
The 1-D
Continuous-Time Fourier Transform
275
As the period approaches infinity, the individual magnitudes approach zero
still maintaining the same relative variations of the magnitudes. The fre-
quency increment between adjacent frequency components tends to zero
and, hence, the spectrum becomes continuous. The envelopes of the spec-
tra shown in Figs. 13.2(a), (c), and (e) are the magnitude of the FT of
the signal shown in Fig. 13.1 with an infinite period, with different scale
factors. The envelopes of the spectra shown in Figs. 13.2(b), (d), and (f)
are the magnitude of the FT of the pulse shown in Fig. 13.1 with an infinite
period (These spectra are the same as those on the left side of Fig. 13.2
except that the magnitudes are multiplied by the period.).
One difference between the FS and the FT is that the FS gives the
amplitudes of the various sinusoidal components. The amplitudes of the si-
nusoidal components of an aperiodic signal tend to zero. However, the limit
of the product of the period of the signal (as the period approaches infinity)
and the infinitesimal amplitudes of the spectral components yields a finite
continuous curve, representing the spectral density. That is, the FT yields
a relative amplitude spectrum. Although the FT yields the spectral density
of a signal, it is still called the spectrum. Essentially, there is no significant
difference between the FS and FT and the continuous spectrum of the FT
is used in the same way as the discrete spectrum of the FS in applications.
Remember that the relative variations of the amplitudes of the various fre-
quency components determine the essential characteristics of a spectrum.
The FS coefficients of a periodic signal can be easily deduced from the FT
of the corresponding aperiodic signal as shown in Example 13.5, since the
FS coefficients are samples of the FT at discrete intervals of ^, apart from
the constant multiplier y. This argument can be mathematically put as
follows. Substituting for
X
cs
(k)
with ^ replaced by |£ in (12.2), we get
°° u
r
ti+T
;(t) = Y
e
J^ot{ o /
x
(l)e-
jkuol
dl}
t
™
2n
Jti
As T tends to oo,
kuiQ
becomes a continuous variable
LJ,
^ = wo tends to a
differential dw, and the summation becomes an integral. Therefore, we get
^{ir- / x{l)e-
iu,
dl] = £- / { / x(l)e-
jul
dl}e
jut
cLj
-oo
i7r
J-oo to J-oo J-oo
i r°°