有效源小波确定

J. van der Kruk, E. Slob
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引用次数: 9

摘要

对于探地雷达(GPR)数据成像,通常不考虑雷达小波的形式,因为实际源天线和接收天线的行为相当复杂,它们对小波有很大的影响。然而,小波的知识有可能改善探地雷达数据的成像和解释。提出了一种有效的处理小波的方法,即引入一个考虑有限长天线影响的有效小波。为了得到这个有效的小波,利用在实际CMP数据上观测到的孤立空气和地波的介质特性,计算了点源-接收机天线系统的脉冲响应。该脉冲响应与实际CMP数据的反卷积,产生一个有效的小波。结合偶极子天线在介质半空间中众所周知的辐射特性,可以有效地描述有限长度源-接收机天线系统发射的电磁波的传播。我们证明了从地波中可以以合理的精度提取浅层地下的性质。由数值计算得到的有限长度源接收机天线系统的有效小波,其最小相位小于由点源接收机天线系统产生的电场计算得到的有效小波。
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Effective source wavelet determination
For the imaging of ground-penetrating radar (GPR) data, the form of the radar wavelet is usually not taken into account, because the behaviour of actual source and receiver antennas, that have a large influence on the wavelet, is rather complex. Nevertheless, knowledge of the wavelet has the potential to improve the imaging and interpretation of GPR data. An efficient way to deal with the wavelet is proposed by introducing an effective wavelet that incorporates the influence of the finite-length antennas. To obtain this effective wavelet, the impulse response for a point source-receiver antenna system is calculated using the medium properties, that are obtained from the isolated air- and ground-waves observed on the actual CMP data. The deconvolution of this impulse response with the actual CMP data, yields an effective wavelet. Together with the well-known radiation characteristics of dipole antennas in a dielectric halfspace, the propagation of the electromagnetic waves emitted a finite-length source-receiver antenna system can be effectively described. We demonstrate that propertiesof the shallow subsurface can be extracted from the ground-wave with reasonable accuracy. An effective wavelet determined from numerical data calculated for a finite-length source-receiver antenna system shows an effective wavelet that is less minimum phase than the effective wavelet calculated from the electric field generated by a point source-receiver antenna system.
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