Geology Reference
In-Depth Information
APPENDIX A
Finite Element Matrices of Different VE Damper Models
The explicit form of the matrices used to describe the generalized Kelvin model is given by:
K K
K K
C C
C
T
zz
zw
T
zz
zw
K
=
T K T
=
,
C
=
T C T
=
(A.1)
d
d
d
d
d
d
d
d
C
wz
ww
wz
ww
c k
2
csk
0
0
0
0
0
0
0
0
0
0
0
0
csk
s k
2
0
0
, C zz
=
K zz
=
0
0
(A.2)
0
0
c c
2
csc
2
0
0
c k
csk
m
m
m
m
0
0
csc
csc
2
0
0
csk
s k
m
m
m
m
0
0
.....
0
.......
0
ck
sk
0
.....
0
.......
0
0
0
0
.....
0
.......
0
0
.....
0
.......
0
T
T
0
, C C
=
=
K K
zw
=
=
(A.3)
zw
wz
0
0
..... .....
..... .....
0
cc
sc
wz
0
0
..... .....
..... ......
0
ck
sk
m
m
0
0
0
0
0
0
m
m
(
)
(
)
K K
ww
=
=
diag k
,
k
, ..........,
k
, ,
C C
ww
=
=
diag c
,
c
, ..........,
c
,
(A.4)
ww
1
2
m
ww
1
2
m
where c = cos β , s = sin β , β is the angle between the global and the local coordinate systems
The explicit form of the matrices used to describe the generalized Maxwell model is given by:
K K
K K
C C
C
T
zz
zw
T
zz
zw
K
=
T K T
=
,
C
=
T C T
=
(A.5)
d
d
d
d
d
d
d
d
C
wz
ww
wz
ww
m
m
2
2
c
k
+
k
cs k
+
k
c k
csk
0
i
0
i
0
0
i
=
1
i
=
1
m
m
2
2
cs k
+
k
s
k
+
k
csk
s k
K zz
=
(A.6)
0
i
0
i
0
0
i
=
1
i
=
1
2
2
c k
c
sk
c k
csk
0
0
0
0
2
2
csk
s k
csk
s k
0
0
0
0
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