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Download full text - ELSA - Europa

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Geometric non-linearities<br />

A large-displacement large-strain formulation is adopted<br />

for <strong>full</strong> generality. For continuum-like FE:<br />

• Compute spatial velocity gradient:<br />

L=∂x<br />

/ ∂x<br />

• Use additive decomposition to separate instantaneous<br />

deformation (symmetric) from rotation (antisymmetric part):<br />

L= D+<br />

W<br />

1 (<br />

T<br />

D = L + L ) ( stretching i.e. rate of deformation)<br />

2<br />

1 (<br />

T<br />

W = L−L ) ( spin i.e. rate of rotation)<br />

2<br />

• We obtain then:<br />

ε = D ; ∆ ε = D⋅∆t<br />

25<br />

Geometric non-linearities (2)<br />

For a continuum element the state of stress of interest to us,<br />

Cauchy stress σ , is referred to a fixed frame in space.<br />

Consequently, its time derivative is not invariant with<br />

respect to rotation: σ is not objective.<br />

• An objective rate of stress σˆ may be obtained under the<br />

form: ˆ σ = σ − Aσ + σA<br />

where A is an appropriate<br />

vorticity matrix.<br />

• In the Zaremba-Jaumann-Noll formulation:<br />

(other choices are possible, e.g. Green-Naghdi).<br />

A<br />

W<br />

• However, the above considerations are valid only in an<br />

infinitesimal sense, while we need to use finite increments.<br />

26<br />

13

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