电阻率层析成像技术在土壤沉降调查中的应用——以巴基斯坦查谟和克什米尔地区朗格普拉卫星城为例

S. Kazmi, A. Niaz, J. Khan, S. Z. A. Gurdazi, J. Niaz
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引用次数: 1

摘要

土壤下沉是一个主要的工程问题,需要通过适当的规划和调查来解决。通常,工程师依靠钻孔数据或土壤测试来设计解决这类问题的方案。考虑到成本、时间和较少的破坏,地球物理方法是探测此类工程和环境问题的最佳方法。因此,采用电阻率层析成像(ERT)方法研究了巴基斯坦穆扎法拉巴德喜马拉雅山脉下Azad Jammu和Kashmir卫星城Langerpura的土壤沉降。两条剖面在研究区重叠,电极间距为5m,平均深度为40 ~ 50m。根据电阻率资料,确定了三个不同的地质带。电阻率3.0 - 15Ωm的低阻带为水饱和脆性砂岩。中电阻率带电阻率范围为100-1000 Ωm,由砂层、粘土层和河流层相间组成。在电阻率范围为1000 ~ 4000 Ωm的高阻带中,可见地下空腔。检测出引起地表土壤下沉的洞室大小。淤泥充填或压实灌浆建议作为沉降土稳定的工程解决方案。
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The use of Electrical Resistivity Tomography for Soil Sinking Investigation a case study in Satellite Town Langerpura Sub Himalaya Azad Jammu and Kashmir Pakistan
Soil sinking is a major engineering concern need to be addressed through proper planning and investigation. Usually Engineers depend on borehole data or soil tests for designing the solution for such problems. In view of cost, time and less destruction, geophysical methods are best to probe such engineering and environmental problems. Therefore, Electrical resistivity tomography (ERT) method used to investigate soil sinking in Satellite town Langerpura, Sub Himalayas Azad Jammu and Kashmir Muzaffarabad Pakistan. Two profiles acquired overlap the zone under study with electrode spacing 5m and average depth of 40-50m. Three different geological zones are identified on the base of resistivity data. Low resistivity zone having resistivity 3.0 – 15Ωm is water saturated friable sandstone. Intermediate resistivity zone with resistivity range 100-1000 Ωm consists of alternate layers of sand, clay and river deposits. High resistivity zone with resistivity range 1000-4000 Ωm show cavities in subsurface. The room size cavity detected which cause the soil sinking at surface. Muck filling or compaction grouting recommended as engineering solution for stabilization of sink soil.
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