Issue 42
J.-M. Nianga et alii, Frattura ed Integrità Strutturale, 42 (2017) 280-292; DOI: 10.3221/IGF-ESIS.42.30
1 j y
0 0
1 1
0 0
0
0
(
(
(
)
)
)
dx
dx
dx
ij
ij
ij
x
x
x
y
x
j
i
j
i
i
0 k
0 k
1
1 1
0 0
1 1
(
(
(
u x
u
)
)
)
dx e
ij
dy
e
dx
ikl
ikl
i y
y
y
x
xl
(59)
j
i
l
i
1 k u l y
1 k
0 0
1 1
(
(
u
)
)
0 1 0; , ( ) H
1 0
dx e
dy
e
i
kl
ikl
x
y
y
i
l
i
with represents the operator average defined on any Y-periodic function f(y) by:
1
f
( ) f y dy YY
(60)
In the particular case where 1 1
1 1 , v u and
we get:
0 0
(
0 k 0 1 1 , v v ( ( )) H ijkl l l a 0 1 , ( ) ij j j x y H 3 0 u u x y 0 1 1 k
0 0
v u
)
0
1
(
v u
x y
)
j
j
i
i
dx e
dx
0;
ijk
(61)
x
x
i
k
k
j
0 k u u x y 1 k
0 0
0 0
(
(
)
)
dx e
dx
0;
ikl
(62)
x
x
i
l
l
i
1 0
Consequently, the corresponding homogenized equations in which there are no more fissures then follow:
0 ij j x
0
(63)
0 k u u x y 1 k l l
0
1
0
a
e
ij
ijkl
ijk
x y
k
k
and
i i D x
0
0
(64)
0 k u u x y 1 k l l
0
1
D
0
e
i
ij
ikl
xj y
j
287
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