Preliminary Result: Identification of Landslides Using Electrical Resistivity Tomography Case Study Mt. Betung

E. Ibrahim, Hikhmadhan Gultaf, H. Saputra, L. Agustina, Virgian Rahmanda, C. Suhendi, M. Sudibyo, R. Rizki
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引用次数: 1

Abstract

Institut Teknologi Sumatera (ITERA), ITB and local governments had been cooperated in establishing an astronomy observatory of ITERA Lampung (OAIL), which was located at Mt. Betung in the Pasawaran area. Geological setting of this area showed that the dominant lithology of Mt. Betung is pyroclastic, andesite, and breccia rocks. These volcanic deposits have the potential to move the materials down-slope by the force of gravity, steep slope, and high water-content. We have investigated some area with the potential of a landslide along OAIL construction area, which may be the cause of the landslip as well. We applied electrical resistivity tomography to analyse the electrical properties of the subsurface soil and determine the vulnerable area of the landslide. The result indicated that the area is divided into high resistivity at the top of the soil and low resistivity below. These high resistivity numbers are caused by pyroclastic flow while the lower one is caused by fracture-filled, mostly with water and clay.
初步结果:利用电阻率层析成像技术识别滑坡——以白头山为例
苏门答腊技术研究所(ITERA)、ib和地方政府已经合作建立了一个ITERA楠蓬天文台(OAIL),该天文台位于Pasawaran地区的Betung山。该地区地质背景表明,中间山主要岩性为火山碎屑岩、安山岩和角砾岩。这些火山沉积物有可能在重力、陡坡和高含水量的作用下将物质移下坡。我们调查了一些沿油田施工区域可能发生滑坡的地区,这些地区也可能是造成滑坡的原因。我们应用电阻率层析成像技术分析了地下土壤的电性,确定了滑坡的易损区。结果表明,该地区分为上部高电阻率区和下部低电阻率区。这些高电阻率值是由火山碎屑流引起的,而低电阻率值是由裂缝填充引起的,主要是水和粘土。
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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