Geology Reference
In-Depth Information
Figure 10. Stiffness of two-way asymmetric system (Chopra 2000)
where M is the seismic mass matrix of the
20-story building and b and d are the distances of
structural plan of the NS- and EW-directions,
respectively. Finally, the governing equation of
motion is
output, y r is the vector of regulated responses, v
is a measurement noise vector, and C r , D r , and F r
depend on the sensor locations and the number of
actuators and locations, and
0
I
,
(23)
ndof ndof
×
ndof ndof
×
A
=
M x +C

x + K

x =
M
1
K
M
1
C
3D20s
3D20s
3D20s
3D20s
3D20s
ndof ndof
×
3D20s
3
D20s ndof ndof
×
(19)
- M G
x g
+ P
f
3D20s
3D20s
3D20s 3D20
s
0
where K 3D20s (60x60) is the global stiffness ma-
trix, M 3D20s (60x60) is the global mass matrix,
C 3D20s (60x60) is the global damping matrix that
is defined by 2% proportional Rayleigh damping,
G 3D20s is ground motion matrix, P 3D20s is a loca-
tion vector of the control device forces, and f 3D20s
is the control force input. The 2 nd order differen-
tial equations can be transformed into the 1 st order
state space equations
ndof ndof
×
B
=
,
(24)
-1
M
f
3D20s
a
ndof ndof
×
I
0
ndof ndof
×
ndof ndof
×
,
C
=
0
I
m
3 3
×
ndof ndof
×
1
1
M
K
M
C
3D20s
3D20s
ndof
×
ndof
3D20s
3D20s
ndof ndof
×
(25)
0
0
ndof ndof
×
D
=
,
(26)
m
ndof ndof
×
x =
Ax Bf
+
+
E x g

(20)
1
f M
(
)
a
3D20s
ndof ndof
×
y
=
C x D f
+
+
F
x g
+
v
(21)
0
G 3D20s
m
m
m
m
ndof
×
1
E
=
,
(27)
ndof
1
×

x g
y
=
x +C x D f
+
+
F
(22)
r
r
r
r
where x is the state vector, f is control force input,
y m is the vector corresponding to the measured
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