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Analyzing Soil Electrical and Strength Parameters Using Geophysical and Geotechnical Methods in Sungai Batu, Kedah

机译:利用Sugai Batu,Kedah中的地球物理和岩土工程分析土壤电气和强度参数

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Engineering structures require strong foundations to prevent hazards occur due to lack of understanding the subsurface soil. Geophysical and geotechnical surveys were conducted in Sungai Batu, Kedah to determine the effectiveness of correlating electrical parameters for vertical resolution and to evaluate soil strength by integrating Electrical Resistivity Tomography (ERT), Ground Penetrating Radar (GPR) and Standard Penetration Test (SPT). Results from ERT and GPR showed heterogeneity in the subsurface stratigraphy from surface to 8.6 m depth. The inversion model showed two zones of saturated (<150 Ωm) and dry zone (>150 Ωm). The integration of ERT, GPR and SPT is applied at the borehole position which is at distance of 9.5 m of the survey line. The resistivity values at distance of 9.5 m range from 7 - 30 Ωm due to soil formed by sedimentation originated from fluvial system (sandy clay and clay). Calculated electrical conductivity values from GPR radargram coincide and in range with values from ERT. At distance of 9.5 m, the electrical conductivity range from 32 - 148 mS/m. The N-value from SPT showed low value with range of 12 - 20. The correlation of electrical parameters from ERT and GPR showed good agreement which is effective for vertical resolution. Low resistivity (high conductivity), low N-value and heterogeneity of the soil denote unstable subsurface. Sandy clay/clay in Sungai Batu are detrimental for shallow foundation as the soil material is susceptible to subsidence and has irregular characteristics influenced by the weather. Hence, the soils up to 8 m depth were unstable, weak and may cause harm to building structure.
机译:工程结构需要强大的基础,以防止由于缺乏理解地下土壤而发生的危害。在Sungai Batu,Kedah进行地球物理和岩土工程调查,以确定通过整合电阻率断层扫描(ERT),地面穿透雷达(GPR)和标准渗透试验(SPT)来确定电气参数的有效性。 ERT和GPR的结果在从表面到8.6米深度的地下地层中显示出异质性。反转模型显示出两个饱和(<150Ωm)和干燥区(>150Ωm)的两个区域。 ERT,GPR和SPT的整合施加在钻孔位置,距离测量线的距离为9.5米。由于沉积物形成的土壤,从7-30Ωm的距离为9.5米的电阻率值,该距离来自河流系统(桑迪粘土和粘土)。计算GPR Radargram的电导率值与ERT的值相一致。在9.5米的距离,电导率范围为32-148ms / m。来自SPT的N值显示出低的值,范围为12-20.电气参数来自ERT和GPR的相关性显示出良好的垂直分辨率有效。低电阻率(高导电性),低N值和土壤的异质性表示不稳定的地下。 Sungai Batu的桑迪粘土/粘土对浅基础有害,因为土壤材料易受沉降,并且受到天气影响的不规则特征。因此,高达8米深度的土壤不稳定,弱,可能对建筑结构造成伤害。

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