IDENTIFICATION OF GROUNDWATER DISTRIBUTION USING SELF POTENTIAL METHOD

Applied Research on Civil Engineering and Environment (ARCEE) Pub Date : 2019-10-28 DOI:10.32722/ARCEE.V1I01.1953

M. Hasan, T. Swastika, N. Martina, L. Wulandari

{"title":"IDENTIFICATION OF GROUNDWATER DISTRIBUTION USING SELF POTENTIAL METHOD","authors":"M. Hasan, T. Swastika, N. Martina, L. Wulandari","doi":"10.32722/ARCEE.V1I01.1953","DOIUrl":null,"url":null,"abstract":"Drought is one of the biggest problems for the community, this problem will be slightly resolved by the compilation of regions with groundwater sources. This research has been carried out in the karst area, Druju Village, Sumbermanjing District, Wetan Regency, Malang. The purpose of this study is to determine the distribution of underground air and the pattern between underground rivers in the Wonorejo draw well and spring sources in the Kaligoro River, Wonorejo Hamlet.The method that used is the Self Potential (SP) method to set the moving electrode (leap frop) with 104 measurement points. The results of this study indicate the value of electric potential shown between 0-13.5 mV, and assume that a low potential value (0-1 mV) is an indication of groundwater distribution. Areas with low potential values are found in the empathy area. When taking a distribution of water on the surface of the land that appears through the Kaligoro River, it does not need to go out in one stream with an underground river flowing in the wells of the residents. The area with the lowest potential value is a reference in making wells","PeriodicalId":378971,"journal":{"name":"Applied Research on Civil Engineering and Environment (ARCEE)","volume":"78 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2019-10-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Applied Research on Civil Engineering and Environment (ARCEE)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.32722/ARCEE.V1I01.1953","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}

引用次数: 1

Abstract

Drought is one of the biggest problems for the community, this problem will be slightly resolved by the compilation of regions with groundwater sources. This research has been carried out in the karst area, Druju Village, Sumbermanjing District, Wetan Regency, Malang. The purpose of this study is to determine the distribution of underground air and the pattern between underground rivers in the Wonorejo draw well and spring sources in the Kaligoro River, Wonorejo Hamlet.The method that used is the Self Potential (SP) method to set the moving electrode (leap frop) with 104 measurement points. The results of this study indicate the value of electric potential shown between 0-13.5 mV, and assume that a low potential value (0-1 mV) is an indication of groundwater distribution. Areas with low potential values are found in the empathy area. When taking a distribution of water on the surface of the land that appears through the Kaligoro River, it does not need to go out in one stream with an underground river flowing in the wells of the residents. The area with the lowest potential value is a reference in making wells

查看原文本刊更多论文

利用自电位法识别地下水分布

干旱是社会面临的最大问题之一，这一问题将通过地下水资源地区的编制略微解决。本研究在马琅魏滩县桑伯曼泾区Druju村喀斯特地区进行。本研究的目的是确定Wonorejo井地下河流与Wonorejo哈姆雷特Kaligoro河地下河流之间的地下空气分布和格局。采用自电位(SP)法设置运动电极(跃跃)，共104个测点。本研究的结果表明电位值在0-13.5 mV之间，并假设电位值低(0-1 mV)是地下水分布的指示。潜在价值较低的区域位于共情区。从卡利戈罗河(Kaligoro River)流出的地面上分配的水，不需要像从居民的水井中流出的地下河一样，以一条溪流的形式流出。潜力值最低的区域是打井时的参考

本文章由计算机程序翻译，如有差异，请以英文原文为准。

求助全文

约1分钟内获得全文求助全文

来源期刊

Applied Research on Civil Engineering and Environment (ARCEE)

自引率

0.00%

发文量