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    CHAPTER FOURTEEN

    OSCILLATIONS

    14.1 INTRODUCTIONIn our daily life we come across various kinds of motions.

    You have already learnt about some of them, e.g. rectilinear

    motion and motion of a projectile. Both these motions are

    non-repetitive. We have also learnt about uniform circular

    motion and orbital motion of planets in the solar system. In

    these cases, the motion is repeated after a certain interval of

    time, that is, it is periodic. In your childhood you must haveenjoyed rocking in a cradle or swinging on a swing. Both

    these motions are repetitive in nature but different from the

    periodic motion of a planet. Here, the object moves to and fro

    about a mean position. The pendulum of a wall clock executesa similar motion. Examples of such periodic to and fro motion

    abound : a boat tossing up and down in a river, the piston in

    a steam engine going back and forth, etc. Such a motion is

    termed as oscillatory motion. In this chapter we study this

    motion.

    The study of oscillatory motion is basic to physics; its

    concepts are required for the understanding of many physical

    phenomena. In musical instruments like the sitar, the guitar

    or the violin, we come across vibrating strings that produce

    pleasing sounds. The membranes in drums and diaphragms

    in telephone and speaker systems vibrate to and fro about

    their mean positions. The vibrations of air molecules makethe propagation of sound possible. In a solid, the atoms vibrate

    about their equilibrium positions, the average energy of

    vibrations being proportional to temperature. AC power

    supply give voltage that oscillates alternately going positive

    and negative about the mean value (zero).

    The description of a periodic motion in general, and

    oscillatory motion in particular, requires some fundamentalconcepts like period, frequency, displacement, amplitude and

    phase. These concepts are developed in the next section.

    14.1 Introduction

    14.2 Periodic and oscillatorymotions

    14.3 Simple harmonic motion

    14.4 Simple harmonic motionand uniform circularmotion

    14.5 Velocity and accelerationin simple harmonic motion

    14.6 Force law for simpleharmonic motion

    14.7 Energy in simple harmonicmotion

    14.8 Some systems executingSHM

    14.9 Damped simple harmonicmotion

    14.10 Forced oscillations andresonance

    Summary

    Points to ponderExercises

    Additional Exercises

    Appendix

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    14.2 PERIODIC AND OSCILLATORY MOTIONS

    Fig. 14.1 shows some periodic motions. Supposean insect climbs up a ramp and falls down it

    comes back to the initial point and repeats theprocess identically. If you draw a graph of itsheight above the ground versus time, it wouldlook something like Fig. 14.1 (a). If a child climbsup a step, comes down, and repeats the process,its height above the ground would look like thatin Fig. 14.1 (b). When you play the game ofbouncing a ball off the ground, between yourpalm and the ground, its height versus timegraph would look like the one in Fig. 14.1 (c).Note that both the curved parts in Fig. 14.1 (c)are sections of a parabola given by the Newtons

    equation of motion (see section 3.6),

    21

    2+ gth=ut for downward motion, and

    21

    2 gth = u t for upward motion,

    with different values ofuin each case. Theseare examples of periodic motion. Thus, a motionthat repeats itself at regular intervals of time iscalled periodic motion.

    Fig. 14.1 Examples of periodic motion. The period T

    is shown in each case.

    Very often the body undergoing periodicmotion has an equilibrium position somewhereinside its path. When the body is at this position

    no net external force acts on it. Therefore, if it isleft there at rest, it remains there forever. If thebody is given a small displacement from theposition, a force comes into play which tries tobring the body back to the equilibrium point,giving rise to oscillations orvibrations. Forexample, a ball placed in a bowl will be inequilibrium at the bottom. If displaced a littlefrom the point, it will perform oscillations in thebowl. Every oscillatory motion is periodic, butevery periodic motion need not be oscillatory.Circular motion is a periodic motion, but it isnot oscillatory.

    There is no significant difference betweenoscillations and vibrations. It seems that whenthe frequency is small, we call it oscillation (likethe oscillation of a branch of a tree), while whenthe frequency is high, we call it vibration (likethe vibration of a string of a musical instrument).

    Simple harmonic motion is the simplest formof oscillatory motion. This motion arises whenthe force on the oscillating body is directlyproportional to its displacement from the meanposition, which is also the equilibrium position.Further, at any point in its oscillation, this force

    is directed towards the mean position.In practice, oscillating bodies eventuallycome to rest at their equilibrium positions,because of the damping due to friction and otherdissipative causes. However, they can be forcedto remain oscillating by means of some externalperiodic agency. We discuss the phenomena ofdamped and forced oscillations later in thechapter.

    Any material medium can be pictured as acollection of a large number of coupledoscillators. The collective oscillations of theconstituents of a medium manifest themselves

    as waves. Examples of waves include waterwaves, seismic waves, electromagnetic waves.We shall study the wave phenomenon in the nextchapter.

    14.2.1 Period and frequency

    We have seen that any motion that repeats itselfat regular intervals of time is called periodicmotion.The smallest interval of time afterwhich the motion is repeated is called itsperiod. Let us denote the period by the symbolT. Its S.I. unit is second. For periodic motions,

    OSCILLATIONS 337

    (a)

    (b)

    (c)

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    PHYSICS338

    which are either too fast or too slow on the scaleof seconds, other convenient units of time areused. The period of vibrations of a quartz crystal

    is expressed in units of microseconds (106

    s)abbreviated as s. On the other hand, the orbitalperiod of the planet Mercury is 88 earth days.The Halleys comet appears after every 76 years.

    The reciprocal of T gives the number ofrepetitions that occur per unit time. Thisquantity is called the frequency of the periodicmotion. It is represented by the symbol . Therelation between and Tis

    = 1/T (14.1)

    The unit of is thus s1. After the discoverer ofradio waves, Heinrich Rudolph Hertz (1857-1894),a special name has been given to the unit offrequency. It is called hertz (abbreviated as Hz).Thus,

    1 hertz = 1 Hz =1 oscillation per second =1s1

    (14.2)

    Note, that the frequency, , is not necessarilyan integer.

    ! Example 14.1 On an average a humanheart is found to beat 75 times in a minute.Calculate its frequency and period.

    AnswerThe beat frequency of heart = 75/(1 min)= 75/(60 s)

    = 1.25 s1

    = 1.25 Hz The time period T = 1/(1.25 s1)

    = 0.8 s "14.2.2 DisplacementIn section 4.2, we defined displacement of aparticle as the change in its position vector. Inthis chapter, we use the term displacement

    in a more general sense. It refers to changewith time of any physical property under

    consideration. For example, in case of rectilinearmotion of a steel ball on a surface, the distancefrom the starting point as a function of time is

    its position displacement. The choice of originis a matter of convenience. Consider a blockattached to a spring, the other end of which isfixed to a rigid wall [see Fig.14.2(a)]. Generally itis convenient to measure displacement of the

    body from its equilibrium position. For anoscillating simple pendulum, the angle from thevertical as a function of time may be regarded

    as a displacement variable [see Fig.14.2(b)]. Theterm displacement is not always to be referred

    Fig. 14.2(a)A block attached to a spring, the other

    end of which is fixed to a rigid wall. The

    block moves on a frictionless surface. The

    motion of the block can be described in

    terms of its distance or displacement xfrom the wall.

    Fig.14.2(b) An oscillating simple pendulum; itsmotion can be described in terms ofangular displacementfrom the vertical.

    in the context of position only. There can bemany other kinds of displacement variables. Thevoltage across a capacitor, changing with timein an a.c. circuit, is also a displacementvariable. In the same way, pressure variationsin time in the propagation of sound wave, thechanging electric and magnetic fields in a lightwave are examples of displacement in differentcontexts. The displacement variable may take

    both positive and negative values. Inexperiments on oscillations, the displacementis measured for different times.

    The displacement can be represented by amathematical function of time. In case of periodicmotion, this function is periodic in time. One ofthe simplest periodic functions is given by

    f(t) = Acost (14.3a)

    If the argument of this function, t, isincreased by an integral multiple of 2radians,

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    OSCILLATIONS 339

    the value of the function remains the same. Thefunctionf(t) is then periodic and its period, T,is given by

    2=T (14.3b)

    Thus, the functionf(t) is periodic with period T,

    f(t) = f(t+T)

    The same result is obviously correct if weconsider a sine function,f(t) = Asin t. Further,a linear combination of sine and cosine functionslike,

    f(t) = Asint + Bcost (14.3c)is also a periodic function with the same periodT. Taking,

    A = Dcos and B = Dsin

    Eq. (14.3c) can be written as,

    f(t) = Dsin(t + ) , (14.3d)

    Here Dand are constant given by

    2 2 1and tanBD = A + B

    A

    The great importance of periodic sine andcosine functions is due to a remarkable resultproved by the French mathematician, Jean

    Baptiste Joseph Fourier (1768-1830): Anyperiodic function can be expressed as asuperposition of sine and cosine functionsof different time periods with suitablecoefficients.

    ! Example 14.2 Which of the followingfunctions of time represent (a) periodic and(b) non-periodic motion? Give the period foreach case of periodic motion [ is anypositive constant].(i) sin t+ cos t

    (ii) sin t+ cos 2 t+ sin 4 t(iii) et

    (iv) log (t)

    Answer

    (i) sin t+ cos tis a periodic function, it can

    also be written as 2 sin (t+ /4).

    Now 2 sin (t+/4)= 2 sin (t+ /4+2)

    = 2 sin [(t + 2/) + /4]

    The periodic time of the function is 2/.

    (ii) This is an example of a periodic motion. Itcan be noted that each term represents aperiodic function with a different angularfrequency. Since period is the least intervalof time after which a function repeats itsvalue, sin thas a periodT

    0= 2/; cos 2 t

    has a period /=T0/2; and sin 4 thas a

    period 2/4= T0/4. The period of the first

    term is a multiple of the periods of the lasttwo terms. Therefore, the smallest intervalof time after which the sum of the threeterms repeats is T

    0, and thus the sum is a

    periodic function with a period 2/.(iii) The function et is not periodic, it

    decreases monotonically with increasingtime and tends to zero as t and thus,never repeats its value.

    (iv) The function log(t) increases mono-tonically with time t. It, therefore, neverrepeats its value and is a non-periodicfunction. It may be noted that as t,log(t) diverges to . It, therefore, cannotrepresent any kind of physicaldisplacement. "

    14.3 SIMPLE HARMONIC MOTION

    Consider a particle oscillating back and forthabout the origin of an x-axis between the limits+Aand Aas shown in Fig. 14.3. This oscillatorymotion is said to be simple harmonic if the

    Fig. 14.3 A particle vibrating back and forth about

    the origin of x-axis, between the limits +A

    and A.

    displacementxof the particle from the originvaries with time as :

    x(t) =Acos (t+ ) (14.4)whereA, and are constants.

    Thus, simple harmonic motion (SHM) is notany periodic motion but one in whichdisplacement is a sinusoidal function of time.Fig. 14.4 shows what the positions of a particleexecuting SHM are at discrete value of time, eachinterval of time being T/4 where Tis the period

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    of motion. Fig. 14.5 plots the graph ofxversus t,which gives the values of displacement as acontinuous function of time. The quantitiesA,and which characterize a given SHM havestandard names, as summarised in Fig. 14.6.Let us understand these quantities.

    The amplitutdeAof SHM is the magnitudeof maximum displacement of the particle.[Note,Acan be taken to be positive without

    any loss of generality]. As the cosine functionof time varies from +1 to 1, the displacementvaries between the extremes Aand A. Twosimple harmonic motions may have same and but different amplitudes Aand B, asshown in Fig. 14.7 (a).

    Fig. 14.4 The location of the particle in SHM at thediscrete values t = 0, T/4, T/2, 3T/4, T,

    5T/4. The time after which motion repeats

    itself is T. T will remain fixed, no matter

    what location you choose as the initial (t =

    0) location. The speed is maximum for zerodisplacement (at x = 0) and zero at the

    extremes of motion.

    Fig. 14.5 Displacement as a continuous function of

    time for simple harmonic motion.

    Fig. 14.7 (b)A plot obtained from Eq. (14.4) . The

    curves 3 and 4 are for = 0 and -/4

    respectively. The amplitude A is same for

    both the plots.

    Fig. 14.7 (a)A plot of displacement as a function oftime as obtained from Eq. (14.4) with

    = 0. The curves 1 and 2 are for twodifferent amplitudes A and B.

    x(t) : displacement xas a function of time tA : amplitude : angular frequencyt + : phase (time-dependent) : phase constant

    Fig. 14.6 The meaning of standard symbols

    in Eq. (14.4)

    While the amplitude A is fixed for a givenSHM, the state of motion (position and velocity)of the particle at any time tis determined by the

    argument (t+ ) in the cosine function. Thistime-dependent quantity, (t+ ) is called thephaseof the motion. The value of plase att= 0is and is called thephase constant(orphaseangle). If the amplitude is known, can bedetermined from the displacement att= 0. Twosimple harmonic motions may have the sameAand but different phase angle , as shown inFig. 14.7 (b).

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    OSCILLATIONS 341

    Finally, the quantity can be seen to berelated to the period of motion T. Taking, forsimplicity, = 0 in Eq. (14.4), we have

    x( t) = Acos t (14.5)

    Since the motion has a period T, x(t) is equal tox( t+ T). That is,

    Acos t=Acos (t + T) (14.6)

    Now the cosine function is periodic with period2, i.e., it first repeats itself when the argumentchanges by 2. Therefore,

    (t + T) = t + 2

    that is = 2/T (14.7)

    is called the angular frequency of SHM. ItsS.I. unit is radians per second. Since thefrequency of oscillations is simply 1/T, is 2times the frequency of oscillation. Two simpleharmonic motions may have the same A and ,but different, as seen in Fig. 14.8. In this plotthe curve (b) has half the period and twice thefrequency of the curve (a).

    This function represents a simple harmonicmotion having a period T = 2/and aphase angle (/4) or (7/4)

    (b) sin2

    t= cos 2 tThe function is periodic having a periodT = /. It also represents a harmonicmotion with the point of equilibrium

    occurring at instead of zero. "

    14.4 SIMPLE HARMONIC MOTION ANDUNIFORM CIRCULAR MOTION

    In this section we show that the projection ofuniform circular motion on a diameter of thecircle follows simple harmonic motion. Asimple experiment (Fig. 14.9) helps us visualize

    this connection. Tie a ball to the end of a stringand make it move in a horizontal plane abouta fixed point with a constant angular speed.The ball would then perform a uniform circularmotion in the horizontal plane. Observe theball sideways or from the front, fixing yourattention in the plane of motion. The ball willappear to execute to and fro motion along ahorizontal line with the point of rotation asthe midpoint. You could alternatively observethe shadow of the ball on a wall which isperpendicular to the plane of the circle. In this

    process what we are observing is the motionof the ball on a diameter of the circle normal

    Fig. 14.9 Circular motion of a ball in a plane viewededge-on is SHM.

    Fig. 14.8 Plots of Eq. (14.4) for= 0 for two differentperiods.

    ! Example 14.3 Which of the following

    functions of time represent (a) simpleharmonic motion and (b) periodic but notsimple harmonic? Give the period for eachcase.(1) sin t cos t(2) sin2t

    Answer(a) sin t cos t

    = sin t sin (/2 t)= 2 cos (/4) sin (t/4)= 2 sin (t/4)

    to the direction of viewing.Fig. 14.10 describes the same situation

    mathematically. Suppose a particle P is movinguniformly on a circle of radius Awith angularspeed. The sense of rotation is anticlockwise.The initial position vector of the particle, i.e.,

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    the vectorOP att= 0 makes an angle ofwith

    the positive direction ofx-axis. In time t, it willcover a further angle tand its position vectorwill make an angle oft + with the +ve x-axis. Next consider the projection of the

    position vector OP on the x-axis. This will beOP. The position of P on the x-axis, as theparticle P moves on the circle, is given by

    x(t) = Acos (t+ )

    which is the defining equation of SHM. Thisshows that if P moves uniformly on a circle,its projection P on a diameter of the circleexecutes SHM. The particle P and the circleon which it moves arc sometimes referred toas the reference particleand the reference circlerespectively.

    We can take projection of the motion of P onany diameter, say the y-axis. In that case, thedisplacementy(t) of P on the y-axis is given by

    y=Asin (t+ )

    which is also an SHM of the same amplitudeas that of the projection on x-axis, but differingby a phase of/2.

    In spite of this connection between circular

    motion and SHM, the force acting on a particlein linear simple harmonic motion is very

    different from the centripetal force needed tokeep a particle in uniform circular motion.! Example 14.4 Fig. 14.10 depicts two

    circular motions. The radius of the circle,the period of revolution, the initial positionand the sense of revolution are indicatedon the figures. Obtain the simple harmonicmotions of the x-projection of the radiusvector of the rotating particle P in eachcase.

    Answer

    (a) At t= 0, OP makes an angle of 45o = /4 radwith the (positive direction of) x-axis. After

    time t, it covers an angle tT

    2 in the

    anticlockwise sense, and makes an angle

    of4

    +2

    tT

    with the x-axis.

    The projection of OP on the x-axis at time tis given by,

    x(t) = Acos( 2 +4

    tT

    )ForT= 4 s,

    x(t) = Acos2

    +4 4

    t

    which is a SHM of amplitudeA, period 4 s,

    and an initial phase* =4

    .(b) In this case att= 0, OP makes an angle of

    90o =2

    with the x-axis. After a time t, it

    * The natural unit of angle is radian, defined through the ratio of arc to radius. Angle is a dimensionlessquantity. Therefore it is not always necessary to mention the unit radian when we use, its multiples

    or submultiples. The conversion between radian and degree is not similar to that between metre and

    centimetre or mile. If the argument of a trigonometric function is stated without units, it is understood

    that the unit is radian. On the other hand, if degree is to be used as the unit of angle, then it must be

    shown explicitly. For example, sin(150) means sine of 15 degree, but sin(15) means sine of 15 radians.Hereafter, we will often drop rad as the unit, and it should be understood that whenever ang le is

    mentioned as a numerical value, without units, it is to be taken as radians.

    Fig. 14.10

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    OSCILLATIONS 343

    covers an angle of 2 tT

    in the clockwise

    sense and makes an angle of2

    2 tT

    with the x-axis. The projection of OP on thex-axis at time tis given by

    x( t) = Bcos2

    2

    tT

    = Bsin (2 tT

    )ForT= 30 s,

    x(t) = Bsin15

    t

    Writing this as x(t) = Bcos 15 2

    t

    , and

    comparing with Eq. (14.4). We find that thisrepresents a SHM of amplitudeB, period 30 s,

    and an initial phase of2

    . "

    14.5 VELOCITY AND ACCELERATION IN

    SIMPLE HARMONIC MOTION

    The speed of a particle v in uniform circularmotion is its angular speed times the radius

    of the circleA.

    v= A (14.8)

    The direction of velocity v at a time tis along

    the tangent to the circle at the point where theparticle is located at that instant. From thegeometry of Fig. 14.11, it is clear that the velocityof the projection particle P at time tis

    v( t) = Asin (t + ) (14.9)

    where the negative sign shows thatv(t) has adirection opposite to the positive direction ofx-axis. Eq. (14.9) gives the instantaneous

    velocity of a particle executing SHM, wheredisplacement is given by Eq. (14.4). We can, ofcourse, obtain this equation without usinggeometrical argument, directly by differentiating(Eq. 14.4) with respect oft:

    d( )

    dv(t) = x t

    t(14.10)

    The method of reference circle can be similarlyused for obtaining instantaneous accelerationof a particle undergoing SHM. We know that thecentripetal acceleration of a particle P in uniformcircular motion has a magnitude v2/A or2A,

    and it is directed towards the centre i.e., thedirection is along PO. The instantaneousacceleration of the projection particle P is then(See Fig. 14.12)

    a(t) = 2Acos (t+ )

    = 2x(t) (14.11)

    Fig. 14.11 The velocity, v (t), of the particle Pis the

    projecti on of the ve loci ty v of thereference particle, P.

    Fig. 14.12 The acceleration, a(t), of the particle Pis

    the projection of the accelerationaof thereference particle P.

    Eq. (14.11) gives the acceleration of a particlein SHM. The same equation can again beobtained directly by differentiating velocityv(t)given by Eq. (14.9) with respect to time:

    d( ) ( )

    da t = v t

    t(14.12)

    We note from Eq. (14.11) the importantproperty that acceleration of a particle in SHMis proportional to displacement. For x(t) > 0,a(t)< 0 and for x(t) < 0, a(t) > 0. Thus, whatever the

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    value ofxbetween AandA, the accelerationa(t) is always directed towards the centre.For simplicity, let us put = 0 and write the

    expression forx(t), v(t) and a(t)x(t) = A cos t, v(t) = Asin t, a(t)=2 A cos tThe corresponding plots are shown in Fig. 14.13.All quantitites vary sinusoidally with time; onlytheir maxima differ and the different plots differin phase. xvaries between AtoA; v(t) variesfrom Ato Aand a(t) from 2Ato 2A. Withrespect to displacement plot, velocity plot has aphase difference of/2 and acceleration plothas a phase difference of.

    (b) Using Eq. (14.9), the speed of the body= (5.0 m)(2 s1) sin [(2 s1) 1.5 s+ /4]

    = (5.0 m)(2s1

    ) sin [(3+ /4)]= 10 0.707 m s1

    = 22 m s1

    (c) Using Eq.(14.10), the acceleration of thebody

    = (2 s1)2 displacement= (2s1)2 (3.535 m)

    = 140 m s2 "

    14.6 FORCE LAW FOR SIMPLE HARMONICMOTION

    Using Newtons second law of motion, and the

    expression for acceleration of a particleundergoing SHM (Eq. 14.11), the force actingon a particle of mass min SHM is

    F(t) = ma

    = m2 x(t)

    i.e., F(t) = k x(t) (14.13)

    where k = m2 (14.14a)

    or =k

    m(14.14b)

    Like acceleration, force is always directedtowards the mean position - hence it is sometimescalled the restoring force in SHM. To summarizethe discussion so far, simple harmonic motioncan be defined in two equivalent ways, either byEq. (14.4) for displacement or by Eq. (14.13) thatgives its force law. Going from Eq. (14.4) to Eq.(14.13) required us to differentiate two times.Likewise by integrating the force law Eq. (14.13)two times, we can get back Eq. (14.4).

    Note that the force in Eq. (14.13) is linearlyproportional to x(t). A particle oscillating undersuch a force is, therefore, calling a linear

    harmonic oscillator. In the real world, the forcemay contain small additional terms proportionalto x2, x3, etc. These then are called non-linearoscillators.

    ! Example 14.6Two identical springs ofspring constantkare attached to a blockof mass mand to fixed supports as shownin Fig. 14.14. Show that when the mass isdisplaced from its equilibrium position oneither side, it executes a simple harmonicmotion. Find the period of oscillations.

    Fig. 14.13 Displacement, velocity and acceleration of

    a particle in simple harmonic motion have

    the same period T, but they differ in phase

    ! Example 14.5 A body oscillates with SHMaccording to the equation (in SI units),

    x = 5 cos [2t+ /4].

    Att= 1.5 s, calculate the (a) displacement,(b) speed and (c) acceleration of the body.

    AnswerThe angular frequency of the body= 2s1 and its time period T= 1 s.Att= 1.5 s(a) displacement = (5.0 m) cos [(2 s1)

    1.5 s + /4]= (5.0 m) cos [(3+ /4)]= 5.0 0.707 m= 3.535 m

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    Fig. 14.14

    AnswerLet the mass be displaced by a smalldistance x to the right side of the equilibriumposition, as shown in Fig. 14.15. Under thissituation the spring on the left side gets

    Fig. 14.15

    elongated by a length equal to xand that onthe right side gets compressed by the same

    length. The forces acting on the mass arethen,

    F1

    = k x(force exerted by the spring on

    the left side, trying to pull themass towards the mean

    position)

    F2

    =k x (force exerted by the spring on

    the right side, trying to push the

    mass towards the meanposition)

    The net force, F, acting on the mass is thengiven by,

    F = 2kx

    Hence the force acting on the mass isproportional to the displacement and is directed

    towards the mean position; therefore, the motionexecuted by the mass is simple harmonic. The

    time period of oscillations is,

    T = 2m

    2k "

    14.7 ENERGY IN SIMPLE HARMONICMOTION

    Both kinetic and potential energies of a particlein SHM vary between zero and their maximum

    values.In section14.5 we have seen that the velocity

    of a particle executing SHM, is a periodicfunction of time. It is zero at the extreme positions

    of displacement. Therefore, the kinetic energy (K)of such a particle, which is defined as

    2

    2

    1mv=K

    2 2 21 sin ( + )2

    = m A t

    2

    1sin ( + )

    2

    2= k A t (14.15)

    is also a periodic function of time, being zerowhen the displacement is maximum and

    maximum when the particle is at the meanposition. Note, since the sign ofvis immaterial

    in K, the period ofKis T/2.What is the potential energy (U) of a particle

    executing simple harmonic motion? In

    Chapter 6, we have seen that the concept ofpotential energy is possible only for conservativeforces. The spring force F = kxis a conservative

    force, with associated potential energy

    21

    2U = k x (14.16)

    Hence the potential energy of a particleexecuting simple harmonic motion is,

    U(x) = 2

    2

    1xk

    2 21

    cos ( + )2

    = k A t (14.17)

    Thus, the potential energy of a particle

    executing simple harmonic motion is also

    periodic, with periodT/2, being zero at the mean

    position and maximum at the extreme

    displacements.

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    It follows from Eqs. (14.15) and (14.17) that

    the total energy, E, of the system is,

    E = U + K

    2 2 2 2

    1 1cos ( + ) + sin ( + )

    2 2= k A t k A t

    2 2 21 cos ( + ) + sin ( + )2

    = k A t t

    Using the familiar trigonometric identity, thevalue of the expression in the brackets is unity.Thus,

    21

    2E = k A (14.18)

    The total mechanical energy of a harmonic

    oscillator is thus independent of time as expected

    for motion under any conservative force. The

    time and displacement dependence of the

    potential and kinetic energies of a linear simple

    harmonic oscillator are shown in

    Fig. 14.16.

    Observe that both kinetic energy and

    potential energy in SHM are seen to be always

    positive in Fig. 14.16. Kinetic energy can, of

    course, be never negative, since it isproportional to the square of speed. Potential

    energy is positive by choice of the undermined

    constant in potential energy. Both kinetic

    energy and potential energy peak twice during

    each period of SHM. Forx = 0, the energy is

    kinetic; at the extremes x= A, it is all potential

    energy. In the course of motion between these

    limits, kinetic energy increases at the expense

    of potential energy or vice-versa.

    !Example 14.7 A block whose mass is 1 kgis fastened to a spring. The spring has aspring constant of 50 N m1. The block ispulled to a distance x = 10 cm from itsequilibrium position atx= 0 on a frictionlesssurface from rest at t= 0. Calculate thekinetic, potential and total energies of theblock when it is 5 cm away from the meanposition.

    AnswerThe block executes SHM, its angularfrequency, as given by Eq. (14.14b), is

    =k

    m

    =50 N m

    1

    1kg

    = 7.07 rad s1

    Its displacement at any time t is then given by,

    x(t) = 0.1 cos (7.07 t)

    Therefore, when the particle is 5 cm away fromthe mean position, we have

    0.05 = 0.1 cos (7.07t)

    Or cos (7.07t) = 0.5 and hence

    sin (7.07t) =3

    2 = 0.866

    Fig. 14.16 Kinetic energy, potential energy and total

    energy as a function of time [shown in (a)]and displacement [shown in (b)] of a particle

    in SHM. The kinetic energy and potential

    energy both repeat after a period T/2. The

    total energy remains constant at all t or x.

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    Then, the velocity of the block atx= 5 cm is

    = 0.1 7.07 0.866 m s1

    = 0.61 m s

    1

    Hence the K.E. of the block,

    2

    1= 2vm

    = [1kg (0.6123 m s1 )2 ]

    = 0.19 J

    The P.E. of the block,

    2

    1= 2xk

    = (50 N m1 0.05 m 0.05 m)= 0.0625 J

    The total energy of the block atx= 5 cm,

    = K.E. + P.E.

    = 0.25 J

    we also know that at maximum displacement,K.E. is zero and hence the total energy of thesystem is equal to the P.E. Therefore, the totalenergy of the system,

    = (50 N m1 0.1 m 0.1 m )

    = 0.25 J

    which is same as the sum of the two energies ata displacement of 5 cm. This is in conformitywith the principle of conservation of energy. "

    14.8 SOME SYSTEMS EXECUTING SIMPLEHARMONIC MOTION

    There are no physical examples of absolutelypure simple harmonic motion. In practice wecome across systems that execute simpleharmonic motion approximately under certainconditions. In the subsequent part of thissection, we discuss the motion executed by some

    such systems.14.8.1 Oscillations due to a Spring

    The simplest observable example of simpleharmonic motion is the small oscillations of ablock of mass mfixed to a spring, which in turnis fixed to a rigid wall as shown in Fig. 14.17.The block is placed on a frictionless horizontalsurface. If the block is pulled on one side and isreleased, it then executes a to and fro motionabout a mean position. Letx= 0, indicate theposition of the centre of the block when the

    spring is in equilibrium. The positions markedas A and +A indicate the maximumdisplacements to the left and the right of themean position. We have already learnt thatsprings have special properties, which were firstdiscovered by the English physicist RobertHooke. He had shown that such a system whendeformed, is subject to a restoring force, themagnitude of which is proportional to thedeformation or the displacement and acts inopposite direction. This is known as Hookeslaw (Chapter 9). It holds good for displacementssmall in comparison to the length of the spring.

    At any time t, if the displacement of the blockfrom its mean position isx, the restoring force Facting on the block is,

    F(x) = k x (14.19)

    The constant of proportionality, k, is calledthe spring constant, its value is governed by theelastic properties of the spring. A stiff spring haslarge kand a soft spring has small k. Equation(14.19) is same as the force law for SHM andtherefore the system executes a simple harmonicmotion. From Eq. (14.14) we have,

    = km

    (14.20)

    and the period, T, of the oscillator is given by,

    = 2m

    Tk

    (14.21)Stiff springs have high value of k (spring

    constant). A block of small mass mattached toa stiff spring will have, according to Eq. (14.20),large oscillation frequency, as expectedphysically.

    Fig. 14.17A linear simple harmonic osci llator

    consisting of a block of mass m attached

    to a spring. The block moves over africtionless surface. The box, when pulled

    or pushed and released, executes simple

    harmonic motion.

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    of pendulum. You can also make your ownpendulum by tying a piece of stone to a longunstretchable thread, approximately 100 cm

    long. Suspend your pendulum from a suitablesupport so that it is free to oscillate. Displacethe stone to one side by a small distance andlet it go. The stone executes a to and fro motion,

    it is periodic with a period of about two seconds.We shall show that this periodic motion is

    simple harmonic for small displacements fromthe mean position. Consider simple pendulum a small bob of mass mtied to an inextensiblemass less string of length L. The other end ofthe string is fixed to a support in the ceiling.

    The bob oscillates in a plane about the vertical

    line through the support. Fig. 14.18(a) showsthis system. Fig. 14.18(b) is a kind of free-body

    diagram of the simple pendulum showing theforces acting on the bob.

    ! Example 14.8A 5 kg collar is attachedto a spring of spring constant 500 N m1. Itslides without friction over a horizontal rod.The collar is displaced from its equilibriumposition by 10.0 cm and released. Calculate(a) the period of oscillation,(b) the maximum speed and(c) maximum acceleration of the collar.

    Answer (a) The period of oscillation as given byEq. (14.21) is,

    = 2m

    Tk

    = 2 1mN500kg0.5

    = (2/10) s = 0.63 s(b) The velocity of the collar executing SHM is

    given by,v(t) = Asin (t +)

    The maximum speed is given by,v

    m= A

    = 0.1k

    m

    = 0.1kg5

    1mN500

    = 1 m s1

    and it occurs atx= 0(c) The acceleration of the collar at the

    displacementx(t) from the equilibrium isgiven by,

    a(t) = 2 x(t)

    = k

    x(t)

    Therefore the maximum acceleration is, a

    max= 2A

    =500 N m

    1

    5 kgx 0.1 m

    = 10 m s2

    and it occurs at the extremities. "

    14.8.2 The Simple Pendulum

    It is said that Galileo measured the periods of aswinging chandelier in a church by his pulsebeats. He observed that the motion of thechandelier was periodic. The system is a kind

    (a)

    (b)

    Fig. 14.18 (a) A bob oscillating about its meanposition. (b) The radial force T-mg cos

    provides centripetal force but no torque

    about the support. The tangential force

    mgsinprovides the restoring torque.

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    Let be the angle made by the string withthe vertical. When the bob is at the mean

    position, = 0

    There are only two forces acting on the bob;the tension T along the string and the vertical

    force due to gravity (=mg). The force mgcan beresolved into the componentmgcos along thestring and mg sin perpendicular to it. Sincethe motion of the bob is along a circle of lengthLand centre at the support point, the bob has

    a radial acceleration (2L) and also a tangentalacceleration; the latter arises since motion along

    the arc of the circle is not uniform. The radialacceleration is provided by the net radial forceT mgcos, while the tangential acceleration is

    provided bymg sin. It is more convenient towork with torque about the support since the

    radial force gives zero torque. Torque aboutthe support is entirely provided by the tangentalcomponent of force

    = L(mgsin) (14.22)

    This is a restoring torque that tends to reduceangular displacement hence the negativesign. By Newtons law of rotational motion,

    = I (14.23)

    where Iis the moment of inertia of the system

    about the support and is the angularacceleration. Thus,

    I= m gsin L (14.24)

    Or,

    = sinm gL

    I (14.25)

    We can simplify Eq. (14.25) if we assume thatthe displacementis small. We know that sin can be expressed as,

    sin ...3! 5!

    (14.26)

    where is in radians.Now if is small, sin can be approximated

    byand Eq. (14.25) can then be written as,

    = mgL

    I (14.27)

    In Table 14.1, we have listed the angle indegrees, its equivalent in radians, and the value

    SHM - how small should the amplitude be?

    When you perform the experiment to

    determine the time period of a simplependulum, your teacher tells you to keepthe amplitude small. But have you everasked how small is small? Should theamplitude to 50, 20, 10 or 0.50? Or could itbe 100, 200 or 300?

    To appreciate this, it would be better tomeasure the time period for differentamplitudes, up to large amplitudes. Ofcourse, for large oscillations, you will haveto take care that the pendulum oscillatesin a vertical plane. Let us denote the time

    period for small-amplitude oscillations asT(0) and write the time period for amplitude

    0as T(

    0) = cT(0), where cis the multiplying

    factor. If you plot a graph ofcversus 0,

    you will get values somewhat like this:

    0

    : 200 450 500 700 900

    c : 1.02 1.04 1.05 1.10 1.18

    This means that the error in the timeperiod is about 2% at an amplitude of 200,5% at an amplitude of 500, and 10% at anamplitude of 700 and 18% at an amplitude

    of 900

    .In the experiment, you will never be able

    to measure T(0) because this means thereare no oscillations. Even theoretically,sin is exactly equal to only for = 0.There will be some inaccuracy for all othervalues of. The difference increases withincreasing . Therefore we have to decidehow much error we can tolerate. Nomeasurement is ever perfectly accurate.You must also consider questions likethese: What is the accuracy of the

    stopwatch? What is your own accuracy instarting and stopping the stopwatch? Youwill realise that the accuracy in yourmeasurements at this level is never betterthan 5% or 10%. Since the above tableshows that the time period of the pendulumincreases hardly by 5% at an amplitude of500 over its low amplitude value, you couldvery well keep the amplitude to be 50 inyour experiments.

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    of the function sin . From this table it can beseen that for as large as 20 degrees, sin isnearly the same as expressed in radians.

    Table 14.1 sin as a function of angle

    Equation (14.27) is mathematically, identical

    to Eq. (14.11) except that the variable is angulardisplacement. Hence we have proved that forsmall, the motion of the bob is simple harmonic.From Eqs. (14.27) and (14.11),

    =mgL

    I

    and

    I

    TmgL

    (14.28)Now since the string of the simple pendulum

    is mass less, the moment of inertiaIis simplymL2. Eq. (14.28) then gives the well-knownformula for time period of a simple pendulum.

    LT

    g (14.29)

    ! Example 14.9What is the length of asimple pendulum, which ticks seconds ?

    AnswerFrom Eq. (14.29), the time period of asimple pendulum is given by,

    L

    Tg

    From this relation one gets,

    2

    2 4

    gTL

    The time period of a simple pendulum, whichticks seconds, is 2 s. Therefore, forg= 9.8 m s2

    and T = 2 s, Lis

    Fig. 14.19 The viscous surrounding medium exerts

    a damping force on an oscillating spring,

    eventually bringing it to rest.

    2 2

    2

    9.8(m s ) 4(s )

    4

    = 1 m "

    14.9 DAMPED SIMPLE HARMONIC MOTION

    We know that the motion of a simple pendulum,swinging in air, dies out eventually. Why does ithappen ? This is because the air drag and thefriction at the support oppose the motion of thependulum and dissipate its energy gradually.

    The pendulum is said to execute dampedoscillations. In dampled oscillations, the energyof the system is dissipated continuously; but,for small damping, the oscillations remain

    approximately periodic. The dissipating forcesare generally the frictional forces. To understandthe effect of such external forces on the motionof an oscillator, let us consider a system asshown in Fig. 14.19. Here a block of mass mconnected to an elastic spring of spring constant

    koscillates vertically. If the block is pushed downa little and released, its angular frequency of

    oscillation isk

    m, as seen in Eq. (14.20).

    However, in practice, the surrounding medium(air) will exert a damping force on the motion ofthe block and the mechanical energy of theblock-spring system will decrease. The energyloss will appear as heat of the surroundingmedium (and the block also) [Fig. 14.19].

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    The damping force depends on the nature ofthe surrounding medium. If the block isimmersed in a liquid, the magnitude of damping

    will be much greater and the dissipation ofenergy much faster. The damping force isgenerally proportional to velocity of the bob.[Remember Stokes Law, Eq. (10.19)] and actsopposite to the direction of velocity. If thedamping force is denoted byF

    d, we have

    Fd

    = bv (14.30)

    where the positive constant b depends oncharacteristics of the medium (viscosity, forexample) and the size and shape of the block,etc. Eq. (14.30) is usually valid only for small

    velocity.

    When the mass mis attached to the springand released, the spring will elongate a little andthe mass will settle at some height. This position,shown by O in Fig 14.20, is the equilibriumposition of the mass. If the mass is pulled downor pushed up a little, the restoring force on theblock due to the spring is F

    S= kx, where x is

    the displacement* of the mass from itsequilibrium position. Thus, the total force actingon the mass at any time t, isF= kx bv.

    Ifa(t) is the acceleration of mass at time t,

    then by Newtons Law of Motion applied alongthe direction of motion, we have

    m a(t) = k x(t) b v(t) (14.31)Here we have dropped the vector notation

    because we are discussing one-dimensionalmotion.

    Using the first and second derivatives ofx(t)forv(t) and a(t) respectively, we have

    2d d

    dd 2x x

    m b k x 0 tt

    (14.32)

    The solution of Eq. (14.32) describes themotion of the block under the influence of adamping force which is proportional to velocity.The solution is found to be of the form

    x( t) = A eb t/2mcos(t + ) (14.33)

    where ais the amplitude and is the angularfrequency of the damped oscillator given by,

    4m

    b

    m

    k'

    2

    2

    = (14.34)

    In this function, the cosine function has a

    period 2/ but the function x(t) is not strictlyperiodic because of the factor eb t/2mwhichdecreases continuously with time. However, if thedecrease is small in one time period T, the motionrepresented by Eq. (14.33) is approximatelyperiodic.

    The solution, Eq. (14.33), can be graphicallyrepresented as shown in Fig. 14.20. We canregard it as a cosine function whose amplitude,which isAeb t/2m, gradually decreases with time.

    * Under gravity, the block will be at a certain equilibrium position O on the spring; x here represents thedisplacement from that position.

    Fig. 14.20A damped oscillator is approximatelyperiodic with decreasing amplitude of

    oscillation. With greater damping,

    oscillations die out faster.

    Now the mechanical energy of the undampedoscillator is 1/2 kA2. For a damped oscillator,the amplitude is not constant but depends ontime. For small damping, we may use the sameexpression but regard the amplitude as A ebt/2m.

    1

    ( ) 22 b t/m

    E t k A e = (14.35)

    Equation (14.35) shows that the total energyof the system decreases exponentially with time.Note that small damping means that the

    dimensionless ratio

    mk

    b is much less than 1.

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    Of course, an expected, if we put b = 0, allequations of a damped oscillator in this sectionreduce to the corresponding equations of an

    undamped oscillator.

    ! Example 14.10 For the damped oscillatorshown in Fig. 14.20, the mass mof the blockis 200 g, k = 90 N m1 and the dampingconstantb is 40 g s1. Calculate (a) theperiod of oscillation, (b) time taken for itsamplitude of vibrations to drop to half ofits initial value and (c) the time taken forits mechanical energy to drop to half itsinitial value.

    Answer(a) We see thatkm= 900.2 = 18 kg N

    m1 = kg2 s2; therefore km= 4.243 kg s1, and

    b= 0.04 kg s1. Therefore bis much less than

    km. Hence the time period Tfrom Eq. (14.34)

    is given by

    2m

    Tk

    1

    0.22

    90 N m

    kg

    = 0.3 s

    (b) Now, from Eq. (14.33), the time, T1/2

    , for theamplitude to drop to half of its initial value isgiven by,

    ln(1/2)

    /2T =1/2

    b m

    0.6 39 2 200 s40

    = 6.93 s

    (c) For calculating the time, t1/ 2

    , for itsmechanical energy to drop to half its initial valuewe make use of Eq. (14.35). From this equationwe have,

    E(t1/2

    )/E(0) = exp (bt1/2

    /m)

    Or = exp (bt1/2

    /m)

    ln (1/2) = (bt1/2

    /m)

    Or t1/2

    1

    0.6 39200 g

    40 g s

    = 3.46 sThis is just half of the decay period for

    amplitude. This is not surprising, because,according to Eqs. (14.33) and (14.35), energydepends on the square of the amplitude. Noticethat there is a factor of 2 in the exponents ofthe two exponentials. "

    14.10 FORCED OSCILLATIONS AND

    RESONANCEWhen a system (such as a simple pendulum ora block attached to a spring) is displaced fromits equilibrium position and released, it oscillates

    with its natural frequency, and the oscillationsare called free oscillations. All free oscillationseventually die out because of the ever present

    damping forces. However, an external agencycan maintain these oscillations. These are calledforce ordriven oscillations. We consider thecase when the external force is itself periodic,

    with a frequencydcalled the driven frequency.

    A most important fact of forced periodicoscillations is that the system oscillates not with

    its natural frequency, but at the frequencyd

    of the external agency; the free oscillations dieout due to damping. A most familiar example of

    forced oscillation is when a child in a gardenswing periodically presses his feet against theground (or someone else periodically gives thechild a push) to maintain the oscillations.

    Suppose an external force F(t) of amplitudeF

    0that varies periodically with time is applied

    to a damped oscillator. Such a force can be

    represented as,F(t) = F

    ocos

    dt (14.36)

    The motion of a particle under the combinedaction of a linear restoring force, damping forceand a time dependent driving force representedby Eq. (14.36) is given by,

    m a(t) = k x(t) bv(t) + Focos

    dt (14.37a)

    Substituting d2x/d t2 for acceleration inEq. (14.37a) and rearranging it, we get

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    frequency of pendulum 1, i.e. the frequency ofthe driving force but with different amplitudes.They oscil late with small amplitudes. The

    response of pendulum 4 is in contrast to thisset of pendulums. It oscillates with the samefrequency as that of pendulum 1 and itsamplitude gradually picks up and becomes verylarge. A resonance-like response is seen. Thishappens because in this the condition forresonance is satisfied, i.e. the natural frequencyof the system coincides with that of the drivingforce.

    We have so far considered oscillating systemswhich have just one natural frequency. Ingeneral, a system may have several natural

    frequencies. You will see examples of suchsystems (vibrating strings, air columns, etc.) inthe next chapter. Any mechanical structure, likea building, a bridge, or an aircraft may haveseveral possible natural frequencies. Anexternal periodic force or disturbance will setthe system in forced oscillation. If, accidentally,the forced frequency

    dhappens to be close to

    one of the natural frequencies of the system,the amplitude of oscillation will shoot up(resonance), resulting in possible damage. Thisis why soldiers go out of step while crossing abridge. For the same reason, an earthquake will

    not cause uniform damage to all building in anaffected area, even if they are built with thesame strength and materials. The naturalfrequencies of a building depend on its height,and other size parameters, and the nature ofbuilding materials. The one with its naturalfrequency close to the frequency of seismic wavein likely to be damaged more.

    SUMMARY

    1. The motions which repeat themselves are calledperiodic motions.

    2. Theperiod Tis the time required for one complete oscillation, or cycle. It is related tothe frequencyby,

    1T=

    assorted lengths suspended from a common ropeas shown in Fig. 14.22. The pendulums 1 and 4have the same lengths and the others have

    different lengths. Now let us set pendulum 1 intomotion. The energy from this pendulum getstransferred to other pendulums through theconnecting rope and they start oscillating. Thedriving force is provided through the connectingrope. The frequency of this force is the frequencywith which pendulum 1 oscillates. If we observethe response of pendulums 2, 3 and 5, they firststart oscillating with their natural frequenciesof oscillations and different amplitudes, but thismotion is gradually damped and not sustained.Their frequencies of oscillation gradually

    change and ultimately they oscillate with the

    Fig. 14.22 Five simple pendulums of different

    lengths suspended from a common

    support.

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    The frequencyof periodic or oscillatory motion is the number of oscillations perunit time. In the SI, it is measured in hertz :

    1 hertz = 1 Hz = 1 oscillation per second = 1s1

    3. In simple harmonic motion (SHM), the displacementx (t) of a particle from itsequilibrium position is given by,

    x(t) =Acos (t+ ) (displacement),

    in whichAis the amplitudeof the displacement, the quantity (t + ) is the phase of

    the motion, and is the phase constant. The angular frequency is related to theperiod and frequency of the motion by,

    2

    2T

    (angular frequency).

    4. Simple harmonic motion is the projection of uniform circular motion on the diameterof the circle in which the latter motion occurs.

    5. The particle velocity and acceleration during SHM as functions of time are given by,

    v(t) = Asin (t+ ) (velocity),

    a(t) = 2Acos (t+ )

    = 2x(t) (acceleration),

    Thus we see that both velocity and acceleration of a body executing simple harmonicmotion are periodic functions, having the velocityamplitudev

    m=A and acceleration

    amplitudeam

    =2A, respectively.

    6. The force acting simple harmonic motion is proportional to the displacement andis always directed towards the centre of motion.

    7. A particle executing simple harmonic motion has, at any time, kinetic energyK = mv 2 and potential energyU = kx 2. If no friction is present the mechanicalenergy of the system, E = K + Ualways remains constant even though Kand Uchangewith time.

    8. A particle of mass moscillating under the influence of a Hookes law restoring forcegiven byF = k xexhibits simple harmonic motion with

    k

    m= (angular frequency)

    2m

    T

    k

    (period)Such a system is also called a linear oscillator.

    9. The motion of a simple pendulum swinging through small angles is approximatelysimple harmonic. The period of oscillation is given by,

    2L

    Tg

    10. The mechanical energy in a real oscillating system decreases during oscillations because

    external forces, such as drag, inhibit the oscillations and transfer mechanical energyto thermal energy. The real oscillator and its motion are then said to be damped. If the

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    damping forceis given byFd

    = bv, where vis the velocity of the oscillator and b is adamping constant, then the displacement of the oscillator is given by,

    x(t) =Aebt/2m cos (t+ )

    where , the angular frequency of the damped oscillator, is given by

    2

    24

    bk

    m m

    If the damping constant is small then , where is the angular frequency of theundamped oscillator. The mechanical energyEof the damped oscillator is given by

    /1

    22 bt m E(t) kA e

    11. If an external force with angular frequencydacts on an oscillating system with natural

    angular frequency, the system oscillates with angular frequencyd. The amplitude of

    oscillations is the greatest when

    d =

    a condition called resonance.

    POINTS TO PONDER

    1. The period Tis the least timeafter which motion repeats itself. Thus, motion repeatsitself afternTwhere nis an integer.

    2. Every periodic motion is not simple harmonic motion. Only that periodic motiongoverned by the force lawF = k xis simple harmonic.

    3. Circular motion can arise due to an inverse-square law force (as in planetary motion)as well as due to simple harmonic force in two dimensions equal to: m2r. In thelatter case, the phases of motion, in two perpendicular directions (xand y) must differby /2. Thus, a particle subject to a force m2r with initial position (o,A) andvelocity (A, o) will move uniformly in a circle of radius A.

    4. For linear simple harmonic motion with a given two arbitrary initial conditions arenecessary and sufficient to determine the motion completely. The initial conditionmay be (i) initial position and initial velocity or (ii) amplitude and phase or (iii) energyand phase.

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    5. From point 4 above, given amplitude or energy, phase of motion is determined by theinitial position or initial velocity.

    6. A combination of two simple harmonic motions with arbitrary amplitudes and phasesis not necessarily periodic. It is periodic only if frequency of one motion is an integralmultiple of the others frequency. However, a periodic motion can always be expressedas a sum of infinite number of harmonic motions with appropriate amplitudes.

    7. The period of SHM does not depend on amplitude or energy or the phase constant.Contrast this with the periods of planetary orbits under gravitation (Keplers thirdlaw).

    8. The motion of a simple pendulum is simple harmonic for small angular displacement.

    9. For motion of a particle to be simple harmonic, its displacementxmust be expressiblein either of the following forms :

    x = Acos t + Bsin t

    x=Acos (t+ ), x= Bsin (t+ )

    The three forms are completely equivalent (any one can be expressed in terms of anyother two forms).

    Thus, damped simple harmonic motion [Eq. (14.31)] is not strictly simple harmonic. Itis approximately so only for time intervals much less than 2m/bwherebis the dampingconstant.

    10. In forced oscillations, the steady state motion of the particle (after the force oscillationsdie out) is simple harmonic motion whose frequency is the frequency of the drivingfrequency

    d, not the natural frequencyof the particle.

    11. In the ideal case of zero damping, the amplitude of simple harmonic motion at resonance

    is infinite. This is no problem since all real systems have some damping, however,small.

    12. Under forced oscillation, the phase of harmonic motion of the particle differs from thephase of the driving force.

    Exercises

    14.1 Which of the following examples represent periodic motion?(a) A swimmer completing one (return) trip from one bank of a river to the other

    and back.

    (b) A freely suspended bar magnet displaced from its N-S direction and released.(c) A hydrogen molecule rotating about its centre of mass.(d) An arrow released from a bow.

    14.2 Which of the following examples represent (nearly) simple harmonic motion andwhich represent periodic but not simple harmonic motion?(a) the rotation of earth about its axis.(b) motion of an oscillating mercury column in a U-tube.(c) motion of a ball bearing inside a smooth curved bowl, when released from a

    point slightly above the lower most point.(d) general vibrations of a polyatomic molecule about its equilibrium position.

    14.3 Fig. 14.23 depicts four x-tplots for linear motion of a particle. Which of the plotsrepresent periodic motion? What is the period of motion (in case of periodic motion) ?

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    Fig. 14.23

    14.4 Which of the following functions of time represent (a) simple harmonic, (b) periodicbut not simple harmonic, and (c) non-periodic motion? Give period for each case ofperiodic motion ( is any positive constant):(a) sin t cos t(b) sin3t(c) 3 cos (/4 2t)(d) cos t+ cos 3t+ cos 5t(e) exp ( 2t2)(f) 1 + t+ 2t2

    14.5 A particle is in linear simple harmonic motion between two points, A and B, 10 cmapart. Take the direction from A to B as the positive direction and give the signs ofvelocity, acceleration and force on the particle when it is(a) at the end A,(b) at the end B,(c) at the mid-point of AB going towards A,(d) at 2 cm away from B going towards A,(e) at 3 cm away from A going towards B, and(f) at 4 cm away from B going towards A.

    14.6 Which of the following relationships between the acceleration aand the displacementxof a particle involve simple harmonic motion?(a) a= 0.7x

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    (b) a= 200x2

    (c) a= 10x(d) a= 100x3

    14.7 The motion of a particle executing simple harmonic motion is described by thedisplacement function,

    x(t) =Acos (t+ ).

    If the initial (t= 0) position of the particle is 1 cm and its initial velocity is cm/s,what are its amplitude and initial phase angle ? The angular frequency of theparticle is s1. If instead of the cosine function, we choose the sine function todescribe the SHM : x = B sin (t+ ), what are the amplitude and initial phase of theparticle with the above initial conditions.

    14.8 A spring balance has a scale that reads from 0 to 50 kg. The length of the scale is 20cm. A body suspended from this balance, when displaced and released, oscillateswith a period of 0.6 s. What is the weight of the body ?

    14.9 A spring having with a spring constant 1200 N m1 is mounted on a horizontal

    table as shown in Fig. 14.24. A mass of 3 kg is attached to the free end of thespring. The mass is then pulled sideways to a distance of 2.0 cm and released.

    Fig. 14.24

    Determine (i) the frequency of oscillations, (ii) maximum acceleration of the mass,

    and (iii) the maximum speed of the mass.

    14.10 In Exercise 14.9, let us take the position of mass when the spring is unstreched asx = 0, and the direction from left to right as the positive direction ofx-axis. Give xas a function of time tfor the oscillating mass if at the moment westart the stopwatch (t= 0), the mass is(a) at the mean position,(b) at the maximum stretched position, and(c) at the maximum compressed position.In what way do these functions for SHM differ from each other, in frequency, inamplitude or the initial phase?

    14.11 Figures 14.25 correspond to two circular motions. The radius of the circle, theperiod of revolution, the initial position, and the sense of revolution (i.e. clockwiseor anti-clockwise) are indicated on each figure.

    Fig. 14.25

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    Obtain the corresponding simple harmonic motions of the x-projection of the radiusvector of the revolving particle P, in each case.

    14.12 Plot the corresponding reference circle for each of the following simple harmonic

    motions. Indicate the initial (t=0) position of the particle, the radius of the circle,and the angular speed of the rotating particle. For simplicity, the sense of rotationmay be fixed to be anticlockwise in every case: (xis in cm and tis in s).

    (a) x= 2 sin (3t+ /3)

    (b) x= cos (/6 t)

    (c) x= 3 sin (2t+ /4)

    (d) x= 2 cos t

    14.13 Figure 14.26 (a) shows a spring of force constantkclamped rigidly at one end anda mass mattached to its free end. A force Fapplied at the free end stretches thespring. Figure 14.26 (b) shows the same spring with both ends free and attached toa mass mat either end. Each end of the spring in Fig. 14.26(b) is stretched by thesame force F.

    Fig. 14.26

    (a) What is the maximum extension of the spring in the two cases ?

    (b) If the mass in Fig. (a) and the two masses in Fig. (b) are released, what is theperiod of oscillation in each case ?

    14.14 The piston in the cylinder head of a locomotive has a stroke (twice the amplitude)of 1.0 m. If the piston moves with simple harmonic motion with an angular frequencyof 200 rad/min, what is its maximum speed ?

    14.15 The acceleration due to gravity on the surface of moon is 1.7 m s2. What is the timeperiod of a simple pendulum on the surface of moon if its time period on the surfaceof earth is 3.5 s ? (gon the surface of earth is 9.8 m s2)

    14.16 Answer the following questions :(a) Time period of a particle in SHM depends on the force constantkand mass m

    of the particle:

    T

    m

    k= 2 . A simple pendulum executes SHM approximately. Why then isthe time period of a pendulum independent of the mass of the pendulum?

    (b) The motion of a simple pendulum is approximately simple harmonic for smallangle oscillations. For larger angles of oscillation, a more involved analysis

    shows that T is greater than 2l

    g. Think of a qualitative argument to

    appreciate this result.

    (c) A man with a wristwatch on his hand falls from the top of a tower. Does thewatch give correct time during the free fall ?

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    (d) What is the frequency of oscillation of a simple pendulum mounted in a cabinthat is freely falling under gravity ?

    14.17 A simple pendulum of length land having a bob of mass Mis suspended in a car.

    The car is moving on a circular track of radius Rwith a uniform speed v. If thependulum makes small oscillations in a radial direction about its equilibriumposition, what will be its time period ?

    14.18 A cylindrical piece of cork of density of base areaAand heighthfloats in a liquid ofdensity

    l.The cork is depressed slightly and then released. Show that the cork

    oscillates up and down simple harmonically with a period

    Th

    g1

    = 2

    where is the density of cork. (Ignore damping due to viscosity of the liquid).

    14.19 One end of a U-tube containing mercury is connected to a suction pump and the

    other end to atmosphere. A small pressure difference is maintained between thetwo columns. Show that, when the suction pump is removed, the column of mercuryin the U-tube executes simple harmonic motion.

    Additional Exercises

    14.20 An air chamber of volume Vhas a neck area of cross section ainto which a ball ofmass mjust fits and can move up and down without any friction (Fig.14.27). Showthat when the ball is pressed down a little and released , it executes SHM. Obtainan expression for the time period of oscillations assuming pressure-volume variationsof air to be isothermal [see Fig. 14.27].

    14.21 You are riding in an automobile of mass 3000 kg. Assuming that you are examiningthe oscillation characteristics of its suspension system. The suspension sags

    15 cm when the entire automobile is placed on it. Also, the amplitude of oscillationdecreases by 50% during one complete oscillation. Estimate the values of (a) thespring constantkand (b) the damping constantbfor the spring and shock absorbersystem of one wheel, assuming that each wheel supports 750 kg.

    14.22 Show that for a particle in linear SHM the average kinetic energy over a period ofoscillation equals the average potential energy over the same period.

    14.23 A circular disc of mass 10 kg is suspended by a wire attached to its centre. The wireis twisted by rotating the disc and released. The period of torsional oscillations isfound to be 1.5 s. The radius of the disc is 15 cm. Determine the torsional springconstant of the wire. (Torsional spring constant is defined by the relation

    J= , whereJis the restoring couple and the angle of twist).

    Fig.14.27

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    14.24 A body describes simple harmonic motion with an amplitude of 5 cm and a period of0.2 s. Find the acceleration and velocity of the body when the displacement is(a) 5 cm (b) 3 cm (c) 0 cm.

    14.25 A mass attached to a spring is free to oscillate, with angular velocity, in a horizontalplane without friction or damping. It is pulled to a distance x

    0and pushed towards

    the centre with a velocityv0at time t= 0. Determine the amplitude of the resulting

    oscillations in terms of the parameters , x0

    and v0. [Hint : Start with the equation

    x= acos (t+) and note that the initial velocity is negative.]