This chapter covers fundamental concepts of vibrations and waves, including:
Vibrations of a Pendulum
Wave Description
Wave Speed
Transverse Waves
Longitudinal Waves
Wave Interference
Standing Waves
Doppler Effect
Bow Waves
Shock Waves
A vibration is a periodic wiggle in time.
A wave is a periodic wiggle in both space and time, extending from one place to another.
Examples of waves:
Electromagnetic Waves: Light (needs no medium)
Mechanical Waves: Sound (requires a medium)
Vibration: Wiggle in time
Wave: Wiggle in space and time
A simple pendulum consists of a stone suspended at the end of a string.
The pendulum's swing rate:
Depends only on the length of the pendulum.
Mass does not affect the swing rate (similar to mass not affecting ball fall rate).
Period: The duration of one complete to-and-fro swing.
Longer pendulum length = longer period (similar to free-fall duration).
If a 1-meter-long pendulum (1 kg) changes its bob to a mass of 2 kg, the period:
Remains the same; period depends on the length, not mass.
If the bob lengthens to 2 meters, the period:
Increases with increasing length.
Waves can be visually represented using a sine curve:
This is created by tracing the path of a swinging pendulum with sand that drops onto paper.
A marking pen also illustrates sine curves with vertical movement traced over horizontal time.
Crests: High points of the wave.
Troughs: Low points of the wave.
Amplitude: Distance from the midpoint to the crest or trough.
Wavelength: Distance between successive crests or troughs.
Frequency: How frequently a vibration occurs, measured in Hertz (Hz).
1 Hz = 1 vibration/second.
Mechanical vibrations: a few Hz.
Sound frequencies: a few hundred to thousand Hz.
Radio waves: up to millions Hz (MHz).
Cell phones: billions Hz (GHz).
Period (T): Time to complete one vibration, inversely related to frequency.
Example: 2 Hz frequency corresponds to a 0.5 second period.
Wave Motion: Waves transport energy without transporting matter.
When a stone is dropped in water, ripples travel without moving water across the pond.
Wave Speed: Distance traveled by waves, determined by frequency and wavelength.
Example: Wave speed formula: speed = frequency × wavelength.
Transverse Waves: Medium vibrates perpendicularly to the direction of energy transfer (side-to-side).
Examples: Vibrations of musical instrument strings, light waves, transverse seismic waves (S-waves).
Longitudinal Waves: Medium vibrates parallel to the energy transfer direction (back-and-forth).
Composed of compressions and rarefactions.
Examples: Sound waves, longitudinal seismic waves (P-waves).
Wave Interference: The interaction of waves when they meet, can cause:
Constructive Interference: Amplitudes add, creating a wave of increased amplitude.
Destructive Interference: Crest of one wave overlaps the trough of another, reducing overall amplitude.
Standing Waves: Created when waves are reflected back, forming a pattern with stationary nodes (minimal displacement) and antinodes (maximal displacement).
Examples: Waves in strings, sound waves in instruments.
Describes frequency changes in waves due to motion:
Sound Waves: A pitch increase as the source approaches, decrease as it moves away.
Light Waves: Blue shift (increase) as a light source approaches; red shift (decrease) as it recedes.
Bow Waves: Occur when waves superimpose to create a barrier when objects travel faster than the wave speed.
Shock Waves: Formed by objects traveling faster than sound, resulting in overlapping spherical patterns that create a cone. This generates sonic booms from supersonic aircraft.