Proposing New Methods to Enhance the Low-Resolution Simulated GPR Responses in the Frequency and Wavelet Domains

Q4 Earth and Planetary Sciences International Journal of Mining and Geo-Engineering Pub Date : 2014-12-01 DOI:10.22059/IJMGE.2014.53102
R. Ahmadi, N. Fathianpour, G. Norouzi
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Abstract

To date, a number of numerical methods, including the popular Finite-Difference Time Domain (FDTD) technique, have been proposed to simulate Ground-Penetrating Radar (GPR) responses. Despite having a number of advantages, the finite-difference method also has pitfalls such as being very time consuming in simulating the most common case of media with high dielectric permittivity, causing the forward modelling process to be very long lasting, even with modern high-speed computers. In the present study the well-known hyperbolic pattern response of horizontal cylinders, usually found in GPR B-Scan images, is used as a basic model to examine the possibility of reducing the forward modelling execution time. In general, the simulated GPR traces of common reflected objects are time shifted, as with the Normal Moveout (NMO) traces encountered in seismic reflection responses. This suggests the application of Fourier transform to the GPR traces, employing the time-shifting property of the transformation to interpolate the traces between the adjusted traces in the frequency domain (FD). Therefore, in the present study two post-processing algorithms have been adopted to increase the speed of forward modelling while maintaining the required precision. The first approach is based on linear interpolation in the Fourier domain, resulting in increasing lateral trace-to-trace interval of appropriate sampling frequency of the signal, preventing any aliasing. In the second approach, a super-resolution algorithm based on 2D-wavelet transform is developed to increase both vertical and horizontal resolution of the GPR B-Scan images through preserving scale and shape of hidden hyperbola features. Through comparing outputs from both methods with the corresponding actual high-resolution forward response, it is shown that both approaches can perform satisfactorily, although the wavelet-based approach outperforms the frequency-domain approach noticeably, both in amplitude and shape of the outputted hyperbola response.
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提出了在频率域和小波域增强低分辨率探地雷达模拟响应的新方法
迄今为止,已经提出了许多数值方法,包括流行的时域有限差分(FDTD)技术来模拟探地雷达(GPR)的响应。尽管有限差分法有许多优点,但它也有缺陷,例如在模拟具有高介电常数的最常见介质时非常耗时,导致正演建模过程非常持久,即使使用现代高速计算机也是如此。在本研究中,通常在探地雷达b扫描图像中发现的水平圆柱体的众所周知的双曲模式响应作为基本模型来研究减少正演建模执行时间的可能性。一般来说,常见反射目标的模拟GPR走线是时移的,就像地震反射响应中遇到的正常移动(NMO)走线一样。这表明将傅里叶变换应用于GPR走线,利用变换的时移特性在频域(FD)调整走线之间插入走线。因此,在本研究中,采用了两种后处理算法来提高正演建模的速度,同时保持所需的精度。第一种方法是基于傅里叶域中的线性插值,从而增加信号的适当采样频率的横向迹到迹间隔,防止任何混叠。第二种方法是基于二维小波变换的超分辨率算法,通过保持隐藏双曲线特征的尺度和形状,提高探地雷达b扫描图像的垂直和水平分辨率。通过将两种方法的输出与相应的实际高分辨率前向响应进行比较,表明两种方法的性能都令人满意,尽管基于小波的方法在输出双曲线响应的幅度和形状上都明显优于频域方法。
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来源期刊
International Journal of Mining and Geo-Engineering
International Journal of Mining and Geo-Engineering Earth and Planetary Sciences-Geotechnical Engineering and Engineering Geology
CiteScore
0.80
自引率
0.00%
发文量
0
审稿时长
12 weeks
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