ANALISA KEDALAMAN AIR PANAS MENGGUNAKAN METODE GEOLISTRIK KONFIGURASI SCHLUMBERGER DI OBJEK WISATA AIR PANAS PAWAN

Cici Sang Putri, Usman Malik
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引用次数: 4

Abstract

Hot water depth analysis have been carried out using the Schlumberger Configuration geoelectric method. This research investigatis subsurface conditions by analyzing the resistivity value. The study was conducted at the Pawan Hot Spring tourisme object, Rokan Hulu, Riau using the Schlumberger rule which is brought closer to 2 track points with a length of 90 meters each. Measurment data were processed using Progress Software and the resistivity values obtained at Line I 100,83 – 63,54 Ohm.m with depths of 0,00 – 46 m and at Line II 146,73 – 239,71 Ohm.m with depths of 0,00 – 33 m. The interpretation result of the two tracks obtained that the hot water flow in Line I is in the sand layer with resistivity values 95,28 Ohm.m and 63,54 Ohm.m at depths of 3,77 – 46 m. Line II is found in the sandy clay layer with a resistivity value of 1,05 Ohm.m at depth of 3,56 – 3,66 m.
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温水深度分析使用斯伦贝谢在帕万温泉旅游景点的排气管配置
热水深度分析采用斯伦贝谢配置地电方法进行。本研究通过分析电阻率值来调查地下情况。该研究是在廖内省罗坎Hulu的坡湾温泉旅游对象进行的,使用斯伦贝谢规则,即接近2个轨道点,每个轨道点的长度为90米。使用Progress软件处理测量数据,并在I线100,83 - 63,54欧姆处获得电阻率值。m深度为0 - 46米,II线为146,73 - 239,71欧姆。M,深度为0 - 33米。两条轨迹解释结果表明,1线热水流位于砂层,电阻率为95,28欧姆。m和63,54欧姆。在3.77 - 46米的深度。线II位于砂质粘土层,其电阻率值为1.05欧姆。水深3.56 - 3.66米。
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