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Assessment of Subsurface Profile at SILC, Nusajaya by 2D Resistivity Method

机译:2D电阻率法评估Silc,Nusajaya的地下谱

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An assessment of subsurface profile of a study area at Nusajaya. Johor was conducted using 2D resistivity method. The aims of the study are to determine the subsurface profile hence contouring the appearance of outcrop by 2D resistivity imaging. Subsurface structure can be delineated based on the physical and chemical parameter which is apparent resistivity of the medium. A survey line of 80m and minimum 2m electrode spacing was adopted using Pole-dipole array. Data acquisition on the survey line was completed and processed by using Res2Dinv software. The inversion model resistivity shows sandstone contains iron mineral (30-250 ohm-m) and weathered sandstone (500-1000 ohm-m). The lower part of the layer represents sandstone and siltstone exhibit high resistivity values of 1500-5000 ohm-m. The range from 30-1000 ohm-m correspond to the grade IV and V of sandstone in the actual profile. Meanwhile, the high range of the resistivity value matched the material with weathering grade II and III in ground mass. The deterioration of most physical properties was associated with the increase number of weathering grade.
机译:NUSAJAYA的研究区地下简谱评估。使用2D电阻率法进行了柔佛。该研究的目的是确定地下轮廓,因此通过2D电阻率成像来轮廓轮廓的外观。基于介质的表观电阻率的物理和化学参数,可以描绘地下结构。采用极偶极阵列采用80米和最小2M电极间距的测量线。通过使用Res2dinv软件完成并处理调查线上的数据采集。反转模型电阻率显示砂岩含有铁矿物(30-250欧姆-M)和风化的砂岩(500-1000欧姆-M)。该层的下部代表砂岩和硅铁晶具有1500-5000欧姆-M的高电阻率值。 30-1000欧姆-M的范围对应于实际配置文件中的砂岩等级和砂岩。同时,高范围的电阻率值与耐候II和III的材料相匹配。大多数物理性质的恶化与耐候等级的增加相关。

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