Krisman Krisman, Citra Siti Fatimah Julianti, M Juandi
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摘要

地下水是人类赖以生存的重要水源之一。在Pekanbaru Payung Sekaki地区的Labuh Baru Barat村,使用斯伦贝谢地电电极配置进行了地下水流解释研究。测量距离选择240米。测量输出频率和电压。这些数据,然后被输入到软件进度和冲浪者11。该计算机程序输出的是地下水流形态和地下岩性图。地下水流格局的制图结果表明,水流方向由北向南方向,或由槟榔街向Payung Sekaki街流动。层的厚度从第一层开始,分别为4.05米和5.4米为粉砂-粘土层,第二层为13.07米和14.3米为泥石层,第三层为13.07米和15.2米为沙和冲积层,第四层为51.1米和79.2米为砾石砂层。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ANALISA INTERPRETASI POLA ALIRAN AIR BAWAH TANAH KELURAHAN LABUH BARU BARAT KECAMATAN PAYUNG SEKAKI PEKANBARU MENGGUNAKAN METODE GEOLISTRIK KONFIGURASI SCHLUMBERGER
Underground water is one of the important component sources for human being. Study on interpretation of underground water flow has been carried out using Geoelectric Schlumberger Electrode Configuration in Labuh Baru Barat Village, Payung Sekaki District, Pekanbaru. The range measurement was chosen to be 240 meter. The output of measurement  arecurrent and voltage. The data, then was inputed into software progress and surfer 11. The output of this computer program is a map of underground waterflow  pettern and underground lithology. The results of mapping of the pattern of underground water flow indicate that the direction of water flow from North to South direction, or from Pinang street to Payung Sekaki street. The thickness of the layer start  from the first layer that is 4.05 meters and 5.4 meters is a layer of silt- clay, the second layer is 13.07 meters and 14.3 meters is a layer of mud stone, the third layer is 13.07 meters and 15.2 meters is a layer of sand and alluvial and the fourth layer is 51.1 meters and 79.2 meters is layer of gravel sand.
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