The role of geophysical ERT method to evaluate the leakproofness of diapragm wall of deep foundation trenches on the example of the construction of retail and office complex in Lublin, Poland

IF 0.6 Q4 GEOSCIENCES, MULTIDISCIPLINARY
G. Pacanowski, P. Czarniak, A. Bąkowska, R. Mieszkowski, F. Welc
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引用次数: 8

Abstract

Abstract This paper addresses the problem of assessing the leakproofness of the bottom of a deep foundation trench, secured by cavity wall, using geophysical methods of electrical resistivity tomography. The study was conducted on a large construction project in Lublin, in a place where there are complicated soil-water conditions: the groundwater level is above the proposed depth of foundation trench, the subsoil is heterogeneous, and there are karsted and weathered carbonate sediments with confined aquifer below the bottom of the trench. A hydraulic fracture occurred at the bottom of the trench during the engineering works, which caused the water flow into the trench. In order to recognize the soil-water conditions the first stage of geophysical measurements of electrical resistivity tomography (ERT) was made. The applied methodology allowed to determine the extent of the hydraulic fracture zone within the bottom of foundation trench. In order to assess the leakproofness of Diaphragm Wall the geophysical ERT measurements were repeated (stage 2) A clear reduction in the value of the electrical resistivity of soils in the area of hydraulic fracture was caused by clay injection. The results of ERT measurements are discussed and graphically presented.
地球物理ERT方法在波兰卢布林零售和办公综合体建设中深基坑连续墙防漏性评价中的作用
摘要本文研究了利用地球物理电阻率层析成像方法评估深基坑底部防渗性能的问题。本研究是在卢布林的一个大型建设项目中进行的,该地区的土壤-水条件复杂:地下水位高于建议的基坑深度,底土不均匀,沟底以下有岩溶和风化碳酸盐沉积物,含水层承压。工程施工过程中,沟槽底部发生水力裂缝,导致水流进入沟槽。为了识别土壤水分状况,进行了地球物理电阻率层析成像(ERT)的第一阶段测量。所采用的方法可以确定基坑底部水力破裂带的范围。为了评估连续墙的防漏性,重复进行了地球物理ERT测量(第二阶段)。水力裂缝区域土壤电阻率值明显降低是由于注入粘土引起的。对ERT测量结果进行了讨论,并以图形形式呈现。
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来源期刊
Studia Quaternaria
Studia Quaternaria GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
1.40
自引率
0.00%
发文量
0
期刊介绍: Studia Quaternaria is designed to publish scientific works concerning the Quaternary, on local, regional and global scale. Studia Quaternaria is interested in all fields of research dealing with stratigraphy and reconstruction of the past environments, including palaeogeography, palaeoecology, palaeoclimatology, palaeohydrology etc. The journal is also open to studies of natural environmental processes, and to recognition of mechanisms involved in the dynamics of our environment. The clue is that the Quaternary is still ongoing and vivid, and understanding of its past and present development support each other.
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