Geology Reference
In-Depth Information
0
0
0
0
0
0
0
0
m
m
C
zz
=
∑
∑
(A.7)
0
0
c
2
c
cs
c
i
i
i
1
i
1
=
=
m
m
∑
∑
0
0
cs
c
s
2
c
i
i
i
=
1
i
=
1
−
ck
−
ck
.....
−
ck
.......
−
ck
1
2
i
m
−
sk
−
sk
.....
−
sk
.......
−
sk
T
1
2
i
m
K K
zw
=
=
(A.8)
zw
0
0
.......
0
.......
0
0
0
.......
0
.......
0
0
0
.......
0
.......
0
0
0
.......
0
.......
0
C C
zw
=
T
=
(A.9)
zw
−
cc
−
cc
.....
−
cc
i
.......
−
cc
1
2
m
2
.....
.......
−
sc
−
sc
−
sc
−
sc
1
i
m
(
)
(
)
diag k
,
k
, ..........,
k
, ,
diag c
,
c
, ..........,
c
,
K K
ww
=
=
C C
ww
=
=
(A.10)
ww
1
2
m
ww
1
2
m
The explicit form of the vectors and matrices used to describe the simple Kelvin model and the
fractional-derivative Kelvin model of a VE damper is:
T
q
( )
t
=
q
( )
t
=
[ ( ),
q t
q t
( ),
q t
( ),
q t
( )]
(A.11)
d
z
1
2
3
4
2
2
2
2
c
cs
−
c
−
cs
c
cs
−
c
−
cs
2
2
2
2
cs
s
−
cs
−
s
cs
s
−
cs
−
s
C C
d
=
=
c
K K
d
=
=
k
,
zz
1
−
c
2
−
cs
c
2
cs
zz
1
−
c
2
−
cs
c
2
cs
cs
s
2
cs
s
2
cs
s
2
cs
s
2
−
−
−
−
(A.12)
The explicit form of the matrices used to describe the simple Maxwell model and the fractional
Maxwell model of a VE damper is:
T
q
( )
t
=
[
q
( ),
t
q
( )]
t
(A.13)
d
z
w
T
T
q
z
( )
t
=
[ ( ),
q t
q t
( ),
q t
( ),
q t
( )] ,
q
w
( )
t
=
[
q
( )]
t
(A.14)
1
2
3
4
w
,
1
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