在复杂场景中对空洞进行GPR映射,并结合时间深度转换
Raffaele Persico1, Ilaria Catapano2, Giuseppe Esposito2
1Department of Environmental Engineering DIAM, University of Calabria, Via Pietro Bucci Cubo 44A, 87036 Rende, Italy.
Sensors (Basel, Switzerland)
|May 25, 2024
概括
本研究引入了一种综合的时间深度转换策略,以提高使用地面透雷达 (GPR) 的地下空洞成像能力. 该方法改善了地下特征的重建,如空洞和洞穴.
科学领域:
- 地质物理学 地质物理学
- 地下表面成像技术
- 电磁方法 电磁方法
背景情况:
- 从地物理数据中重建地下空洞,如空洞和洞穴,面临着挑战.
- 精确的成像需要考虑不同介质中的电磁波传播.
研究的目的:
- 开发和验证一个综合的时间深度转换策略,以改善空洞重建.
- 通过使用地面穿透雷达 (GPR) 增强地下场景的解释.
主要方法:
- 开发了一种新的综合时间深度转换策略.
- 分析了来自受控实验的地面透雷达 (GPR) 数据.
- 采用了两种成像方法:经典迁移和线性反向散射.
主要成果:
- 综合的时间深度转换策略明显改善了地下空洞的成像.
- 实现了地下特征的改进重建和解释.
- 该策略在经典迁移和反向散射方法中都被证明是有效的.
结论:
- 拟议的综合时间深度转换策略为基于GPR的地下空洞成像提供了显著的改进.
- 这种方法提高了地质物理数据的准确性和可解释性,用于检测地下异常.
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