• Relate awave’s speed to the medium in
which the wave travels.
• Describe how waves are reflected and
refracted at boundaries between media.
• Apply the principle of superposition to
the phenomenon of interference
12.
Waves transport energyby
oscillating a medium’s particles
without moving the medium
itself. From the echo of a shout
against a canyon wall to the
colorful rainbow arching
overhead, wave behaviors—
speed changes, reflections,
refractions, and interference—
shape much of what we observe.
INTRODUCTION
13.
In this module,we explore how
medium properties govern wave
speed, how waves interact at
boundaries (fixed, free, or “no‐end”),
how overlapping waves combine,
and how one‐ and two‐dimensional
waves reveal patterns like standing
waves and ripple‐tank phenomena.
Each section builds deep conceptual
understanding alongside practical,
classroom‐ready examples and
problem solving.
INTRODUCTION
14.
Medium
A material—solid, liquid,or
gas—whose constituent
particles transmit mechanical
disturbances by oscillating
around equilibrium positions.
Examples include air for
sound waves, water for
surface ripples, and metal
strings in instruments.
DEFINITION OF TERMS
15.
Boundary Condition
Constraints atan interface or
end of a medium,
determining wave
displacement and phase
upon reflection or
transmission. Fixed ends
enforce zero displacement;
free ends allow maximal
motion.
DEFINITION OF TERMS
16.
Incident Wave (Pulse)
Theportion of a wave
train or single
disturbance traveling
toward a boundary before
any reflection or
transmission occurs.
DEFINITION OF TERMS
17.
Reflected Wave (Pulse)
Theportion of an incident
wave that reverses
direction upon meeting a
boundary, possibly
inverted (phase‐shifted
by 180°) or upright,
depending on boundary
mobility.
DEFINITION OF TERMS
18.
Transmitted Wave (Pulse)
Thepart of the incident
disturbance that
continues into the second
medium, maintaining
original frequency but
adopting the new
medium’s speed and
wavelength.
DEFINITION OF TERMS
19.
Superposition
The principle thatwhen two or
more waves occupy the same
region, the net displacement at a
point is the algebraic sum of
individual displacements. The
principle that overlapping waves
combine their displacements
algebraically at each point:
𝑦total = 𝑦1 + 𝑦2 + …
DEFINITION OF TERMS
Diffraction
The bending and
spreadingof waves
around obstacles or
through openings, most
pronounced when
obstacle dimensions are
comparable to the
wavelength.
DEFINITION OF TERMS
22.
Refraction
The change indirection
and wavelength of a
wave as it crosses
obliquely from one
medium into another
with different
propagation speed,
governed by Snell’s law.
DEFINITION OF TERMS
23.
Standing Wave (Stationary
Wave)
Apattern formed by two
waves of identical frequency
and amplitude traveling in
opposite directions, yielding
fixed nodes (zero
displacement) and antinodes
(maximum displacement).
DEFINITION OF TERMS
24.
Node
A point ina standing
wave where the net
displacement is
always zero due to
perfect destructive
interference.
DEFINITION OF TERMS
25.
1.1 Dependence onAir Temperature
Sound speed in dry air increases approximately
linearly with temperature because warmer air
molecules transmit pressure variations more
rapidly. An empirical relation valid near atmospheric
pressure is:
SPEED OF SOUND WAVES
Mechanical impedance—rooted indensity and elasticity—dictates
wave speed across materials. Stiffer and less compressible media
conduct sound faster.
DEPENDENCE ON MEDIUM
When the incidentpulse reaches
a boundary, two things occur:
• A portion of the energy carried
by the pulse is reflected and
returns towards the left end of
the rope (reflected pulse).
• A portion of the energy carried
by the pulse is transmitted to
the wall
WAVE INTERACTION WITH BOUNDARY
35.
• Constraint: Endheld
immobile (e.g., rope tied
to a rigid wall).
• Reflection: Pulse inverts
(180° phase shift)
because displacement at
boundary must be zero.
• Speed & Wavelength:
Remain equal to incident
values.
FIXED END
36.
• Reflected waveis
inverted with the
incident wave
• Speed is the same
• Wavelength is the
same
• Reflected wave’s
amplitude is lesser
FIXED END
37.
• Constraint: Endcan move
freely (e.g., rope over
frictionless ring).
• Reflection: Pulse remains
upright (no phase shift)
as boundary
displacement maximizes.
• Speed & Wavelength:
Unchanged from
incident.
FREE END
38.
• Reflected waveis in
phase with the
incident wave
• Speed is the same
• Wavelength is the
same
• Reflected wave’s
amplitude is lesser
FREE END
• Constraint: Mediumextends
indefinitely or terminates in
energy absorber (e.g., water
waves on a sandy beach).
• Reflection: None—incident
energy either continues or
dissipates.
• Illustration: Rope end
dipped in viscous fluid
shows pulse disappearing
without echo.
NO END
• Waves willreact differently with varying linear densities of
the strings.
WAVES IN VARYING DENSITY
43.
• The transmittedpulse is
traveling slower than the
reflected pulse.
• The transmitted pulse has a
smaller wavelength than the
reflected pulse.
• The speed and the
wavelength of the reflected
pulse are the same as the
speed and the wavelength of
the incident pulse
WAVES IN VARYING DENSITY
44.
• Waves willreact differently with varying linear densities of
the strings.
WAVES IN VARYING DENSITY
45.
• The transmittedpulse is
traveling faster than the
reflected pulse.
• The transmitted pulse has a
larger wavelength than the
reflected pulse.
• The speed and the wavelength
of the reflected pulse are the
same as the speed and the
wavelength of the incident
pulse
WAVES IN VARYING DENSITY
46.
As a pulsetravels from medium 1
into medium 2:
• Incident Pulse approaches the
boundary.
• Reflected Pulse returns into
medium 1 with reduced
amplitude.
• Transmitted Pulse continues
into medium 2 at speed 𝑣2 and
wavelength 𝜆2, sharing the
incident frequency 𝑓 .
INCIDENT, REFLECTED, AND TRANSMITTED PULSES
What happens whentwo waves
meet while they travel through
the same medium?
SUPERPOSITION AND INTERFERENCE
51.
INTERFERENCE
• It isa phenomenon that occurs when two waves
meet while traveling along the same medium
52.
PRINCIPLE OF SUPERPOSITION
•When multiple waves coexist in a medium, they do not
collide; rather, their displacements add algebraically at
each point:
53.
PRINCIPLE OF SUPERPOSITION
•It states that the disturbance in a
medium caused by two or more
waves is the algebraic sum of the
displacements produced by the
individual waves.
• Waves can combine to form a new
wave
• Waves moving in opposite
directions can cancel or form a new
wave of lesser or greater amplitude.
• This principle underpins all
interference phenomena.
CONSTRUCTIVE INTERFERENCE
• In‐phasewaves ( 0 °
difference) reinforce, yielding a
resultant amplitude 𝐴res = 𝐴1 +
𝐴2 .
• Two interfering waves have a
displacement in the same
direction.
• The amplitude of the resulting
wave is equal to the sum of
the individual amplitudes
56.
CONSTRUCTIVE INTERFERENCE
• In‐phasewaves ( 0 ° difference)
reinforce, yielding a resultant
amplitude 𝐴res = 𝐴1 + 𝐴2 .
• Two interfering waves have a
displacement in the same
direction.
• The amplitude of the resulting
wave is equal to the sum of the
individual amplitudes
• Waves pass each other.
57.
CONSTRUCTIVE INTERFERENCE
Scenario 1:Same Phase, Unequal Amplitudes
• Description: Two waves are in phase, meaning their crests and
troughs align perfectly. But one wave has a larger amplitude
than the other.
• Result: The amplitudes add together, so the resultant wave has
a larger amplitude than either wave individually.
• Type of Interference: Constructive interference—even though
the amplitudes are unequal, the waves reinforce each other.
• Nickname: You could call this partial constructive interference,
but it's still fundamentally constructive.
58.
DESTRUCTIVE INTERFERENCE
• Out‐of‐phasewaves ( 180 °
difference) cancel, potentially
producing zero net displacement.
• The two interfering waves have a
displacement in the opposite
direction
• When waves overlap, the effect of
one of the pulses on the
displacement of a given particle of
the medium is destroyed or canceled
by the effect of the other pulse.
• Only a momentary condition-waves
pass each other
59.
DESTRUCTIVE INTERFERENCE
• Out‐of‐phasewaves ( 180 °
difference) cancel, potentially
producing zero net displacement.
• The two interfering waves have a
displacement in the opposite
direction
• When waves overlap, the effect of
one of the pulses on the
displacement of a given particle of
the medium is destroyed or canceled
by the effect of the other pulse.
• Only a momentary condition-waves
pass each other
60.
DESTRUCTIVE INTERFERENCE
Scenario 2:Out of Phase, Unequal Amplitudes
• Description: The waves are out of phase (e.g., crest
meets trough), but one wave is larger than the other.
• Result: The smaller wave partially cancels the larger one,
resulting in a wave with reduced amplitude, but not zero.
• Type of Interference: Destructive interference—because
cancellation occurs, even if it's not complete.
• Nickname: This is often called partial destructive
interference or incomplete cancellation.
INSTRUCTIONS: Identify whattype of interference is asked
• G: Partial Constructive
(The waves are partially in phase,
resulting in a resultant wave with an
amplitude greater than the
individual waves but less than the
maximum possible)
• H: Partial Destructive
(The waves are partially out of
phase, resulting in a resultant wave
with a reduced amplitude)
• I: Partial Destructive
(The waves are partially out of
phase, resulting in a resultant wave
with a reduced amplitude)
65.
INSTRUCTIONS: Identify whattype of interference is asked
• J: Partial Constructive
(The waves are partially in phase,
resulting in a resultant wave with an
amplitude greater than the
individual waves but less than the
maximum possible)
• K: Partial Destructive
(Similar to 'I', the waves are partially
out of phase, leading to partial
cancellation)
• L: Partial Destructive
(Similar to 'I', the waves are partially
out of phase, leading to partial
cancellation)
66.
INSTRUCTIONS: Identify whattype of interference is asked
• M: Partial Constructive
(The waves are partially in phase,
resulting in a resultant wave with an
amplitude greater than the individual
waves but less than the maximum
possible)
• N: Partial Constructive
(The waves are partially in phase,
resulting in a resultant wave with an
amplitude greater than the individual
waves but less than the maximum
possible)
• O: Partial Destructive
(Similar to 'I', the waves are partially out
of phase, leading to partial cancellation)
67.
STANDING WAVES (STATIONARYWAVES)
• A combination of two waves
moving in opposite directions,
each having the same
amplitude and frequency.
• Result of interference
• Standing wave pattern - points
that appear to be standing still
• Only created within the
medium at specific
frequencies (harmonics) of
vibration
68.
STANDING WAVES (STATIONARYWAVES)
A standing wave emerges
from two identical waves
traveling oppositely. Nodes
(zero displacement) form at
fixed points; antinodes
(maximum displacement) lie
midway. Only discrete
frequencies (harmonics)
satisfy boundary constraints
on a string of length 𝐿 fixed at
both ends:
WAVES IN ONEDIMENSION
One‐dimensional waves—
such as pulses on a
rope—confine oscillations
along a single axis.
Analysis tracks
displacement vs. position
and time, ideal for
illustrating boundary
reflections and standing
modes.
72.
REFLECTION IN ONEDIMENSION
• When a wave
encounters a barrier,
like with 1-D waves,
it is reflected.
• When a straight wave
encounters a straight
barrier head on, it is
reflected back on the
original path.
73.
REFLECTION IN TWODIMENSION
• The wave pulse moves
toward a rigid barrier that
reflects the wave: the
incident wave moves
forward, and the reflected
wave moves to the right.
• The law of reflection states
that the angle of incidence is
equal to the angle of
reflection.
74.
WAVES IN TWODIMENSION
Surface waves on water spread in
two axes. Visualizing these
requires:
• Wave Front: Curve connecting
points oscillating in phase,
often drawn as concentric
circles around a source.
• Ray: Line perpendicular to wave
fronts indicating energy
propagation direction.
75.
WAVES IN TWODIMENSION
• Example: Ripples on the surface
of water.
• Behavior: The wave spreads out
in a plane—both x and y
directions—forming circular
wavefronts.
• Real-world analogy: Dropping a
pebble into a pond and
watching the ripples expand
outward.
REFLECTION IN TWODIMENSION
• The wave pulse moves
toward a rigid barrier that
reflects the wave: the
incident wave moves
forward, and the reflected
wave moves to the right.
• The law of reflection states
that the angle of incidence is
equal to the angle of
reflection.
80.
REFLECTION IN TWODIMENSION
• When a straight wave
front meets a straight
barrier: Incident and
reflected rays make
equal angles with the
normal (perpendicular
to barrier). Law of
Reflection: 𝜃 𝑖 = 𝜃 𝑟 .
81.
REFLECTION IN TWODIMENSION
• The incident wave is represented by an
arrow pointing upward. The ray of the
reflected wave points to the right. The
barrier is represented by a line. The line
which drawn at a right angle, or
perpendicular, to the barrier is called
the NORMAL LINE.
• The Angle between the normal line and
the reflected ray is called the angle of
reflection. The law of reflection states
that “THE ANGLE OF INCIDENCE IS
EQUAL TO THE ANGLE OF
REFLECTION”
82.
REFRACTION IN TWODIMENSION
• When the waves move from deep to
shallow water, their speed decreases,
and the direction of the waves changes.
• Because the waves in the deep water
generate the waves in the shallow
water, their frequency is not changed.
• Based on the decrease f in the
speed of the waves means that the
wavelength is shorter in the shallower
water.
REFLECTION AND REFRACTIONFACTS
• Do you know that echoes are
caused by the reflection of
sound off hard surfaces, like
the walls of a large warehouse
or a distant rock face?
• RAINBOWS are created when
white light passes through a
raindrop; refraction separates
the light into its colors.