Mechanical Engineering Principles

(Dana P.) #1

17


Simple harmonic motion


At the end of this chapter you should be
able to:


  • understand simple harmonic motion

  • determine natural frequencies for simple
    spring-mass systems

  • calculate periodic times

  • understand the motion of a simple
    pendulum

  • understand the motion of a compound
    pendulum


17.1 Introduction


Simple harmonic motion is of importance in a num-
ber of branches of engineering and physics, includ-
ing structural and machine vibrations, alternating
electrical currents, sound waves, light waves, tidal
motion, and so on.


17.2 Simple harmonic motion (SHM)


A particle is said to be under SHM if its accel-
eration along a line is directly proportional to its
displacement along that line, from a fixed point on
that line.
Consider the motion of a particleA, rotating in a
circle with a constant angular velocityω, as shown
in Figure 17.1.
Consider now the vertical displacement ofAfrom
xx, as shown by the distanceyc.IfPis rotating at
a constant angular velocityωthen the periodic time
Tto travel an angular distance of 2π, is given by:


T=

2 π
ω

( 17. 1 )

Letf=frequency of motionC(in Hertz), where


f=

1
T

=

ω
2 π

( 17. 2 )

0

yc

c

y

−y

A

B

vA

vAsinq
vAcosq

w

−xxr

r
q

Displacement (yc)
Accelration (−ac)
Velocity (vc)

time't'

(a) (b)

Figure 17.1

To determine whether or not SHM is taking place,
we will consider motion ofAin the directionyy.
NowyC=OAsinωt,

i.e., yc=rsinωt ( 17. 3 )

wheret=time in seconds.
Plotting of equation (17.3) againsttresults in the
sinusoidal variation for displacement, as shown in
Figure 17.1(b).
From Chapter 11,vA = ωr, which is the tan-
gential velocity of the particleA. From the veloc-
ity vector diagram, at the pointAon the circle of
Figure 17.1(a),

vC=vAcosθ=vAcosωt ( 17. 4 )

Plotting of equation (17.4) againsttresults in the
sinusoidal variation for the velocityvC, as shown in
Figure 17.1(b).
The centripetal acceleration ofA

=aA=ω^2 r

Now aC=−aAsinθ

Therefore, aC=−ω^2 rsinωt ( 17. 5 )

Plotting of equation (17.5) againsttresults in the
sinusoidal variation for the acceleration atC,aC,as
shown in Figure 17.1(b).
Substituting equation (17.3) into equation (17.5)
gives:

aC=−ω^2 yC ( 17. 6 )
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