transverse wave = waves that oscillate perpendicular to the direction of energy transfer
longitudinal wave = a wave that oscillates parallel to the direction of energy transfer
Secondary waves (S-waves) are shear waves that are transverse in nature. Following an earthquake event, S-waves arrive at seismographstations after the faster-moving P-waves and displace the ground perpendicular to the direction of propagation.
seismic waves = waves that travel through the earth and are caused by earthquakes
examples of longitudinal waves = ultrasound, p waves and sound waves,
example of transverse waves = ripples on surface water, vibration in guitar strings, S waves and electromagnetic waves
compression = regions of high pressure due to particles being close together
rarefactions = regions of low pressure due to particles being spread further apart
demonstrated by :
longitudinal - pushing and pulling a slinky
transverse - moving a rope up and down rapidly
waves transfer energy and information, not matter
wave amplitude = max displacement of point on wave from undisturbed position
wave length = distance from point on wave to same position on adjacent wave. commonly peaks - peak or trough - trough
frequency wave is no. waves which pass a given point each second
frequency = hertz (Hz)
wave speed
speed at which energy is transferred through medium
wave velocity
equal to product of wavelength and frequency of the wave
wave speed = frequency x wave length
period of wave
length of time it takes for one full wave to pass through a point
normal (reflection/refraction)
vertical imaginary line which is perpendicular to the boundary
when light reflects off a boundary it bounces off the smooth flat surface creating the angle of incidence (angle entering)which is the same as the angle of reflection (angle leaving)
refraction
change in speed of wave, it reached boundary between two media, usually resulting in change of direction
when light refracted at boundary :
light changes speed in new medium
if new medium more dense, light travels slower and bend towards normal
if new medium less dense, light will travel faster and bend away from normal
sound wave particles travel through solids by vibrating and transferring kinetic energy through the material
how human ear works :
outer ear collects sound which travels to ear
sound wave causes eardrum to vibrate at same frequency
this is amplifies by 3 ossicles by small bones in ear
caused the hair in cochlea to vibrate
cochlea converts the vibration into electrical signals which are passed to brain through auditory nerves
brain converts electrical signals into sound
human hearing frequency range = 20Hz - 20kHz
ultrasound wave = 20, 000 Hz
infrasound = 20Hz
seismic waves produced by eathquakes, makes P waves (longitudinal) and S waves (transverse)
P waves travel through both solids and liquids
S waves only travel through solids
P waves prove/ are evidence that the earth's core is liquid. The waves are detected on the other side indicating they're able to travel through the liquid within the earth's core
detecting objects in deep water by using echo sound
high frequency sound waves are emitted, reflected and detected
time difference between emissions, detections and wave speed used to calculate distance of water depth
sonar :
ultrasound waves emitted, reflect boundary and their echo is detected
speed of ultrasound known and also time it takes to detect the echoes
distance = speed x time
distance travelled is halved to give distance between emitter and boundary (wave has to travel there and back)
foetal scanning :
ultrasound wave sent into body, passes through it and reflects off organs and tissues
device uses reflected ultrasound waves to product image of the foetus