Plane Seismic Waves

​
time
0
trail length
5
number of points
50
pressure wave
amplitude
0.2
wavelength
3
shear wave
amplitude
0.1
wavelength
1
This Demonstration shows the propagation of elastic waves, commonly known as seismic waves. Two types of seismic waves are shown here: pressure waves (P-waves) and shear waves (S-waves). The P-wave is longitudinal, and so oscillates along the direction of the wave propagation, while the S-wave shakes perpendicular to the travel direction.
By combining these two types, you can simulate other types, such as Rayleigh waves. In such cases, the particles move in a circle or ellipse. The movement can be observed in detail by increasing the length of the trail.

Details

In the event of a real earthquake, the P-wave always precedes the S-wave, because the speed of P-waves is
v
p
=
K+
4
3
μ
ρ
,
while the speed of an S-wave is
v
s
=
μ
ρ
,
where
K
is the bulk modulus, μ is the shear modulus, and ρ is the density.

External Links

Spherical Seismic Waves
Elastic Wave (ScienceWorld)
P-Wave (ScienceWorld)
S-Wave (ScienceWorld)

Permanent Citation

Yu-Sung Chang
​
​"Plane Seismic Waves"​
​http://demonstrations.wolfram.com/PlaneSeismicWaves/​
​Wolfram Demonstrations Project​
​Published: March 7, 2011