ~ 13988 m开始。地下水电阻率值范围为0.453 ~ 33.3 m。研究区含水层岩性为冲积砂岩。在研究地点,地下水一般在5米以上的深度
本文章由计算机程序翻译,如有差异,请以英文原文为准。
IDENTIFIKASI AIR TANAH MENGGUNAKAN METODE GEOLISTRIK DI KECAMATAN POMALAA KABUPATEN KOLAKA PROPINSI SULAWESI TENGGARA
ABSTRACTThis research is motivated by development and population growth continues to increase from day to day. The impact of population growth is the increase in residential land. The increase in residential land is sometimes not accompanied by the provision of clean water by PDAM, so that people use dug wells or drilled wells. In the Kolaka area, especially the Kolaka District area, which is the research location, it is also a location that is difficult to find fresh water, so the geoelectric method plays a very important role in efforts to determine which locations contain fresh water. This research uses resistivity geoelectric method with Wenner and Schlumberger configuration. Processing data using Res2Dinv to map 2D isoresistivity. The well depth data was processed using Microsoft Excel, Surfer 10.2 application and ArcGIS to create a groundwater network map. The measurement trajectory uses a space of 7 meters, 20 meters and 40 meters. The results of the study obtained different resistivity values for each rock. The resistivity variation obtained starts from 0.453 – 13,988 m. Groundwater resistivity values are in the range of resistivity values of 0.453 – 33.3 m. The lithology of the aquifers in the study area is alluvial and sandstone. In the research location, groundwater is generally found at a depth of more than 5 meters
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