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Polarimetric borehole radar measurement at the Mirror Lake test site

机译:Mirror Lake测试现场的极化钻孔雷达测量

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Abstract: In order to understand the potential of polarimetric borehole radar, field measurement was carried out at the Mirror Lake fractured-rock research site (NH, USA), in October 1998. The polarimetric borehole radar system can measure the full- polarimetry in a borehole by changing antenna arrangements. We developed a network analyzer based stepped-frequency radar. The radar penetration depth from the borehole in the reflection measurement was over 10 m, in the frequency range of 2 - 200 MHz. We could observe many clear reflections form fractures in each polarization state. Even in the raw data, we could observe the difference in the radar profile for different polarization states. Polarimetric future for the acquired data is analyzed and it was found that the depolarization effect is different in each fracture. We think this is closely related to the roughness of each fracture, and it is also related to physical properties of the fracture such as water permeability. Cluster analysis was tested for classification of fractures. !6
机译:摘要:为了了解极化钻孔雷达的潜力,1998年10月在Mirror Lake裂隙岩石研究站点(美国新罕布什尔州)进行了现场测量。极化钻孔雷达系统可以测量全波雷达的全极化率。通过更改天线布置来钻孔。我们开发了基于网络分析仪的步进频率雷达。在2-200 MHz的频率范围内,雷达在反射测量中的穿透深度超过10 m。我们可以观察到在每个偏振态下都有许多清晰的反射形成裂缝。即使在原始数据中,我们也可以观察到不同极化状态下雷达剖面的差异。对所获取数据的极化未来进行了分析,发现每个裂缝中的去极化效果都不同。我们认为这与每个裂缝的粗糙度密切相关,也与裂缝的物理性质(如透水性)有关。测试了聚类分析以对骨折进行分类。 !6

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