Published September 2010 | Version v1
Journal article

Application of the nearly perfectly matched layer to the propagation of low-frequency acoustic waves

  • 1. Department of Geosciences, University of Tulsa, Tulsa, OK 74104 (United States)
  • 2. Computer Science Chair, Alabama A and M University, Normal, AL 35762 (United States)

Description

Seismic modelling is a very effective method to help us understand the characteristics of the seismic wave propagation in the Earth's interior. However, one tough problem is the presence of spurious reflections from the boundaries of the truncated computational domain, especially the reflections of low-frequency energy. In this paper, we apply the nearly perfectly matched layer (NPML) technique to suppress the artificial reflections from the edges of the 2D model in the case of acoustic waves of a low-frequency source (5 Hz). For the implementation of the finite-difference operator, we employ fourth-order accuracy methods in space and second-order accuracy methods in time. Through the numerical comparison between the NPML and the technique known as the convolutional perfectly matched layer (CPML), which is considered the boundary condition of optimum absorbing, we demonstrate that the NPML has better absorbing performance than the CPML. We suggest that a greater amount of analysis will be needed to study how NPML works facing the wide variety of complex media that are commonly used in seismic modelling

Availability note (English)

Available from http://dx.doi.org/10.1088/1742-2132/7/3/006

Additional details

Identifiers

DOI
10.1088/1742-2132/7/3/006;
PII
S1742-2132(10)44366-6;

Publishing Information

Journal Title
Journal of Geophysics and Engineering (Online)
Journal Volume
7
Journal Issue
3
Journal Page Range
p. 277-283
ISSN
1742-2140

INIS

Country of Publication
United Kingdom
Country of Input or Organization
International Atomic Energy Agency (IAEA)
INIS RN
44125975
Subject category
S58: GEOSCIENCES;
Descriptors DEI
ACCURACY; BOUNDARY CONDITIONS; LAYERS; PERFORMANCE; REFLECTION; SEISMIC WAVES; SIMULATION; SOUND WAVES