
100 4 System Response Analysis
Comparing the outputs for G1 and G2, note that although they have poles with
the same imaginary part, oscillations for G1 are pretty remarkable since the
oscillations still remain after 5 seconds. G2, on the contrary, is quicker than G1
due to the difference of magnitude of the real part of the poles. This leads us to
remember that the effect of poles far away from the ordinate axis of the s-plane is
ephemeral. On the other hand, the responses of G1, G3, and G4 are good examples
to realize the effect of the imaginary part of the poles in the amplitude of the
oscillations. Systems with poles at the same real position but different imaginary
components produces oscillations with different amplitude, including the absence
of oscillation when no imaginary poles are considered (G4).
Second-Order System Response through a Geometrical Representation
Although the analysis and the representation used in the previous development is
sufficient for understanding the behavior of second-order systems, a different
representation oriented to geometrical variables is widely employed. The intuitive
expression (4.29) is replaced with the more intriguing one given in (4.30).
(4.29)
(4.30)
Since they are both equivalent, it is clear that
(4.31)
In this representation, K is the gain of the system, is called the natural
frequency and is known as damping ratio. The roots of the characteristic
equation (the poles of the system) can be obtained involving these variables as:
(4.32)
Where is called the damped frequency since it relates the damping ratio and the
natural frequency.
Geometrically these variables are represented in the fig.
4.11.
Trigonometrically it can be derived that the magnitude of the complex poles
corresponds to and the phase, α, is , i.e.
. Thus, given a
second-order system expressed as in (4.30) one can guess the position of its poles
0
2
10
()
b
Gs
sasa
=
++
2
22
()
2
n
nn
K
Gs
ss
ω
ωω
=
++
2
0
n
Kb
ω
=
1
2
n
a
ω
=
2
0
n
a
ω
=
n
ω
2
12
,1
nn d
ss j j
ωω
σω
=− ± − =− ±
d
ω
n
ω
1
cos ( )
−
cos( )
α
=