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2-D Resistivity Study: The Horizontal Resolution Improvement by Introducing the Enhancing Horizontal Resolution (EHR) Technique

机译:二维电阻率研究:通过引入增强的水平分辨率(EHR)技术来提高水平分辨率

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2-D resistivity method is an indirect method to the shallow subsurface survey for maintaining the geo-environment. It is used to measure the apparent resistivity of subsurface. EHR technique was developed in order to get detail and deeper penetration for shallow subsurface study. In this study, 2-D resistivity with Enhancing Horizontal Resolution (EHR) technique is adopted to map and characterize the shallow subsurface (mineral exploration, geology, engineering and environment) using Pole-dipole array. The locations are Pagoh, Johor; Nusajaya, Johor and Puchong, Selangor (Malaysia). The study associated with mineral exploration is Pagoh, Johor while for Nusajaya, Johor is associated with geology and Puchong, Selangor is associated with engineering and environment. The 2-D resistivity and Induced polarization (IP) were employed at Pagoh, Johor to study and detect the subsurface variation of resistivity and chargeability of iron ore in the area. Result of the 2-D resistivity as well as the Induced Polarization (IP) shows that the area is underlain by a thick alluvium with resistivity value of 10 - 800 ohm-m iron which has chargeability rate of 0.1 - 3 msec. A sedimentary case study was executed at Nusajaya, Johor shows sandstone contains iron mineral (30 - 250 ohm-m) and weathered sandstone (500 -1000 ohm-m). Interpretation of 2-D resistivity data at Puchong, Selangor showed a low resistivity value (and this could be an influence factor the increasing water level because sandy silt is highly permeable in nature. The borehole, support the results of 2-D resistivity method relating a saturated zone in the survey area. There is a good correlation between the 2-D resistivity investigations and the results of borehole records. The stratigraphy and structure of the three case studies (mineral exploration, geology, engineering and environment) can be mapped effectively using 2-D resistivity with EHR technique.
机译:二维电阻率法是用于维护地下地球环境的一种间接方法。它用于测量地下的视在电阻率。开发EHR技术的目的是为了获得详细信息和更深的渗透性,以进行浅层地下研究。在这项研究中,采用具有增强水平分辨率(EHR)的二维电阻率技术,通过极-偶极子阵列绘制和表征浅层地下(矿物勘探,地质,工程和环境)。地点是柔佛州的帕戈;柔佛州努沙再也和雪兰莪蒲种(马来西亚)。与矿物勘探有关的研究是柔佛州的Pagoh,而对于Nusajaya来说,柔佛州与地质有关,而雪兰莪的蒲种则与工程和环境有关。柔佛州帕果(Pagoh)采用了二维电阻率和感应极化(IP)技术来研究和探测该地区铁矿石的电阻率和带电性的地下变化。二维电阻率和感应极化(IP)的结果表明,该区域位于厚厚的冲积层之下,冲积层的电阻率为10-800 ohm-m铁,带电率为0.1-3毫秒。在柔佛州努沙再也进行的沉积案例研究表明,砂岩中含有铁矿物(30-250 ohm-m)和风化砂岩(500 -1000 ohm-m)。雪兰莪蒲种的二维电阻率数据解释显示电阻率值较低(这可能是水位上升的影响因素,因为砂质粉砂具有高渗透性。该井孔支持二维电阻率方法的相关结果二维电阻率调查与井眼记录结果之间具有良好的相关性,可以有效地绘制三个案例研究(矿物勘探,地质,工程和环境)的地层和结构使用带有EHR技术的二维电阻率。

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