Bayesian frequency-domain blind deconvolution of ground-penetrating radar data

被引:18
作者
Schmelzbach, C. [1 ]
Scherbaum, F. [1 ]
Tronicke, J. [1 ]
Dietrich, P. [2 ]
机构
[1] Univ Potsdam, Inst Erd & Umweltwissensch, D-14476 Potsdam, Germany
[2] UFZ Helmholtz Ctr Environm Res, D-04318 Leipzig, Germany
关键词
Deconvolution; Inverse filtering; Ground penetrating radar; GPR; Data processing; Vertical resolution; WAVELET ESTIMATION; P-WAVE; INVERSION; ENTROPY; PERMITTIVITY; FLUCTUATIONS; OPTIMIZATION; REFLECTIVITY; PRINCIPLES; MINIMUM;
D O I
10.1016/j.jappgeo.2011.08.010
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Enhancing the resolution and accuracy of surface ground-penetrating radar (GPR) reflection data by inverse filtering to recover a zero-phased band-limited reflectivity image requires a deconvolution technique that takes the mixed-phase character of the embedded wavelet into account. In contrast, standard stochastic deconvolution techniques assume that the wavelet is minimum phase and, hence, often meet with limited success when applied to GPR data. We present a new general-purpose blind deconvolution algorithm for mixed-phase wavelet estimation and deconvolution that (1) uses the parametrization of a mixed-phase wavelet as the convolution of the wavelet's minimum-phase equivalent with a dispersive all-pass filter, (2) includes prior information about the wavelet to be estimated in a Bayesian framework, and (3) relies on the assumption of a sparse reflectivity. Solving the normal equations using the data autocorrelation function provides an inverse filter that optimally removes the minimum-phase equivalent of the wavelet from the data, which leaves traces with a balanced amplitude spectrum but distorted phase. To compensate for the remaining phase errors, we invert in the frequency domain for an all-pass filter thereby taking advantage of the fact that the action of the all-pass filter is exclusively contained in its phase spectrum. A key element of our algorithm and a novelty in blind deconvolution is the inclusion of prior information that allows resolving ambiguities in polarity and timing that cannot be resolved using the sparseness measure alone. We employ a global inversion approach for non-linear optimization to find the all-pass filter phase values for each signal frequency. We tested the robustness and reliability of our algorithm on synthetic data with different wavelets, 1-D reflectivity models of different complexity, varying levels of added noise, and different types of prior information. When applied to realistic synthetic 2-D data and 2-D field data, we obtain images with increased temporal resolution compared to the results of standard processing. (C) 2011 Elsevier B.V. All rights reserved.
引用
收藏
页码:615 / 630
页数:16
相关论文
共 67 条
[1]  
Annan A., 2005, NEAR SURF GEOPHYS, P357, DOI [DOI 10.1190/1.9781560801719.CH11, 10.1190/1.9781560801719.ch11, 10.1190/1.9781560801719.ch, DOI 10.1190/1.9781560801719.CH]
[2]  
[Anonymous], 1997, FRACTALS CHAOS GEOLO, DOI DOI 10.1017/CBO9781139174695
[3]  
Arcone S. A., 2003, J ENVIRON ENG GEOPH, V8, P57
[4]   Ground-penetrating radar reflection profiling of groundwater and bedrock in an area of discontinuous permafrost [J].
Arcone, SA ;
Lawson, DE ;
Delaney, AJ ;
Strasser, JC ;
Strasser, JD .
GEOPHYSICS, 1998, 63 (05) :1573-1584
[5]   Complex permittivity and clay mineralogy of grain-size fractions in a wet slit soil [J].
Arcone, Steven ;
Grant, Steven ;
Boitnott, Ginger ;
Bostick, Benjamin .
GEOPHYSICS, 2008, 73 (03) :J1-J13
[6]   Enhancing the vertical resolution of surface georadar data [J].
Belina, F. A. ;
Dafflon, B. ;
Tronicke, J. ;
Holliger, K. .
JOURNAL OF APPLIED GEOPHYSICS, 2009, 68 (01) :26-35
[7]  
Berkhout A. J., 1974, Geophysical Prospecting, V22, P683, DOI 10.1111/j.1365-2478.1974.tb00111.x
[8]   LEAST-SQUARES INVERSE FILTERING AND WAVELET DECONVOLUTION [J].
BERKHOUT, AJ .
GEOPHYSICS, 1977, 42 (07) :1369-1383
[9]   On the Potential of Kinematic GPR Surveying Using a Self-Tracking Total Station: Evaluating System Crosstalk and Latency [J].
Boeniger, Urs ;
Tronicke, Jens .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2010, 48 (10) :3792-3798
[10]   Frequency-dependent attenuation analysis of ground-penetrating radar data [J].
Bradford, John H. .
GEOPHYSICS, 2007, 72 (03) :J7-J16