Estimation of soil overburden thickness/depth of rock strata using geo-physical survey at Himalayan region

IF 0.4 Q4 GEOSCIENCES, MULTIDISCIPLINARY
Luitel Keshar Kumar, V. Thirukumaran, Luitel Homnath
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Abstract

Estimation of soil overburden and depth of competent strata for construction of infrastructures in hilly terrain is a challenging job for engineers. Modern technologies like Electrical Resistivity Survey (ERS) techniques with site geological mapping have been carried out at the ridge area near Palace, Gangtok. Two independent 2D-electrical resistivity surveys profile sections using hybrid Schlumberger-Wenner method were conducted along the ridge line trending in the North-South direction. The ERS profile sections were taken on both the slopes of the ridge along its eastern and western flanks. With the collective information from field and geo-technical data, a comparatively stable slope has been identified with respect to geological conditions in the present work, which focuses on the vulnerable slope failure with respect to slope direction, local geological condition, depth of competent strata, thickness of soil overburden, water saturation zones and resistivity of the materials. Diamond core drilling of 15meters each was carried out at both the flanks of the slope to understand the sub-surface strata and correlate it with resistivity data generated by ERS survey. The result indicates that Sandy/silty soil with flakes of mica having resistivity of 107 ohm-m and weathered mica schist having resistivity more than 300 ohm-m in the present study area. Geological mapping in 1:3000 scale was carried in the area demarcation with various litho-units and rock type. The area is characterized by medium grade metamorphic rock sequence represented in the area by mica schist having dip of foliations towards NE direction and three sets of joint planes. The geometry of the rock orientation and slope direction plays a vital role for determining the overall stability condition of the area. The present study will provide technical input for structural engineers to design the structures in such geological conditions. Further, the thickness of overburden estimated from ERS has been validated by drilling data.
利用地球物理测量估算喜马拉雅地区岩层土壤覆盖层厚度/深度
在丘陵地形中,基础设施施工的覆盖层和适层深度的估算是一项具有挑战性的工作。在Gangtok Palace附近的山脊地区,采用了电阻率测量(ERS)技术和现场地质测绘等现代技术。采用斯伦贝谢-温纳混合方法沿南北方向的脊线进行了两个独立的2d电阻率测量剖面。ERS剖面剖面是在山脊的东侧和西侧斜坡上拍摄的。综合野外资料和土工资料,从地质条件上确定了一个较为稳定的边坡,重点从边坡走向、局部地质条件、适层深度、覆盖层厚度、含水带和材料电阻率等方面研究了边坡的脆性破坏。在边坡两侧各钻15米的金刚石岩心,以了解地下地层,并将其与ERS测量产生的电阻率数据相关联。结果表明,本研究区为砂质/粉质土,其中云母片的电阻率为107 ω -m,风化云母片岩的电阻率大于300 ω -m。对不同岩性单元和岩石类型进行了1:3000比例尺的地质填图。区内发育以云母片岩为代表的中变质岩层序,片理向NE方向倾斜,有3组节理面。岩石方向和边坡方向的几何形状对确定该地区的整体稳定状况起着至关重要的作用。本研究将为结构工程师在这种地质条件下进行结构设计提供技术参考。此外,利用ERS估算的覆盖层厚度已通过钻井数据得到验证。
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来源期刊
Journal of Geology Geography and Geoecology
Journal of Geology Geography and Geoecology GEOSCIENCES, MULTIDISCIPLINARY-
自引率
40.00%
发文量
57
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