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Nonlinear parameter estimation in water-saturated sandy sediment with difference frequency acoustic wave.

Byoung-Nam Kim1, Suk Wang Yoon

  • 1East Sea Environment Research Department, Korea Ocean Research and Development Institute, 695-1 Hujeong-ri, Jukbyeon-myun, Uljin-gun, Gyeongbuk 767-813, Republic of Korea.

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This study introduces a difference frequency acoustic wave method to measure the nonlinearity parameter in ocean sediments. This technique offers a reliable way to assess sediment properties for underwater acoustic investigations.

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Area of Science:

  • Geophysics
  • Acoustics
  • Material Science

Background:

  • Nonlinear acoustic parameters are crucial for characterizing sediments.
  • Ocean floor and sub-bottom profiling require accurate sediment property data.
  • Traditional methods face challenges with attenuation in marine environments.

Purpose of the Study:

  • To utilize difference frequency acoustic waves to estimate the nonlinearity parameter of water-saturated sandy sediment.
  • To validate the applicability of this method in both laboratory and ocean conditions.
  • To compare estimated nonlinearity parameters with existing literature.

Main Methods:

  • Employing parametric acoustic array theory.
  • Generating difference frequency acoustic waves from two primary acoustic waves (76 and 114 kHz).
  • Measuring the nonlinearity parameter (beta) at difference frequencies (e.g., 38 kHz and 67 kHz).

Main Results:

  • The nonlinearity parameter (beta) for water-saturated sandy sediment was estimated as 80.5 ± 5.1 at 38 kHz.
  • Results showed good agreement with estimates at 67 kHz (using primary frequencies 137 and 204 kHz).
  • The estimated parameter aligns well with previously published data for similar sediments.

Conclusions:

  • The difference frequency acoustic wave method is effective for estimating the nonlinearity parameter of water-saturated sandy sediment.
  • This method's lower attenuation makes it suitable for in-situ ocean sediment analysis.
  • The technique shows promise for characterizing fluid-like granular media.