Geology Reference
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Figure 4. A schematic of the generalized Maxwell
model
A typical transformation of nodal parameters
to the global coordinate system is used. The dis-
placements of the damper's external nodes are
transformed as usual but the internal variables of
the damper are still defined in the local coordi-
nate system. This means that the transformation
matrix is:
T 0
0
d
T
=
(14)
d
I
where
T 0
0 T
c s
s c
T =
T
d =
,
(15)
c = cos β , s = sin β , β is the angle between the
global and the local coordinate systems and I is
the (
damping matrices given in the local coordinate
system, respectively.
The equilibrium conditions of the internal
nodes, i.e., u
m × identity matrix.
The equation of the considered model, written
in the global coordinate system, has the form:
)
( )
t
u t
( )
=
0
for i
= 1, .., lead
m
i
1
1
to the following matrix equation:
R
t
K q
t
+
C q
t
( )
=
( )
( )
(16)
d
d
d
d
d
=
(11)
K q
t
+
K q
t
+
C q
t
+
C q
t
0
( )
( )
( )
( )
wz
z
ww w
wz
z
ww w
where
where  
,  
T
T
R
( )
t
=
[
R
( ),
t
0
]
=
T R T
,
= .
The equation of the generalized Kelvin model
written in the local coordinate system can be finally
presented in the form:
T
K K
wz
=
C C
wz
d
z
d
d
d
zw
zw
T
R z
( )
t
=
[
R t R t R t R t
( ),
( ),
( ),
( )] ,
1
2
3
4
T
T
q
( )
t
=
[
q
( ),
t
q
( )
t
=
q
( )]
t
=
T q T
,
d
z
w
w
d
d
d
T
q z
( )
t
=
[ ( ),
q t
q t
( ),
q t
( ),
q t
( )]
1
2
3
4
R
t
=
K q
t
+
C q
t
(12)
( )
( )
( )
d
d
d
d
d
are the vector of nodal reactions and the vector
of nodal parameters, respectively, written in the
global coordinate system. The explicit forms of
matrices K d and C d are given in Appendix A.
The equation of the generalized Maxwell
model could be derived in a similar way. In the
global coordinate system the equation mentioned
above has the form of Equation (16) though with
the matrices K d and C d as given in Appendix A.
T
w h e r e
R
( )
t
=
[
R
( ),
t
0
]
,
d
z
T
q
( )
t
=
[
q
( ),
t
q
( )]
t
,
d
z
w
 
 
 
 
K K
K K
C C
C C
zz
zw
zz
zw
K
=
,
C
=
(13)
d
d
wz
ww
wz
ww
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