Enhancing the vertical resolution of surface georadar data

被引:30
作者
Belina, F. A. [1 ]
Dafflon, B. [1 ]
Tronicke, J. [2 ]
Holliger, K. [1 ]
机构
[1] Univ Lausanne, Inst Geophys, CH-1015 Lausanne, Switzerland
[2] Univ Potsdam, Inst Geosci, D-14415 Potsdam, Germany
基金
瑞士国家科学基金会;
关键词
Deconvolution; Spectral balancing; Georadar; Data processing; Vertical resolution; GROUND-PENETRATING RADAR; REFLECTION; PROPAGATION;
D O I
10.1016/j.jappgeo.2008.08.011
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
There are far-reaching conceptual similarities between bi-static surface georadar and post-stack, "zero-offset" seismic reflection data, which is expressed in largely identical processing flows. One important difference is, however, that standard deconvolution algorithms routinely used to enhance the vertical resolution of seismic data are notoriously problematic or even detrimental to the overall signal quality when applied to surface georadar data. We have explored various options for alleviating this problem and have tested them on a geologically well-constrained surface georadar dataset. Standard stochastic and direct deterministic deconvolution approaches proved to be largely unsatisfactory. While least-squares-type deterministic deconvolution showed some promise, the inherent uncertainties involved in estimating the source wavelet introduced some artificial "ringiness". In contrast, we found spectral balancing approaches to be effective, practical and robust means for enhancing the vertical resolution of surface georadar data, particularly, but not exclusively, in the uppermost part of the georadar section, which is notoriously plagued by the interference of the direct air- and groundwaves. For the data considered in this study, it can be argued that band-limited spectral blueing may provide somewhat better results than standard band-limited spectral whitening, particularly in the uppermost part of the section affected by the interference of the air- and groundwaves. Interestingly, this finding is consistent with the fact that the amplitude spectrum resulting from least-squares-type deterministic deconvolution is characterized by a systematic enhancement of higher frequencies at the expense of lower frequencies and hence is blue rather than white. It is also consistent with increasing evidence that spectral "blueness" is a seemingly universal, albeit enigmatic, property of the distribution of reflection coefficients in the Earth. Our results therefore indicate that spectral balancing techniques in general and spectral blueing in particular represent simple, yet effective means of enhancing the vertical resolution of surface georadar data and, in many cases, could turn out to be a preferable alternative to standard deconvolution approaches. (C) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:26 / 35
页数:10
相关论文
共 26 条
[1]  
Annan AP, 2005, WTR SCI TEC LIBR, V50, P185
[2]   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
[3]   Using two- and three-dimensional georadar methods to characterize glaciofluvial architecture [J].
Beres, M ;
Huggenberger, P ;
Green, AG ;
Horstmeyer, H .
SEDIMENTARY GEOLOGY, 1999, 129 (1-2) :1-24
[4]  
Bristow C. S., 2003, GEOLOGICAL SOC LONDO, V211
[5]   Inferring the lateral subsurface correlation structure from georadar data: Methodological background and experimental evidence [J].
Dafflon, B ;
Tronicke, J ;
Holliger, K .
GEOSTATISTICS FOR ENVIRONMENTAL APPLICATIONS, PROCEEDINGS, 2005, :467-478
[6]   GROUND-PENETRATING RADAR FOR HIGH-RESOLUTION MAPPING OF SOIL AND ROCK STRATIGRAPHY [J].
DAVIS, JL ;
ANNAN, AP .
GEOPHYSICAL PROSPECTING, 1989, 37 (05) :531-551
[7]  
Hardy H.H., 1994, FRACTALS RESERVOIR E
[8]   Modeling ground-penetrating radar wave propagation and reflection with the Jonscher parameterization [J].
Hollender, F ;
Tillard, S .
GEOPHYSICS, 1998, 63 (06) :1933-1942
[9]  
Holliger K, 2003, HETEROGENEITY IN THE CRUST AND UPPER MANTLE: NATURE, SCALING AND SEISMIC PROPERTIES, P131
[10]  
HUGGENBERGER R, 1993, GEOLOGICAL SOC LONDO, V75, P163