Analyzing the Setup
Imagine you are standing on the edge of a quiet swimming pool. Deep below the surface, an underwater speaker is playing a pure tone of frequency 600 Hz. As the sound waves travel upwards, they cross the boundary between water and air, eventually reaching your ears.
We are given the following physical parameters:
- Frequency of the source in water: f=600 Hz
- Speed of sound in water: vwater=1500 m/s
- Speed of sound in air: vair=300 m/s
Our goal is to determine the frequency of the sound wave recorded by you, the observer standing in the air.
The Master Principle
Source vs. Medium
To solve this problem, we must understand a fundamental truth of wave mechanics: frequency is a characteristic of the source, not the medium.
When a wave is generated, the source vibrates at a specific rate. For our speaker, it pushes the surrounding water molecules back and forth exactly 600 times every second. These water molecules then push the adjacent molecules, propagating the wave outward.
When the wave reaches the water-air interface, the water molecules at the boundary vibrate at 600 Hz and force the adjacent air molecules to vibrate at the exact same rate. The air molecules have no choice but to oscillate at the frequency of the driving force.
Therefore, as a wave transitions from one medium to another, its frequency remains absolutely constant:
What Actually Changes? Wavelength and Speed
While the frequency remains unchanged, the speed of the wave is determined strictly by the properties of the medium (such as elasticity and density). Since sound travels much slower in air (300 m/s) than in water (1500 m/s), the wave must slow down.
To maintain the fundamental wave relationship:
the wavelength λ must adjust proportionally to the change in speed.
Let's calculate the wavelength in both media to see this beautiful symmetry.
In water:
λwater=fvwater=600 Hz1500 m/s=2.5 m
In air:
λair=fvair=600 Hz300 m/s=0.5 m
Notice that as the wave enters the air, its speed decreases by a factor of 5 (from 1500 m/s to 300 m/s), and consequently, its wavelength also shrinks by a factor of 5 (from 2.5 m to 0.5 m).
This perfect scaling ensures that the frequency—the number of wave crests passing a point per second—remains exactly 600 Hz.
Final Conclusion
Since the frequency of the sound wave does not change when crossing the boundary, the observer in the air hears the exact same frequency as emitted by the source.
Recorded Frequency=600 Hz
Thus, the correct option is (d).