DHARM
824 GEOTECHNICAL ENGINEERING
z
z
D
D
1
2 2
2
1
=
−
F
H
GG
I
K
exp JJ
π
...(Eq. 20.37)
‘Logarithmic Decrement’ is defined as
δ = ln
z
z
D
D
1
2 2
2
1
=
−
π
...(Eq. 20.38)
In words, logarithmic decrement is defined as the natural logarithm of the ratio of any
two successive amplitudes of same sign in the decay curve obtained in free vibration with
damping.
δ is approximately 2πD, when D is small. Eq. 20.38 also indicates that, in viscous damp-
ing, the ratio of amplitudes of any successive peaks is a constant. It follows that the logarith-
mic decrement may be obtained from any two peak amplitudes z 1 and z1+n from the equation
δ =
(^11)
n 1
z
z n
ln
- ...(Eq. 20.39)
20.2.9 Forced Vibrations with Damping
A system which undergoes forced vibrations, and in which viscous damping is present, may be
analysed by the Mass-spring-dashpot model shown in Fig. 20.13.
k c
P sin to w
Fig. 20.13 Forced vibration with damping
The equation of motion for this system may be written as follows:-
Mz cz kz.&&++.&. = Po sin ωt ...(Eq. 20.40)
This may be rewritten as
&&z c.& .sin
M
z k
M
z
P
M
++= ωo t ...(Eq. 20.41)
or &&&zz z sin
P
M
++n^2 =αωo t ω ...(Eq. 20.42)
where α =
c
M
and ωn^2 =
k
M
.
The particular solution is a steady state harmonic oscillation having a frequency equal
to that of the excitation, and the displacement vector lags the force vector by some angle. Let
us therefore assume that the particular solution is
z = A sin (ωt – φ) ...(Eq. 20.43)