Bedrock Investigation Using Resistivity Method as an Effort to Provide Subsurface Data at ITERA Campus

R. Rizka, S. Satiawan
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引用次数: 2

Abstract

This is a study of the application of resistivity method to provide the subsurface data for building/ foundation construction. The subsurface data which provided is resistivity data laterally and vertically and able to be used to investigate the depth and thickness of bedrock. 35 points of 1D resistivity data had been collected in ITERA campus that covered ± 150 Ha. It concentrates at northern to middle part of ITERA campus. Schlumberger configuration was employed with minimum and maximum AB/2 was 2 and 150 meter respectively and 3 varied MN. Iso-resistivity maps show high apparent resistivity value was distributed laterally and vertically. High apparent resistivity value is indicated as a representative of bedrock. The high apparent resistivity zone (resistive zone) was shown in Iso-resistivity map AB/2 2.5 and consistently up to AB/2 15 with the range of high apparent resistivity value is 80.2 up to 210.8 ohmmeter. The resistive zone was distributed laterally in Northeast to West part of study area where the depth and thickness of bedrock in west part is shallower and thicker than others.
利用电阻率法进行基岩调查,为ITERA校区提供地下数据
这是一项应用电阻率法为建筑/基础施工提供地下数据的研究。所提供的地下资料是横向和纵向的电阻率资料,可以用来调查基岩的深度和厚度。在±150 Ha的ITERA园区内,采集了35点一维电阻率数据。它集中在ITERA校园的北部到中部。采用斯伦贝谢配置,最小AB/2和最大AB/2分别为2和150米,MN变化幅度为3。等电阻率图显示,在横向和纵向上均有较高的视电阻率值。高视电阻率值是基岩的代表。高视电阻率区(电阻区)在等电阻率图AB/ 22.5和AB/ 215范围内一致,高视电阻率值范围为80.2 ~ 210.8欧姆。阻力带横向分布在研究区东北~西部,其中西部基岩深度和厚度较浅、较厚。
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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