ESTIMASI KEDALAMAN BATUAN DASAR MENGGUNAKAN METODA GEOLISTRIK TAHANAN JENIS KONFIGURASI DIPOLE-DIPOLE DI UNIVERSITAS NEGERI PADANG KAMPUS AIR TAWAR

Akmam Akmam, Media Febrina, Fatni Mufit, Akmam Akmam
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Abstract

Estimation of basement rocks depth has been done in Padang State University, Air Tawar campus. The research that uses Dipole-dipole resistivity geoelectrical method was aimed to determine the depth, resistivity value and the kinds of basement rocks. Data were collected by Ares Multielectrode in 4 lines. Processing of data was done using Res2dinv software with Robust Constraint inversion and it results 2D model of earth’s surface that consists of depth and resistivity value. The result of this research shows that there are basement rocks around sounding point 00053’44,0”S and 100020’79,8”E in 1st line and sounding point 00053’53,1”S and 100021’02,8”E in 2nd line at depth of more than 25,2 m with resistivity value 513 – 622 Ωm and 632 – 2150 Ωm. Basement rocks are also found in 3rd line around sounding point 00053’48,9”S dan 100020’50,6”E at depth of more than 21,85 m with resistivity value 596,5 – 734 Ωm, while 4th line at sounding point 00053’55,7”S and 100021’02,3”E did not find basement rocks. Possibility of basement rocks in 4th line are at depth of more than 29,5 m. Basement rocks that are found in this research is interpreted as Andesite. Information about basement rocks can be used for construction planning in Padang State University, Air Tawar campus.
基岩深度估计采用了美国州立大学淡水校园中最先进的凝胶式排泄方法
在巴东国立大学Air Tawar校区进行了基岩深度估算。利用偶极-偶极电阻率地电法进行研究,目的是确定基底岩的深度、电阻率值和种类。Ares多电极采集了4条线的数据。利用Res2dinv软件对数据进行鲁棒约束反演处理,得到由深度和电阻率值组成的地表二维模型。研究结果表明,在1线测深点00053′44 0”S和100020′79 8”E及2线测深点00053′53 1”S和100021′02 8”E附近存在基底岩,测深252 m以上,电阻率值分别为513 ~ 622 Ωm和632 ~ 2150 Ωm。在第3线探测点00053′48,9”S和100020′50,6”E附近也发现了基底岩,深度大于21,85 m,电阻率值为596,5 ~ 734 Ωm,而第4线探测点00053′55,7”S和100021′02,3”E未发现基底岩。4线基底岩的可能性在深度大于29.5 m。在这次研究中发现的基岩被解释为安山岩。有关基岩的资料可用于巴东州立大学Air Tawar校区的建设规划。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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