nature waves
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WAVES
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Describing wave motion
Term Description SI units
Amplitude, A The maximum displacement of the ropefrom the rest position
Metre (m)
Wavelength, The shortest distance between 2 successivecrests or troughs
Metre (m)
Frequency, f The number of complete waves producedper second
Hertz (Hz)
Period, T The time taken to produce one completewave
Second (s)
Wave speed, v The distance travelled by a wave in 1 second Second (s)
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Describing wave motion
trough
crest
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Types of Waves Transverse waves
The vibration of the particles in the medium is perpendicular to thedirection in which the wave travels
Eg. water waves, rope waves, all types of electromagnetic wavesincluding light waves, microwaves, X-rays, gamma rays
The highest point reached by a vibrating particle in a transverse waveis called crest or peak while the lowest point is called trough
Longitudinal waves The vibration of the particles in the medium is parallel to the direction
in which the wave travels Eg. sound waves The section in which the vibrating particles in a longitudinal wave are
closest together is called compression while the section in which thevibrating particles are furthest apart is called rarefaction
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Wavefronts Any line or surface over which all the vibrating particles
are in the same phase Particles in the same phase have the same speed and
are at equal distances from their source In transverse waves, wavefronts are normally lines joining
all the peaks at equal distance from their source The distance between successive wavefronts equals a
wavelength The direction of travel of a wave is always perpendicular
to its wavefronts as indicated by lines drawnperpendicular to the wavefronts.
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Wave Equation Velocity of wave, v = f Example: The speed of light in vacuum is 3 x 10 8 m/sCalculate the frequency of orange light, given that its
wavelength in vacuum is 6 x 107
m.
3 x 10 8 = f x 6 x 10 -7
f = (3 x 10 8)/(6 x 10 -7) = 5 x 1 014 Hz
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Reflection of waves Waves are reflected when an obstacle is placed in their
paths All reflected waves obey the law of reflection which states
The angle of reflection equals the angle of incidence The incident wave, the reflected wave, and the normal all lie on the
same plane
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Properties of reflected waves The reflected wave the same wavelength, frequency, and
speed as the incident wave The velocities of the reflected and incident waves are
different because they travel in different directions The angle of reflection equal to the angle of incidence
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Refraction of waves Waves are refracted when their speeds are changed The speed of a wave is changed when the wave moves
from a dense medium into a less dense medium or fromdeep water to shallower water
If the incident wave is travelling along the normal, it willcontinue to travel along the normal after entering water ofa different depth
In all other cases, refraction produces a change in wavedirection
On entering shallower water, the wave direction bendstowards the normal.
On entering deeper water, the wave direction bends awayfrom the normal
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Refraction of water waves
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Refraction of waves
Properties Shallower to deeperwater
Deeper to shallowerwater
Wavelength Increases Decreases
Frequency Unchanged UnchangedSpeed Increases Decreases
Velocity Increases Decreases
Direction of travel Bends away from normal Bends towards normal
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Sound Production of sound waves by vibrating sources:
sound is produced by vibrating sources (egtuning fork) placed in a medium (solid, liquid, gas)
Nature of sound waves It is a form of energy that can be transferred from one point to another It is an example of longitudinal waves consisting of compressions and
rarefactions Compressions are regions where air pressure is slightly higher than he
surrounding air pressure Rarefactions are regions where air pressure is slightly lower than the
surrounding air pressure
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Sound waves
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Range of audible frequency The range of frequency that a human ear can detect is
from 20 Hz to 20,000 Hz
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Experiments to determine speed of soundin air Pistol method
Observer A and B are positioned at a distance s apart and with ameasuring tape, measure and record s. (must be more than 1km)
A fires a starting pistol
B starts the stopwatch on seeing the flash of the pistol and stops thestopwatch when he hears the sound
The time t, is recorded The speed of sound v can be calculated by
Speed = distance / time
For better accuracy, the experiment should be repeated and theaverage speed of sound can be calculated.
The experiment can be repeated by interchanging the positions ofA and B so as to minimise the effect of the wind direction.
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Experiments to determine speed of soundin air Echo method
Observer A and B are positioned at a distance s from the wall and with ameasuring tape, measure and record s
A claps two wooden blocks.
On hearing the echo (reflected from the wall), he repeats the clap B starts the stopwatch and also starts counting from zero till the nth clap. The time interval t n is recorded The average time between successive claps is t = t n/n The speed of sound v can be calculated by
speed = distance/time
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Reflection of sound An echo is a reflection of sound Reverberation is the effect of a prolonged sound due to
the merging of many echoes
Echoes are used in determining the depth of sea andlocations of shoals of fish