Suryadi Simbolon, Usman Malik
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引用次数: 1

摘要

地下水是人类生命最需要的水资源之一。地下水的可用性和唐克朗拉瓦伊村不断增长的人口需要使用干净的水。这项研究旨在确定构成土壤和土壤含水层的岩层以及地下水的质量。对于土层,采用斯伦贝谢配置地电法,对于含水层测试,采用Jacobs步降法确定地下水位随时间的下降。对于空气质量使用弧度,其中pH值,TDS,浊度值描述电阻率值。研究结果基于90 m长轨道上的数据处理,在7-10 m深度发现地下水,电阻率值为114 m,其电阻率值为< 1000 m的花岗岩、砂、砾石、冲积层组成层或含水层由于存在孔隙小的多孔岩层而部分连通。对井内含水层进行检测,根据相对较小的地下水减少量,即0.2和0.1 cm,流量0.43升/秒,透过率值为971.901 m2/天,分类为自由含水层或连通含水层。根据印度尼西亚共和国卫生部长2010年第492号条例所述的结果,地下水不能被消耗,因为获得的pH值< 6.5或酸性,并被归类为部分连通含水层,因为水的酸性越强,获得的电阻率值就越高。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ANALISA DISTRIBUSI AIR BAWAH TANAH DI KELURAHAN TANGKERANG LABUAI MENGGUNAKAN METODE COOPER-JACOBS DAN GEOLISTRIK KONFIGURASI SCHLUMBERGER
Groundwater, one part of water resources is the most needed by humans for life. The availability of ground water and the increasing population growth in Tangkerang Labuai Village reguire the use of clean water. This study aims to determine the rock layers that makes up the soil and soil aquifers and the quality of groundwater. For the soil layer, it user the Schlumberger configuration geoelectric method,for the aquifer test, uses the Jacobs step drawdown method to determine the decrease of groundwater level is time. For air quality uses radians where the pH, TDS, turbidity values describe the resistivity value. The results of the research based on data processing on a 90 m long track,ground water is found at a depth of 7-10 m with a resistivity value of 114 m, which is categorized as granite, sand, gravel, alluvium constituent layers with a resistivity value of < 1000 m or the aquifer is partially connected due to the presence of a porous rock layerhaving small pores. To test the aquifer in the well based on the relatively small decrease in groundwater, namely 0.2 and 0.1 cm with a discharge of 0.43 liter/second with a transmissivity value of 971.901 m2/day, categorized as free or connected aquifer. Groundwater could not be consumed from the results as as stated to the regulation of the Minister of Health of the Republic of Indonesia number 492 of 2010, because the pH obtained was < 6.5 or acidic nature and categorized as partially connected aquifers because the more acid of water is formal, the higher the resistivity value is obtained.
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