Physics Bk3B Unit 6 Answer
Transcript of Physics Bk3B Unit 6 Answer
3B Wave Motion II Chapter 6 Wave Phenomena
6 Wave Phenomena
Practice 6.1 (p. 48)1 D
2 D
3
4 (a) The wave speed remains to be 3 cm s1.
(b) By v = f, when the frequency is
doubled and the speed remains
unchanged, the wavelength is halved.
Therefore the new wavelength is 1 cm
and the new wavefronts are as shown.
5 Wave troughs are shown on the screen as
dark lines.
Wave crests are shown on the screen as
bright lines.
6 (a) The wavelength of the wave is 2 cm.
(b) The frequency of the wave is 10 Hz.
Speed of water waves
= f = 10 2 = 20 cm s1
(c) Increasing the frequency does not
change the wave speed, so the new
speed is 20 cm s1.
By v = f, when the frequency is
doubled and the speed remains
unchanged, the wavelength is halved.
Therefore the new wavelength is 1 cm.
7 (a) Wavelength = = 1 cm
(b) Speed =
= = 2 cm s1
(c) By v = f,
frequency = = = 2 Hz
(d) Reduce the speed of the vibrator by half.
Practice 6.2 (p. 57)1 D
2 B
3 D
4
+ 65 + 90 = 180
= 25
= 90 = 90 = = 25
5 =
=
deep = 6 cm
The wavelength in the deep region is 6 cm.
6 By nXY = ,
speed in region X = vY nXY
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3B Wave Motion II Chapter 6 Wave Phenomena
= 4 1.25
= 5 cm s1
7
8
9
10 (a)
In region A In region B
Frequency 12 Hz 12 Hz
Wavelength 2 cm 1.5 cm
Wave speed 24 cm s1 18 cm s1
(b) Region A is deeper.
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11
12 (a)
(b) Wave speed in the deep region
= f = 2 3 = 6 cm s1
(c) (i) The speed of the waves in the
shallow region is 3 cm s1.
(ii) By v = f,
wavelength = = = 1.5 cm
13 (a) Region B is deeper.
(b) By = ,
wavelength in region A
= B = = 1 cm
(c)
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3B Wave Motion II Chapter 6 Wave Phenomena
(d) Refractive index from A to B
= = = 0.667
Practice 6.3 (p. 64)1 D
2 C
3 A
4 (a) Diffraction of waves is the spreading of
waves around the edge into the shadow
of an obstacle without a change in
speed.
(b)
5 (a)
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3B Wave Motion II Chapter 6 Wave Phenomena
(b) Diffraction
(c)
6 (a)
(b) No, I do not agree with the company.
This is because ocean waves diffract
into the bay, so that the water in the bay
may not be calm enough for the sports.
7 (a) This design provides an entrance for the
ships and at the same time reduces the
amount of waves entering the typhoon
shelter.
(b) I do not agree with him.
If breakwaters are built as in Figure d,
water waves would diffract through the
opening and travel into the typhoon
shelter.
Practice 6.4 (p. 76)1 D
2 A
3 D
4 B
5 (a) & (b)
(P can be any point on the antinodal
lines labelled by A(P).)
(Q can be any point on the nodal lines
labelled by N(Q).)
(c) Move the sources further apart. /
Decrease the wavelength of waves.
6 (a) Waves are arriving in phase at point P
but in antiphase at point Q.
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(b) Path difference at point P
= YP – XP
= 3.5 – 2.5
=
= 2 cm
Path difference at point Q
= XQ – YQ
= 3.5 – 3
= 0.5
= 1 cm
(c) Constructive interference happens at
point P.
Destructive interference happens at
point Q.
7 (a) By v = f,
wavelength = = = 2 cm
(b) Path difference at point A
= QA – PA
= 66 – 60
= 6 cm
(c) Path difference at point A = 6 cm = 3
Constructive interference will be
observed at point A.
8 (a) Destructive interference
(b) Constructive interference takes place at
positions where the path difference
equals , where n = 0, 1, 2...
Destructive interference takes place at
positions where the path difference
equals n, where n = 0, 1, 2...
9 (a) (i)
(ii)
(b) When t = 2 s, P, Q and R are
momentarily at rest.
Practice 6.5 (p. 88)1 C
2 A
3 D
4 B
5 B
Wavelength = = 0.4 m
Wave speed = f = 50 0.4 = 20 m s1
6 (a) Wavelength = 70 2 = 140 cm
(b) Holding the racquet at point A can
reduce the vibrations felt by the hand.
This is because the amplitude of
vibration at point A is smaller than that
at point B.
7 (a) A travelling wave carries and transmits
energy from one place to another. On
the contrary, energy in a stationary
wave is localized.
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3B Wave Motion II Chapter 6 Wave Phenomena
(b) Both of them do not transfer matter. 8 (a)
(b)
9 (a) They are all momentarily at rest.
(b) (i) Particles B and C are vibrating in
phase.
(ii) Particles B and C are vibrating in
antiphase with particle D.
Revision exercise 6Multiple-choice (p. 93)1 B
By = ,
vshallow = vdeep
= 12
= 8 cm s1
2 B
3 D
4 B
5 C
6 D
(2):
By v = f,
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3B Wave Motion II Chapter 6 Wave Phenomena
wavelength = = = 0.02 m = 2 cm Path difference at P = 6 4 = 2 cm =
Constructive interference occurs at P.
7 C
8 D
9 C
At the mid-point between X and Y, the path
difference is 0 and constructive interference
takes place.
Then consider the left side of the mid-point.
Let the path difference be .
Constructive interference takes place when
= n = 3n
Also, XY = 17 cm
3n = 17
n 5.67
Therefore, the number of points of
constructive interference on the left side of
the mid-point is 5.
By symmetry, there are also 5 points of
constructive interference on the right side of
the mid-point.
total number of points of constructive
interference = 5 + 1 + 5 = 11
10 C
11 D
12 C
13 (HKCEE 2004 Paper II Q25)
14 (HKCEE 2005 Paper II Q36)
15 (HKALE 2005 Paper II Q29)
16 A
17 (HKALE 2006 Paper II Q7)
18 C
Wavelength = 2 0.60 = 1.20 m
Speed = f = 300 1.20 = 360 m s1
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Conventional (p. 96)1 (12 0.5 A)
Wave
speedWavelength
Direction
of travel
Reflection no change no change change
Refraction change change
change / no
change (at
i = 0)
Diffraction no change no change change
Interference no change no change no change
2 (Correct reflected pulse drawn) (3 1A)
(a)
(b)
(c)
3 (a) Largest possible wavelength
= 2L = 2 10 = 20 m (1A)
(b) Wave speed = f (1M)
= 4 20
= 80 m s1 (1A)
(c) A stationary wave could be produced.
(1A)
Wave speed of the new stationary wave
= 80 m s1 (1A)
By v = f,
wavelength of the new stationary wave
= = = 10 m (1A)
4
(Axes with correct labels) (1A)
(Correct amplitude) (1A)
(Correct period) (1A)
(Correct shape) (1A)
5 (a)
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(Decreasing wavelength) (1A)
(Correct change in amplitude) (1A)
(b) Refraction (1A)
(c) The sloped edge of the ripple tank can
reduce reflection of waves. (1A)
(d) Using spongy edge can also achieve the
purpose mentioned in (c). (1A)
6 (a)
(Shorter wavelength) (1A)
(Less bending) (1A)
(b)
(Shorter wavelength in region A than
that in Figure e) (1A)
(Less bending) (1A)
(Shorter wavelength in region B than in
region A) (1A)
7 (a) Wavelength of waves in region A
= = 0.04 m (1A)
Speed of waves in region A
= f (1M)
= 5 0.04
= 0.2 m s1 (1A)
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(b) (i) Region B is deeper. (1A)
(ii) The frequency is unchanged,
which is 5 Hz. (1A)
Speed of waves in region B
= 0.2
= 0.25 m s1 (1A)
By v = f, (1M)
wavelength of waves in region B
= = = 0.05 m (1A)
(c)
(Correct wave direction) (1A)
(Longer wavelength) (1A)
(d) We can put a sheet of perspex in the
ripple tank. The water above the
perspex is shallower than elsewhere.
(1A)
8 (a) Path difference at P
= AP – BP = 2 cm = (1A)
Therefore, destructive interference
occurs. (1A)
(b) Particle P will vibrate up and down with
a larger amplitude. (1A)
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By v = f, doubling the frequency
halves the wavelength, so the new
wavelength is 2 cm. (1A)
The path difference at P, which is 2 cm,
is now equal to . (1A)
Therefore, constructive interference
occurs there. (1A)
The displacementtime graph of particle
P is as shown.
(Correct labelled axes) (1A)
(Correct shape of the graph) (1A)
9 (a) For constructive interference,
largest possible wavelength
= path difference (1A)
= 2 cm (1A)
(b) For destructive interference,
path difference = (1M)
2 =
= 4 cm (1A)
The largest possible wavelength of the
waves is 4 cm.
(c) Path difference at Q
= 22 – 21 = 1 cm (1A)
Therefore, the largest possible
wavelength is 1 cm (i.e. path difference
at Q = and path difference at P = 2).
(1A)
(d) He cannot obtain a clear interference
pattern (1A)
because the two sources are incoherent.
(1A)
10 (a) The boat oscillates up and down. (1A)
(b) When waves approach the shore, their
wave speed (1A)
and wavelength decrease. (1A)
(c) (i) A tsunami is a transverse wave.
(1A)
This is because the moving
direction of water molecules
(vertical) is perpendicular to the
direction of travel of the tsunami
(horizontal). (1A)
(ii) Speed =
= (1M)
= 208 m s1 (1A)
(iii) The depth of seabed in the ocean
varies from place to place. (1A)
Therefore, refraction occurs and
the wavefront bends. (1A)
(iv) The statement is incorrect. (1A)
When water waves travel from the
centre of earthquake to the shore,
water is not transferred. (1A)
Only energy is transferred by the
water waves. (1A)
11 (a) After reflection, the reflected waves
move away from the barrier at 45 to the
normal, and (1A)
they interfere with the incident waves.
(1A)
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(b) (i) From Figure j, there are 4 waves
over 1.4 cm and the scale used by
the figure is 1 : 25. (1A)
Wavelength of the wave
= 25
= 8.75 cm (1A)
(ii)
(Correct shape) (2 1A)
(Constant separation between
wave crests) (1A)
(c) (i) Constructive interference (1A)
(ii) At point G, destructive
interference occurs, (1A)
so the amplitude of the wave is
always zero and there is no wave
energy at that point. (1A)
(iii)
Constructive interference occurs
when the path difference is 0, ,
2... (1A)
and destructive interference occurs
when the path difference is ,
, ... (1A)
At F and H, since the path
difference is 0 and respectively,
constructive interference occurs.
Similarly, constructive interference
occurs along PQ and TU and
forms lines of big crests and
troughs.
(1A)
At G, since the path difference is
, destructive interference
occurs. Similarly, destructive
interference occurs along RS and
so a line of calm water is formed.
(1A)
12 (a) 2 waves travel in opposite directions.
(1A)
The 2 waves should have similar
amplitude. (1A)
Stationary wave forms only at certain
frequencies. (1A)
(b) The displacement of a point on the
string is perpendicular to the mean
position of the string. (1A)
(c) The amplitude of the oscillation of point
A is larger than that of point B, (1A)
and they are in antiphase. (1A)
(d) Wavelength = 1.2 m (1M)
By v = f, (1M)
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frequency = = = 5.17 Hz (1A) (e)
(i) (6 loops) (1A)
(ii) (P, Q and R located appropriately,
i.e. they are not in neighbouring
loops of each other.) (1A)
13 (HKCEE 2005 Paper I Q5)
14 (a) Node (1A)
(b) Wavelength = = 0.48 m (1M)
Speed = f = 75 0.48 = 36 m s1 (1A)
(c) A stationary wave with two loops on the
string has wavelength equal to 1.2 m.
By v = f,
frequency = = = 30 Hz (1A)
Physics in articles (p. 100) (a) The minimum size that ordinary optical
microscopes can resolve is about 200 nm.
(1A)
(b) Diffraction (1A)
(c) Light diffracts around the edges of objects of
size comparable to the wavelength. (1A)
As a result, fine details close to the
wavelength look blurred. (1A)
(d) The microscopes that use X-rays have a
higher resolving power. (1A)
This is because X-rays have a much shorter
wavelength. (1A)
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