基于探地雷达数据振幅反演的颗粒材料岩石物性参数估计——以中国地质大学地球物理研究所(GTO) Irapuato为例。、墨西哥

Félix Antonio Centeno Salas, D. C. Freyre
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引用次数: 0

摘要

为了开展这项工作,采用了一种非常规技术来估计岩石物性参数的空间分布。将振幅反演方法应用于探地雷达数据的反射率估计,所采用的算法需要通过常规处理技术对数据进行预处理。所提出的反演算法,与带矩阵操作,已被证明是计算效率更高的传统方法的反演。在具有近地表岩性序列信息的约束下,采用递推计算技术估计了储层物性的空间分布。岩石物性参数是通过应用地下颗粒材料的电性和物性之间的经验关系来估计的,类似于本工作开发过程中研究的那些。本文提出的探地雷达记录分析方法用于研究地点的特征描述,并从岩土工程钻孔中获得岩性信息。利用该方法反演得到的探地雷达剖面表明,模拟地层与研究地点的岩性层序相对应。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Estimation of Petrophysical Parameters of Granular Materials, Applying an Amplitud Inversion From GPR Data: Case Study Irapuato, GTO., Mexico
For the development of this work an unconventional technique to estimate the spatial distribution of petrophysical parameters was applied. The inversion of the amplitude is applied to the GPR data for estimating reflectivity, the used algorithm requires preconditioning of the data by conventional processing techniques. The proposed inversion algorithm, operating with band matrices, had shown to be computationally more efficient than the conventional methods of inversion. The spatial distribution of physical properties is estimated by a recursive calculation technique, with the constraint of having information of the near surface lithological sequence. Petrophysical parameters are estimated by applying an empirical relationship between electrical and physical properties of the subsoil granular materials, similar to those studied during the development of this work. The methodology for the analysis of GPR records proposed in this paper was used for the characterization of a study site, with available lithological information from a geotechnical borehole. GPR profiles obtained by the inversion proposed method show that the simulated stratigraphy corresponds to the lithological sequence at the study site.
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