PSI - Issue 3
Christos F. Markides et al. / Procedia Structural Integrity 3 (2017) 334–345 Christos F. Markides, Stavros K. Kourkoulis / Structural Integrity Procedia 00 (2017) 000–000
337
4
2
2
2
11 x 12 y 12 x 22 y 66 xy 2 2 x y y x
(4)
0
xy dS dS dy dx
xy dS dS dx dy
or, with xy 0 on L, simply as
(5a)
X
, Y
n
x
n
y
n n r X cos , Y sin (5b) In the above formulae u, v are the components of the displacement, β ij are the so-called reduced elastic constants, X n , Y n are the components of the stress vector acting at the point z(x,y)=z(R,θ) on L from the side of the outer normal unit vector n and S is the arc length on L; in addition, for the orthotropic disc considered here it holds that: r
2
2
1
1
1
(6)
yx
yz
yz
,
,
z E ,
66
zx
11
12
zx
22
2 y
E E
E
E
E
G
E
x
z
y
y
y
xy
where E x , E y , E z are Young’s moduli along the respective directions, G xy is the shear modulus in xy-plane and ν ij , i,j=x, y, z, is Poisson’s ratio ruling contraction/dilatation in j-direction for tension/compression in i-direction. As usual, Eqs.(3) imply the existence of the Airy stress function F(x,y) so that:
2
2
2
F
F
F
(7)
,
,
x
y
xy
2
2
y
x
x y
Substitution in Eq.(4) from Eqs.(7), yields the “generalized” biharmonic differential equation in F: 4 4 4 22 12 66 11 4 2 2 4 F F F 2 0 x x y y Its associated characteristic equation with its four imaginary roots, the so-called complex parameters, read as: 4 2 11 12 66 22 2 0 (9) (8)
(10)
i , i
1 i ,
2 i ,
1
2
3
1
1
4
2
2
where the overbar denotes the complex conjugate and for the parameters β 1 and β 2 it holds that:
2
12 2
2
4
1 2
(11)
66
12
66
11 22
,
1
2
2
11
Then, following Lekhnitskii (1981), F is here expressed with the aid of two functions of the so-called complicated complex variables z 1 =x+μ 1 y and z 2 =x+μ 2 y, as ( denotes the real part): 11 1 12 2 F x, y 2 F z F z (12) with Lekhnitskii’s general complex potentials given as (prime denotes first derivative): 1 1 11 1 2 2 12 2 z F z , z F z (13) The displacement components are then given as (Lekhnitskii 1981): 1 1 1 2 2 2 1 1 1 2 2 2 u 2 p z p z , v 2 q z q z (14) where 2 2 1 11 1 12 2 11 2 12 1 12 1 22 1 2 12 2 22 2 p , p , q , q (15) Concerning Φ 1 and Φ 2 , they are here sought in the form proposed by Lekhnitskii (1968) for circular regions, as:
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