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Detection of Underground Voids in Tahura Japan Cave Bandung Using Ground Penetrating Radar

机译:利用地面穿透雷达检测Tahura Japan Cave Bandung的地下空隙

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The detection of underground voids is important due to their effects on subsidence higher risk. Ground Penetrating Radar is one of geophysical electromagnetic methods that has been proven to be able to detect and locate any void beneath the surface effectively at a shallow depth. This method uses the contrasts of dielectric properties, resistivity and magnetic permeability to investigate and map what lies beneath the surface. Hence, this research focused on how GPR could be applied for detecting underground voids at the site of investigation, The Japan Cave in Taman Hutan Raya located in Dago, Bandung, Indonesia. A 100 MHz GPR shielded antenna frequency were used to measure three >80 meters long measurement lines. These three GPR profiles were positioned on the surface above the Japan Cave. The radargram results showed existences of different amplitude regions proven to be the air-filled cavities, at a depth of <10 meters, and interfaces between the underneath layers.
机译:由于它们对沉陷率更高的风险影响,地下空隙的检测很重要。地面穿透雷达是已被证明能够在浅层深度下有效地检测和定位表面下方的任何空隙的地球物理电磁方法之一。该方法使用介电性质,电阻率和磁导率的对比度来研究和绘制表面下方的内容。因此,这项研究侧重于GPR如何在印度尼西亚大都市达戈·哈丹·林达的日本洞穴中检测调查部门的地下空隙。使用100 MHz GPR屏蔽天线频率测量三个> 80米的测量线。这三个GPR型材定位在日本洞穴上方的表面上。雷达格的结果表明,在<10米的深度处,被证明是空气填充空腔的不同幅度区域的存在,以及下层之间的界面。

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