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Optimization and Computational Fluid Dynamics - Department of ...

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5 Efficient Deterministic Approaches for Aerodynamic Shape <strong>Optimization</strong><br />

�<br />

139<br />

δI(X,w,Z)= δi(X,w,Z)dV<br />

V<br />

V<br />

� �<br />

∂i(X,w,Z)<br />

=<br />

δX +<br />

∂X<br />

∂i(X,w,Z)<br />

δw +<br />

∂w<br />

∂i(X,w,Z)<br />

�<br />

δZ dV .(5.49)<br />

∂Z<br />

The derivation is identical to what has already been seen, <strong>and</strong> gives the<br />

adjoint equations<br />

� � �<br />

∂i ∂R ∂S<br />

+ ψT + φT dV =0, (5.50)<br />

∂w ∂w ∂w<br />

V<br />

�<br />

For the gradient we get<br />

V<br />

V<br />

� �<br />

∂i ∂R ∂S<br />

+ ψT + φT dV =0. (5.51)<br />

∂Z ∂Z ∂Z<br />

δI(X,w,Z)=<br />

� � �<br />

∂i(X,w,Z) T ∂R(X,w,Z) T ∂S(X,w,Z)<br />

δX + ψ δX + φ δX dV (5.52)<br />

∂X<br />

∂X<br />

∂X<br />

It can be shown that Eq. (5.50) is equivalent to the equation<br />

� ��∂ψ�T ∂F<br />

∂ξ ∂w +<br />

� � �<br />

T<br />

∂ψ ∂G<br />

dV = 0 (5.53)<br />

∂η ∂w<br />

V<br />

<strong>and</strong> the boundary condition (in the case <strong>of</strong> the drag)<br />

ψ2nx + ψ3ny + nx cos(α)+ny sin(α) − n T φ =0. (5.54)<br />

Note that the structural adjoint variables appear only in the boundary condition<br />

(5.54), while the adjoint flow equation (5.53) is unchanged. This implies<br />

that in order to implement the coupling, only the boundary condition treatment<br />

in the FLOWer code has to be modified. Equation (5.42) represents<br />

the structural adjoint equation <strong>and</strong> its boundary conditions. The structural<br />

equation reads in the case <strong>of</strong> linear elasticity<br />

S(X,w,Z)=K · Z − a = 0 (5.55)<br />

where K is the symmetric stiffness matrix <strong>and</strong> a is the aerodynamic force.<br />

The derivative ∂S<br />

∂Z in (5.42) can thus be replaced by K <strong>and</strong> the product φT K<br />

by Kφ. In this way, the same solver can be used for the structural direct <strong>and</strong><br />

adjoint equation, with different boundary conditions, given by the first <strong>and</strong><br />

second term in Eq. (5.42). The first term is reduced to a surface integral by

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