GCSE Physics - Intro to Waves - Longitudinal and Transverse Waves #61
Basics of Waves
Waves transfer energy from one place to another without transferring matter.
Example: Light waves from a phone screen to your eye, sound waves from speakers to your ear.
Energy can represent meaningful information, such as images and tunes.
Wave Properties
Waves oscillate or vibrate as they travel.
Displacement-distance graph shows:
Distance: how far the wave has traveled.
Displacement: how far the wave moves from its equilibrium point (up or down).
Amplitude: maximum displacement from equilibrium.
Wavelength: distance of one entire oscillation (crest to crest or trough to trough).
Crest: top of the wave; Trough: bottom of the wave.
Displacement-Time Graph
Shows time on the x-axis:
One complete oscillation is measured as the time period.
Time Period: time taken for one complete oscillation.
Frequency (in hertz): number of complete oscillations per second.
Frequency Calculation
Frequency (f) can be calculated using:
f = 1 / Time Period
Example: If the time period is 0.5 seconds, frequency is f = 1 / 0.5 = 2 Hz.
Wave Speed Calculation
Wave Speed (v) is calculated by:
v = Wavelength (λ) x Frequency (f).
Example:**
Sound wave with frequency of 400 Hz and wavelength of 70 cm (0.7 m):
Wave Speed = 0.7 m x 400 Hz = 280 m/s.
Types of Waves
Transverse Waves
Oscillations are perpendicular to the direction of energy transfer:
Example: Light waves, radio waves, water waves, waves on a string (e.g., guitar).
Longitudinal Waves
Oscillations are parallel to the direction of energy transfer:
Regions of compression (more dense) and rarefaction (less dense).
Example: Sound waves, seismic P-waves.
Conclusion
Understanding these fundamentals will help in grasping more complex wave behaviors.