Superposition Of Waves
Each particle executes the same type of vibration.
Particles at the mean position perform SHM.
Have e same amplitude, period, and frequency.
The state of vibration of a particle (phase) changes from one period to another.
V = 0 at extreme position.
The particle attains the maximum velocity after passing through the mean position.
Progressive wave 2 types -
Transverse Wave
Longitudinal Wave
Transverse Wave
Vibrations of particles are perpendicular to the direction of propagation of the wave. Produces crests and troughs.
Can propagate through solids.
Longitudinal Wave
Vibrations of particles produce compressions and rarefaction along the wave’s propagation direction.
Can propagate through solids and fluids.
Positive x-direction
y(x,t)=A sin(kx - wt)
Negative x-direction
y(x,t)=A sin(kx + wt)
y = A sin(wt - kx)
y = A sin [wt - (2π/λ)x]
y = A sin 2π(nt - x/λ)
y = A sin 2πn (t - x/v)
y = A sin 2π/λ (vt - x)
y = A sin 2π(t/T - x/λ)
If the simple harmonic progressive wave is given by
y = A sin (wt - kx)
then,
Particle velocity,
dy/dt = wA cos (wt - kx)
Wave speed,
v = w/k
The phenomenon in which a part of the wave is returned to the original medium with the reduction in its energy and hence in intensity and amplitude is called reflection of waves.
A denser medium
The crest is reflected as a trough
The phase change of 180° or π radians, when transverse waves are reflected from a denser medium
A rarer medium
The crest is reflected as the crest and vice-versa with a reduction in amplitude.
No change in phase angle.
A denser medium
To return to normal condition, the particle begins to press in opposite direction, therefore compression gets reflected as compression and vice-versa.
Displacement in reflected is opposite to displacement of the incident wave, therefore phase angle is 180° or π radians.
A rarer medium
Each particle executes the same type of vibration.
Particles at the mean position perform SHM.
Have e same amplitude, period, and frequency.
The state of vibration of a particle (phase) changes from one period to another.
V = 0 at extreme position.
The particle attains the maximum velocity after passing through the mean position.
Progressive wave 2 types -
Transverse Wave
Longitudinal Wave
Transverse Wave
Vibrations of particles are perpendicular to the direction of propagation of the wave. Produces crests and troughs.
Can propagate through solids.
Longitudinal Wave
Vibrations of particles produce compressions and rarefaction along the wave’s propagation direction.
Can propagate through solids and fluids.
Positive x-direction
y(x,t)=A sin(kx - wt)
Negative x-direction
y(x,t)=A sin(kx + wt)
y = A sin(wt - kx)
y = A sin [wt - (2π/λ)x]
y = A sin 2π(nt - x/λ)
y = A sin 2πn (t - x/v)
y = A sin 2π/λ (vt - x)
y = A sin 2π(t/T - x/λ)
If the simple harmonic progressive wave is given by
y = A sin (wt - kx)
then,
Particle velocity,
dy/dt = wA cos (wt - kx)
Wave speed,
v = w/k
The phenomenon in which a part of the wave is returned to the original medium with the reduction in its energy and hence in intensity and amplitude is called reflection of waves.
A denser medium
The crest is reflected as a trough
The phase change of 180° or π radians, when transverse waves are reflected from a denser medium
A rarer medium
The crest is reflected as the crest and vice-versa with a reduction in amplitude.
No change in phase angle.
A denser medium
To return to normal condition, the particle begins to press in opposite direction, therefore compression gets reflected as compression and vice-versa.
Displacement in reflected is opposite to displacement of the incident wave, therefore phase angle is 180° or π radians.
A rarer medium