Abstract

We attenuated incoherent seismic noise using singular value decomposition in the Laplace domain. Laplace-domain wavefields are sensitive to small-amplitude noise contaminating the first-arrival signals due to damping in the Laplace transform; this noise is boosted by the Laplace transform, so we need to attenuate the amplified noise in the Laplace domain. We transformed seismic wavefields into the Laplace domain and attenuated noise in the logarithmic wavefields by applying a moving average filter and low-rank approximation using truncated singular value decomposition. The process was very efficient since the number of matrix decomposition was the same as the number of damping coefficients. We removed highly oscillatory random noise from the logarithmic wavefields, and the denoised Laplace-domain wavefields were used in subsequent Laplace-domain full waveform inversions. The inversions of synthetic and field data demonstrated that denoising the Laplace-domain wavefield does not significantly alter the inversion results; however, this approach could reduce the misfit errors and uncertainties from noise.

Highlights

  • Seismic exploration is one of the most important tools for finding hydrocarbon reservoirs

  • Even when the signal-to-noise ratio (SNR) in the time-domain seismogram is high, the Laplace-transformed wavefield can suffer from amplified noise near the first arrival

  • We described how we suppressed the noise in the Laplace domain

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Summary

INTRODUCTION

Seismic exploration is one of the most important tools for finding hydrocarbon reservoirs. Even when the signal-to-noise ratio (SNR) in the time-domain seismogram is high, the Laplace-transformed wavefield can suffer from amplified noise near the first arrival. The overall SNRs for the damping coefficients of 4 s−1, 7 s−1, and 10 s−1 are 39.6, 46.3, and 50.0, respectively These SNRs are higher than those of the time-domain seismogram because they are dominated by large-amplitude near-offset signals. Laplace-domain wavefields suffer from small-amplitude noise near the first arrival in the time-domain seismogram, especially when the damping coefficient is small and the offset is large. The matrix approximation using SVD can be used for denoising since the seismic signal corresponds to large singular values, whereas random noise corresponds to small singular values [35]. We manually examined singular values and used the inflection point value of singular value graphs as the threshold value for each matrix [36]

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