 |
| You will need a slinky. |
| |
 |
| Stretch the slinky across the table with the help of a friend. |
| |
 |
| Pull about 5 or 6 coils towards you with one finger and release. What do you see? |
| |
 |
| Pull a coil sideways and release. What happens this time? |
| |
Try this: Seismic slinky
You will need
- Slinky
- Friend
- Long table or bench
What to do
- Have a friend hold one end of the slinky at one end of the table.
- Holding the other end of the slinky, stand at the other end of the table. Stretch the slinky tight across the tabletop.
- Pull about 5 or 6 coils towards you with one finger.
- Release your finger. What do you observe? Which way do the coils move?
- Keeping the slinky stretched tight, pull a coil sideways and release. Which way do the coils move this time?
What’s happening?
Both types of motion observed in the slinky are examples of wave motion. Waves are a way of transferring energy from one place to another.
In this activity the waves move through a medium – the slinky. The medium a wave travels through can be many things, including water, air and the Earth. A medium is made up of individual parts, which in this activity are the slinky’s coils. In a medium such as air, the components are gas molecules.
This activity demonstrates two types of waves. The first wave is an example of a longitudinal wave. In a longitudinal wave, the coils move in the same direction as the wave itself. An example of a longitudinal wave is sound moving through the air.
Transverse waves are the second type of wave in this activity. In a transverse wave, the coils move at right angles to the direction of the wave. The ripples on the surface of water look something like transverse waves.
Applications
Seismic waves are caused by earthquakes. In seismology, primary waves (or P-waves) are a type of longitudinal seismic wave. In this case, the medium is the Earth. P-waves travel fastest through the Earth, and are the first type of seismic wave detected after an earthquake. Secondary waves (or S-waves) are transverse seismic waves that travel slower than P-waves, so are detected later.
Both P-waves and S-waves travel deeper within the Earth. There are other types of waves, called surface waves, which travel along the surface of the Earth.
Earthquakes, and particularly surface waves, can be highly destructive. Being able to detect the less damaging P-waves before the surface waves arrive can allow authorities to prepare, minimising the damage caused by a quake.
In Japan in 2011, P-waves were detected with enough time for the train system to be shut down. While the earthquake was still highly damaging, stopping the trains most likely saved lives.
By Patrick Mahony
More information
View the online version
No comments:
Post a Comment