Modeling of low-frequency seismic waves in a shallow sea using the staggered grid difference method

Zaihua Lu; Zhihong Zhang; Jiannong Gu

doi:10.1007/s00343-017-6026-4

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Modeling of low-frequency seismic waves in a shallow sea using the staggered grid difference method

Updated：2023-05-16

- Modeling of low-frequency seismic waves in a shallow sea using the staggered grid difference method
- Journal of Oceanology and Limnology Vol. 35, Issue 5, Pages: 1010-1017(2017)
- Affiliations：
  
  College of Science Naval University of Engineering
- Author bio：
- Funds：
- DOI：10.1007/s00343-017-6026-4
  CLC：
- Online First：21 October 2016，
  
  Published：2017
- Accepted：
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Lu, Z., Zhang, Z. & Gu, J. Modeling of low-frequency seismic waves in a shallow sea using the staggered grid difference method., Chin. J. Ocean. Limnol. 35, 1010–1017 (2017). https://doi.org/10.1007/s00343-017-6026-4
DOI：

Lu, Z., Zhang, Z. & Gu, J. Modeling of low-frequency seismic waves in a shallow sea using the staggered grid difference method., Chin. J. Ocean. Limnol. 35, 1010–1017 (2017). https://doi.org/10.1007/s00343-017-6026-4 DOI：

摘要

Abstract

Elastic waves in the seabed generated by low-frequency noise radiating from ships are known as ship seismic waves and can be used to detect and identify ships. To obtain the propagation characteristics of ship seismic waves

an algorithm for calculating seismic waves at the seafloor is presented based on the staggered-grid finite difference method. The accuracy of the algorithm was tested by comparison with analytical solutions. Numerical simulation of seismic waves generated by a low-frequency point sound source in a typical shallow sea environment was carried out. Using various source frequencies and locations in the numerical simulation

we show that the seismic waves in the near field are composed mostly of transmitted S-waves and interface waves while transmitted P-waves are weak near the seafloor. However

in the far field

the wave components of the seismic wave are mainly normal modes and interface waves

with the latter being relatively strong in the waveforms. As the source frequency decreases

the normal modes become smaller and the interface waves dominate the time series of the seismic waves.

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references

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