Lesson 1 of 5
What travels in a wave?
I can describe wave motion using ropes, springs and a ripple tank, including wavefronts.Syllabus
Syllabus K326 / K327, 9(a). Describe wave motion using ropes, springs and a ripple tank, including wavefronts.
I can explain wave transfer of energy without transfer of matter.Syllabus
Syllabus K326 / K327, 9(b). Explain wave transfer of energy without transfer of matter.
I can compare transverse and longitudinal waves and give suitable examples.Syllabus
Syllabus K326 / K327, 9(e). Compare transverse and longitudinal waves and give suitable examples.
Make a guess. You are not marked.
A cork floats on a pond. Water waves travel across the pond from left to right. What does the cork do as the waves pass?
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It bobs up and down and stays roughly where it is.
A wave transfers energy, not the water. Each part of the water, and the cork on it, vibrates about its rest position while the pattern moves on.
A wave is a travelling disturbance that transfers energy. The material it passes through does not have to travel along with it.
An oscillation is a repeated motion about an equilibrium position. A vibrating part can move away from that position and return while passing a disturbance to its neighbours.
Follow a mark on a rope
Give one end of a stretched rope a brief up-and-down movement. A pulse travels along the rope. A small mark on the rope rises and falls as the pulse passes, then returns to its starting position.
The mark identifies the same piece of material throughout. It does not travel to the far end with the pulse. Yet the disturbance can make something at the far end move, showing that energy has been transferred.
Move the end repeatedly and a train of waves is produced. Each part oscillates about its local position as the pattern travels. This is what it means for a wave to transfer energy without transferring matter along with the disturbance. An independent bulk flow, such as a water current, is a separate effect.
A travelling disturbance and a local vibration
Green arrows show wave travel. Blue double arrows show the directions of local oscillation, not the instantaneous velocity at a turning point. Orange marks the same material point in each pair.
Transverse pulse on a rope
Longitudinal pulse in a spring
Compare transverse and longitudinal motion
- Transverse wave
- The material vibrates perpendicular to the direction of wave travel. A wave travelling horizontally along a rope while its material moves up and down is an example. A spring can also carry a transverse disturbance if its end is moved sideways relative to its length.
- Longitudinal wave
- The material vibrates parallel to the direction of wave travel. Push and pull the end of a stretched spring along its length: close and wide coil spacings travel along it while a marked coil moves to and fro locally. Sound in air is another example.
The spring's close-spaced region is a compression; its more widely spaced region is a rarefaction. Those regions travel, but a particular coil does not stay in a compression and travel all the way along the spring.
Worked classification
Two disturbances travel to the right
In the first, marked points move up and down. Their vibration is perpendicular to the rightward travel, so the wave is transverse.
In the second, marked points move left and right. Their vibration is parallel to the rightward travel, so the wave is longitudinal. Calling a wave "horizontal" is not enough: both patterns travel horizontally in these examples.
Wavefronts in a ripple tank
A ripple tank is a shallow transparent tank in which disturbances on the water surface can be observed. A vibrating straight dipper can produce approximately straight wavefronts. A small point source can produce circular wavefronts spreading outwards.
A wavefront joins points at the same stage of oscillation, such as points along one crest. In the uniform region shown, the direction of wave travel is perpendicular to the local wavefront. Straight fronts travel across the tank; circular fronts spread radially away from the source.
Ripple-tank wavefronts, seen from above
Each green line joins crests at one instant. Arrows show travel perpendicular to the local front in the uniform region shown. The lines are not paths of water particles.
A straight dipper gives straight fronts
A point source gives circular fronts
Water surface patterns help show wavefronts and crest spacing. The rope is the simpler model for purely up-and-down transverse motion; real water-particle motion need not be an exactly vertical line.
Separate observation from explanation
Watch a marked point on a rope or spring as the disturbance passes, and compare its position before and afterwards. Describe that local motion separately from the changing position of a crest or compression. In a ripple tank, observe successive fronts and their spacing; the front itself is a pattern rather than a permanent set of particles.
Compare two directions. Transverse and longitudinal describe vibration relative to propagation. They do not mean that the material traces the whole drawn wave shape or travels with the crest.
Check your understanding
A pulse travels to the right along a rope. A small mark on the rope rises and falls, then returns to its starting position. What has travelled along the rope?
Show the answer
The disturbance and energy have travelled, while the marked material has moved locally.
The wave transfers energy along the rope. Its material oscillates about local equilibrium positions; it does not need to travel with the pulse. Here that local motion is perpendicular to the rightward propagation.