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In the h
o S 1 h 2 << 1. Here the adjustment distance is the inverse of the
galvanic parameter:
interval
S 1 R 2 =
1
g
d
=
(7
.
33)
Considering a model with continuous change of the conductance S 1 , we assume
that intensity of the S -effect depends on relation between generation of excess cur-
rent in the upper layer and its leakage into the underlying intermediate layer. To
gain a better insight into this mechanism, we examine a two-dimensional model
suggested by Kuznetsov (2005). Letting
2
L
S 1 ( y )
=
S 1 +
S o cos ly
l
=
S o < S 1 ,
(7
.
34)
we turn to the initial equation (7.18) and write for the h -interval:
d 2
dy 2 S 1 ( y ) Z ( y )
Z ( y )
R 2
=
i
o h
,
(7
.
35)
where Z ( y ) is represented as a Fourier decomposition
Z ( y )
=
a n cos nly
.
(7
.
36)
o
Substituting (7.36) in (7.35) and taking into account that
1
2 [cos(1
cos ly cos nly
=
+
n ) ly
+
cos(1
n ) ly ]
,
we have
S 1
n ) ly ]
d 2
dy 2
1
2 S o
R 2
a n cos nly
+
a n [cos(1
+
n ) ly
+
cos(1
o
o
(7
.
37)
a n cos nly
=
i
o h
,
o
from which
S 1
1
2 S o
l 2 R 2
a n n 2 cos nly
n ) 2 cos(1
+
a n [(1
+
+
n ) ly
o
o
n ) ly ]
n ) 2 cos(1
+
(1
+
a n cos nly
+
i
o h
=
b n cos nly
=
0
.
o
o
.
(7
38)
 
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