Page 253 - Intro to Tensor Calculus
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Additional Symmetries
If the material (crystal) is such that there is an additional plane of symmetry, say the x 2 -x 3 plane, then
reversal of the x 1 axis should leave the equations (2.4.14) unaltered. If there are two planes of symmetry
then there will automatically be a third plane of symmetry. Such a material (crystal) is called orthotropic.
Introducing the additional transformation
x 1 = −x 1 , x 2 = x 2 , x 3 = x 3
which represents the reversal of the x 1 axes, the expanded form of equations (2.4.9) are used to calculate the
effect of such a transformation upon the stress and strain tensor. We find σ 1 ,σ 2 ,σ 3 ,σ 6 ,e 1 ,e 2,e 3 ,e 6 remain
unchanged while σ 4 ,σ 5 ,e 4 ,e 5 change sign. The equation (2.4.14) then becomes
e 1 s 11 s 12 s 13 s 14 0 0 σ 1
s 21 s 22 s 23 s 24 0
e 2 0 σ 2
s 31 s 32 s 33 s 34 0
. (2.4.15)
e 3 0 σ 3
=
s 41 s 42 s 43 s 44 0
−e 4 0 −σ 4
−e 5 0 0 0 0 s 55 s 56 −σ 5
e 6 0 0 0 0 s 65 s 66 σ 6
Note that if the constitutive equations (2.4.14) and (2.4.15) are to produce the same results upon reversal
of the x 1 axes, then we require that the following coefficients be equated to zero:
s 14 = s 24 = s 34 =0
s 41 = s 42 = s 43 =0
s 56 = s 65 =0.
This then produces the constitutive equation
0 0 0
e 1 s 11 s 12 s 13 σ 1
0 0
s 21 s 22 s 23
e 2 0 σ 2
0 0
s 31 s 32 s 33
e 3 0 σ 3 (2.4.16)
0 0 0 0
=
e 4 s 44 0 σ 4
e 5 0 0 0 0 s 55 0 σ 5
e 6 0 0 0 0 0 s 66 σ 6
or its equivalent form
σ 1 c 11 c 12 c 13 0 0 0 e 1
c 21 c 22 c 23 0 0
σ 2 0 e 2
c 31 c 32 c 33 0 0
σ 3 0 e 3
0 0 0 c 44 0
=
σ 4 0 e 4
σ 5 0 0 0 0 c 55 0 e 5
σ 6 0 0 0 0 0 c 66 e 6
and the original 36 constants have been reduced to 12 constants. This is the constitutive equation for
orthotropic material (crystals).