Efficient Deconvolution of Ground-Penetrating Radar Data

被引:24
|
作者
Schmelzbach, Cedric [1 ]
Huber, Emanuel [2 ]
机构
[1] ETH, Dept Earth Sci, Inst Geophys, CH-8092 Zurich, Switzerland
[2] Univ Basel, Appl & Environm Geol, CH-4056 Basel, Switzerland
来源
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING | 2015年 / 53卷 / 09期
关键词
Deconvolution; ground-penetrating radar (GPR); inverse filtering; signal processing; GPR DATA; DETERMINISTIC DECONVOLUTION; BLIND DECONVOLUTION; WAVELET ESTIMATION; OPTIMIZATION; PRINCIPLES;
D O I
10.1109/TGRS.2015.2419235
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The time (vertical) resolution enhancement of ground-penetrating radar (GPR) data by deconvolution is a long-standing problem due to the mixed-phase characteristics of the source wavelet. Several approaches have been proposed, which take the mixed-phase nature of the GPR source wavelet into account. However, most of these schemes are usually laborious and/or computationally intensive and have not yet found widespread use. Here, we propose a simple and fast approach to GPR deconvolution that requires only a minimal user input. First, a trace-by-trace minimum-phase (spiking) deconvolution is applied to remove the minimum-phase part of the mixed-phase GPR wavelet. Then, a global phase rotation is applied to maximize the sparseness (kurtosis) of the minimum-phase deconvolved data to correct for phase distortions that remain after the minimum-phase deconvolution. Applications of this scheme to synthetic and field data demonstrate that a significant improvement in image quality can be achieved, leading to deconvolved data that are a closer representation of the underlying reflectivity structure than the input or minimum-phase deconvolved data. Synthetic-data tests indicate that, because of the temporal and spatial correlation inherent in the GPR data due to the frequency-and wavenumber-bandlimited nature of the GPR source wavelet and the reflectivity structure, a significant number of samples are required for a reliable sparseness (kurtosis) estimate and stable phase rotation. This observation calls into question the blithe application of kurtosis-based methods within short time windows such as that for time-variant deconvolution.
引用
收藏
页码:5209 / 5217
页数:9
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