Multi-parameter Imaging by Finite Difference Frequency Domain Full Waveform Inversion of GPR Data: A Guide for Sedimentary Architecture Modeling

IF 1.9 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS pure and applied geophysics Pub Date : 2024-06-14 DOI:10.1007/s00024-024-03520-1
Mrinal Kanti Layek, Probal Sengupta
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Abstract

The need for reconstruction of the distribution of physical properties like dielectric permittivity and electrical conductivity of shallow subsurface sedimentary architecture leads to the development of an optimum strategy of GPR data inversion. In this paper, we present finite difference frequency domain (FDFD) full waveform inversion (FWI) method to get high-resolution subsurface model using GPR data. FWI is an optimization technique which involves in search of the minima between recorded and predicted data. The inversion process includes the quasi-Newton method and simultaneous frequency sampling strategy of irregular sampling. The Hessian term in quasi-Newton algorithm is approximated using preconditioned-LBFGS consideration and the search directions are also optimized after following the Wolfe conditions. At the end of each iteration during inversion, permittivity and conductivity models were updated and became ready to be the initial model for the next iteration. The goals of this research were to develop a robust framework for sedimentary-GPR data inversion and to evaluate the efficacy of the novel grid strategy introduced by Layek and Sengupta (2021) proposed for FWI. This paper presents a comparative analysis between conventional and newly proposed technique from Layek and Sengupta (2021), supported by numerical experiments conducted through our own MATLAB programming. Numerical tests conducted on a benchmark from previously published article, established the fact that new grid formulation produces a faster converging rate and required less computation time. This approach demonstrates remarkable efficacy when applied to a comprehensive sedimentary model comprising a lossy medium.

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通过有限差分频域全波形反演 GPR 数据进行多参数成像:沉积构造建模指南
由于需要重建浅表次表层沉积结构的介电常数和导电率等物理性质的分布,因此需要开发一种最佳的 GPR 数据反演策略。本文提出了有限差分频域(FDFD)全波形反演(FWI)方法,利用 GPR 数据获得高分辨率地下模型。全波形反演是一种优化技术,涉及寻找记录数据和预测数据之间的最小值。反演过程包括准牛顿法和不规则采样的同步频率采样策略。准牛顿算法中的 Hessian 项使用预处理-LBFGS 考虑近似,搜索方向也在遵循 Wolfe 条件后进行优化。在反演过程中的每次迭代结束时,都会更新介电常数和电导率模型,并将其作为下一次迭代的初始模型。本研究的目标是为沉积物-GPR 数据反演开发一个稳健的框架,并评估 Layek 和 Sengupta(2021 年)为 FWI 提出的新型网格策略的有效性。本文对 Layek 和 Sengupta(2021 年)提出的传统技术和新技术进行了比较分析,并通过我们自己的 MATLAB 编程进行了数值实验。对以前发表的文章中的基准进行的数值测试表明,新的网格计算方法收敛速度更快,所需的计算时间更少。这种方法在应用于包含有损介质的综合沉积模型时,显示出卓越的功效。
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来源期刊
pure and applied geophysics
pure and applied geophysics 地学-地球化学与地球物理
CiteScore
4.20
自引率
5.00%
发文量
240
审稿时长
9.8 months
期刊介绍: pure and applied geophysics (pageoph), a continuation of the journal "Geofisica pura e applicata", publishes original scientific contributions in the fields of solid Earth, atmospheric and oceanic sciences. Regular and special issues feature thought-provoking reports on active areas of current research and state-of-the-art surveys. Long running journal, founded in 1939 as Geofisica pura e applicata Publishes peer-reviewed original scientific contributions and state-of-the-art surveys in solid earth and atmospheric sciences Features thought-provoking reports on active areas of current research and is a major source for publications on tsunami research Coverage extends to research topics in oceanic sciences See Instructions for Authors on the right hand side.
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