20 L.A. Aghalovyan
correlations of thermoelasticity
θασσσσσσ
θασσσσσσ
23464544342414
332211321
11161514131211
v
),,;,,;,v,;,,(
++++++=
∂
∂
+
∂
∂
++++++=
∂
∂
xyxzyzzzyyxx
iii
xyxzyzzzyyxx
aaaaaa
zy
w
aaaaaawuzyx
aaaaaa
x
u
),,;6,5,4;,,;,,(
121323
ααα
wvuzyx
(38)
Satisfying the boundary conditions
),(),,(),,(v),,(v),,(),,( yxwhyxwyxhyxyxuhyxu
−−−
=−=−=−
(39)
),(),,(),,(),,(),,(),,( yxhyxyxhyxyxhyx
zzzzyzyzxzxz
+++
===
σσσσσσ
(40)
or
),(),,(),,(v),,(v),,(),,( yxwhyxwyxhyxyxuhyxu
+++
===
(41)
and the conditions on the lateral surface, which for now are considered to be
arbitrary.
In the equations (37), (38) passing to dimensionless coordinates and displace-
ments
AAAAA /,/v,/,/,/,/ wWVuUhzyx ======
, we
again obtain singularly perturbed by small parametre
A/h=
system, the solu-
tion of which has the form of (1), but, for
int
I asymptotics (4), (33) is not admis-
sible, which indicates inapplicability of the hypotheses of classical theory for the
solution of the above formulated problems. For their solution asymptotics is
applicable
0,1
,v,
=−=
wu
qq
ij
σ
(42)
Substituting the representation (4), (42) into transformed system (37), (38) we get
a recurrent system for determining
),,(
)(
ζηξ
s
Q . The solution of this system
will contain six arbitrary functions, which are uniquely determined from condi-
tions (39), (40) or (39), (41).
This class of problems differs from classical by this, too, as the solution
int
I
becomes fully known. Rising residual on the lateral surface is removed by the so-
lution for the boundary layer, which does not influence on the solution of the inner
problem any more. If the functions ),( yxQ
±
entering conditions (39)-(41) are
polynomials, the iteration process cuts off and we obtain a mathematically precise
solution of the inner problem (solution for layer).
We derive it for the plate with general anisotropy, corresponding the problem
(39), (40), when
constwu
zzyzxz
====
+++−−−
σσσ
,,,0v :