首页> 外文期刊>MATEC Web of Conferences >Application of 2D spatial imaging method for identification of a fault lines and subsurface landslide at “Taman Unnes”, Semarang, Indonesia
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Application of 2D spatial imaging method for identification of a fault lines and subsurface landslide at “Taman Unnes”, Semarang, Indonesia

机译:二维空间成像方法在印尼三宝垄“ Taman Unnes”断层线和地下滑坡识别中的应用

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In the last five years, landslide occurred many times in this area. The worst landslide was in 2014, which destroyed many houses and infrastructure such as road, water supply utilities and electricity. This study proposed an identification of landslide method by using of geo electricity as subsurface investigation of landslide. This study aims to identify the type of landslide and slip surface potential by using emergence of 2D spatial imaging. The application of geophysical has not been used as a result of landslide identification. The well-known argument state that geophysical is the only way to make images on the type and rock by using resistivity. The geological and soil physical properties required by engineers to analyse landslide potential are not well presented. As a consequence, the solution of soil reinforcement on landslide prone area to minimize the risk is presented as an engineering judgment of problem solving. Therefore, this paper discusses about soil properties and imaging to identify the area affected by future landslide. By using a multi-electrode electrical array, the 2D geophysical imaging was used to investigate the complex structure of soil stratigraphy and geological properties. The results showed that the area of the study was shown as a stable area with andesite intrusion. In addition, some areas were suspected as landslide prone area which was indicated resources by saturated clay of soil beneath.
机译:在过去的五年中,该地区发生了多次滑坡。最严重的滑坡发生在2014年,摧毁了许多房屋和基础设施,例如道路,供水公用事业和电力。这项研究提出了一种利用地电作为地下滑坡调查方法来识别滑坡的方法。这项研究旨在通过使用二维空间成像技术来识别滑坡的类型和滑坡面的潜力。由于滑坡识别,尚未使用地球物理方法。众所周知,地球物理是通过电阻率在类型和岩石上成像的唯一方法。工程师分析滑坡潜力所需的地质和土壤物理特性并未得到很好的介绍。因此,提出了在滑坡易发地区进行土壤加固以最大程度降低风险的解决方案,作为解决问题的工程判断。因此,本文讨论了土壤特性和成像,以识别受未来滑坡影响的区域。通过使用多电极电阵列,二维地球物理成像被用来研究土壤地层的复杂结构和地质特性。结果表明,研究区域显示为安山岩侵入的稳定区域。此外,有些地区被怀疑是滑坡易发地区,其下方的土壤饱和黏土表明资源丰富。

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