Reflection of Sound & Definition of an Echo:
Like light, sound waves obey the laws of reflection: the incident wave, reflected wave, and the normal lie in the same plane, and the angle of incidence equals the angle of reflection. An echo is the distinct repetition of the original sound heard after reflection from an obstacle (such as a cliff, high wall, or mountain).
Conditions Necessary for Hearing an Echo:
- Persistence of Hearing: The sensation of sound persists in the human auditory nerve for approximately $0.1\text{ s}$ ($\frac{1}{10}\text{th}$ of a second). To be perceived as a distinct echo, the reflected sound must reach the listener at least $0.1\text{ s}$ after the original sound.
- Minimum Distance Calculation: If $d$ is the distance between source and reflector, and $v$ is the speed of sound: $$2d = v \times t \implies d = \frac{v \times t}{2}$$ At $20^\circ\text{C}$ in air, speed of sound $v \approx 340\text{ m/s}$. With $t = 0.1\text{ s}$: $$\mathbf{d_{\min} = \frac{340 \times 0.1}{2} = \frac{34}{2} = 17\text{ m}}.$$ Hence, the reflecting surface must be situated at a minimum distance of $17\text{ meters}$ from the sound source.
- Size and Texture of Reflector: The dimensions of the reflecting surface must be comparable to or larger than the acoustic wavelength. Hard rigid surfaces (granite, brick) reflect sound well; soft porous materials (curtains, foam) absorb sound.
SONAR (Sound Navigation and Ranging):
SONAR uses high-frequency ultrasonic waves ($f > 20\text{ kHz}$) to detect underwater submarines, icebergs, and measure ocean depth. Ultrasonic waves travel long distances without dispersion. If transit time to seabed and back is $t$, ocean depth is $d = \frac{v \times t}{2}$.