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Application of cross-hole radar tomograph in karst Area

机译:跨孔雷达层析成像仪在喀斯特地区的应用

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摘要

Electromagnetic wave CT, containing velocity CT and attenuation CT, is one of the effective geophysical prospecting methods to detect underground caves. The accuracy is low when applying the velocity CT and the attenuation CT separately into investigation in a karst area. This paper briefs the basic theory of electromagnetic wave CT imaging, and then mainly introduces the basic theory and applying methodology of cross-hole radar tomography for exploration in a karst area. Through numerical value simulation and practice verification, the advantage and disadvantage of the velocity CT and the attenuation CT of electromagnetic wave based on very high frequency have been studied, respectively. It has been found that the attenuation CT does better in confirming the location of karst caves, and the velocity CT is better in determining the shape of the karst caves although the whole distribution regular of the velocity CT is almost consistent with the attenuation CT.
机译:包含速度CT和衰减CT的电磁波CT是探测地下洞穴的有效地球物理勘探方法之一。将速度CT和衰减CT分别用于岩溶地区的调查时,精度较低。本文简要介绍了电磁波CT成像的基本原理,然后重点介绍了跨孔雷达层析成像在岩溶地区勘探的基本理论和应用方法。通过数值模拟和实践验证,分别研究了基于极高频的电磁波速度CT和衰减CT的优缺点。已经发现,尽管速度CT的整个分布规律几乎与衰减CT一致,但衰减CT能够更好地确定岩溶洞穴的位置,而速度CT可以更好地确定岩溶洞穴的形状。

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