在马来西亚槟城使用4-D电阻率层析成像和土壤力学方法联合解释土壤性质和行为研究

A. A. Bery, N. E. H. Ismail, N. Muztaza
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引用次数: 1

摘要

在3 - 4月的边坡研究中,采用地球物理和土力学相结合的方法研究了粘砂土的性质和行为。本研究采用的地球物理方法是4维电阻率层析成像(ERT),土力学采用了室内直剪、含水率、孔隙率、塑性极限和液限等试验。利用4-D ERT进行了3个月的内场调查,并沿调查线采集了土壤样品。模型电阻率随地形变化的结果表明,所有ERT结果均较好,均方根误差在2.4 ~ 2.4%之间。根据模型电阻率结果,将坡区地下划分为干粘土砂土(100 ~ 550 ω .m)和粘土砂土(550 ~ 1300 ω .m)两个主要带。模型电阻率结果表明,在3个月的调查期间,土壤的电特性发生了变化,这与土壤本身的含水量、孔隙度和结构有关。综上所述,ERT和土力学相结合的方法能够研究粘土砂土在3个月期间的性质和行为。
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Soil Properties and Behaviour Studies using Joint-interpretation of 4-D Electrical Resistivity Tomography and Soil Mechanics Methods in Penang, Malaysia
Summary The paper presents the integration of geophysics and soil mechanics methods in investigate the properties and behaviour of clayey sand soil properties for slope study from March until April. The geophysical method used in this study is 4-D electrical resistivity tomography (ERT), meanwhile soil mechanics used several laboratory tests, namely direct shear, moisture content, porosity, plastic limit and liquid limit. The infield survey using 4-D ERT was conducted for three different months and soil samples were collected along the survey line. The model resistivity with topography obtained showed all the ERT results gave a good results with RMS error between 2.4 - 2.4 %. Based on the model resistivity results, the subsurface of slope area can be divided into two main zone, dry clayey sand soil (100 - 550 ohm.m) and clayey sand soil (550 - 1300 ohm.m). The model resistivity results showed there are changes in electrical properties of soil, which associated with the moisture content, porosity and structure of soil itself during the three months of investigation period. In conclusion, the integration of both ERT and soil mechanics methods are capable to investigate the clayey sand soil’s properties and its behaviour during three months period.
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