Wave Properties Flashcards
Wave Basics
Energy Transfer
- Waves transfer energy from one place to another without transferring matter.
- Example: Light waves from a phone screen to the eye, sound waves from speakers to the ear.
- Energy can be interpreted as meaningful information by the brain to build up images and tunes.
Wave Properties
- Waves vibrate or oscillate as they travel.
- Displacement-Distance Graph:
- Distance: How far the wave has traveled from the starting point.
- Displacement: How far from the equilibrium point the wave has oscillated (up or down).
- Amplitude: The maximum displacement from the equilibrium point.
- Wavelength: The distance of one complete oscillation.
- Can be measured from equilibrium, up, down, and back up.
- Also measured from crest to crest (or trough to trough).
- Crest: The very top of a wave.
- Trough: The opposite of the crest (the very bottom of a wave).
Displacement-Time Graph
- X-axis represents time instead of distance.
- The length of one complete oscillation represents the time period (T).
- Time Period (T): The time it takes for one complete oscillation.
- Frequency (f): The number of complete oscillations per second, measured in Hertz (Hz).
- f = \frac{1}{T}
- T = \frac{1}{f}
- Example:
- If each oscillation takes 0.5 seconds (T = 0.5 s), then the frequency is 2 Hz (two oscillations per second).
- If the frequency of a wave is 4 Hz, then the time period is 0.25 seconds per oscillation.
Wave Speed
- Wave speed (v) is calculated by multiplying the wavelength ((\lambda)) by the frequency (f).
- v = \lambda f
- Example: Sound wave with a frequency of 400 Hz and a wavelength of 70 cm.
- Convert 70 cm to 0.7 meters.
- v = 0.7 \, \text{m} \times 400 \, \text{Hz} = 280 \, \text{m/s}
Types of Waves
Transverse Waves
- Oscillations are perpendicular to the direction of energy transfer.
- Vibrations go up and down while the wave travels horizontally.
- Examples:
- Electromagnetic waves (light, radio waves).
- Ripples and waves in water.
- Waves on a string (e.g., guitar string).
Longitudinal Waves
- Oscillations are parallel to the direction of energy transfer.
- Leads to regions of compression and rarefaction (more spread out).
- Area of compression moves from left to right within the wave.
- Examples:
- Sound waves.
- Some types of shock waves (e.g., seismic P-waves).