4.6 Article

A numerical study of simultaneous-source full waveform inversion with l1-norm

Journal

GEOPHYSICAL JOURNAL INTERNATIONAL
Volume 194, Issue 3, Pages 1727-1737

Publisher

OXFORD UNIV PRESS
DOI: 10.1093/gji/ggt182

Keywords

Inverse theory; Numerical approximation and analysis; Probability distributions; Computational seismology; Wave propagation

Funding

  1. Energy Efficiency & Resources of the Korea Institute of Energy Technology Evaluation and Planning (KETEP)
  2. Korea government Ministry of Knowledge Economy [2010T100200133]
  3. Human Resources Development of the Korea Institute of Energy Technology Evaluation and Planning (KETEP)
  4. INHA UNIVERSITY
  5. Korea Evaluation Institute of Industrial Technology (KEIT) [2013251010005A] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)

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Simultaneous-source techniques have been proposed to reduce the acquisition cost and alleviate the computational overburden of data processing, and they have been applied to full waveform inversion (FWI) in recent years. These techniques are mainly based on the l(2)-norm objective function (least-squares criterion). However, if we consider that real field data contain noise such as outliers, it would be preferable to use the robust objective function in simultaneous-source FWI. In this study, we propose combining the simultaneous-source FWI with the l(1)-norm objective function (least-absolute criterion), which is known to be robust to data containing noise, specifically outliers. For the l(1)-norm-based simultaneous-source (SS-1) FWI, we first verify the crosstalk reduction and the robustness to data containing outliers. The expectations of the gradient direction directly give an evidence for the crosstalk reduction, and a signal-to-noise ratio analysis supports the convergence of our algorithm. The analysis shows that the crosstalk noise of the SS-1 FWI can be suppressed by random phase encoding. In addition, the spectrum of the weighted residuals indicates that the main property of the l(1)-norm objective function is preserved in the SS-1 FWI. Numerical examples show that the SS-1 FWI produces reliable results as the l(2)-norm simultaneous-source FWI does, similar to the case of the individual-source FWI. These results support the idea that combining the simultaneous-source FWI with the l(1)-norm objective function improves the computational efficiency and preserves the intrinsic characteristics of the l(1)-norm objective function.

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