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Download full text - ELSA - Europa

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Time integration<br />

Each time increment is split into three phases:<br />

v<br />

w<br />

1. Explicit Lagrangian phase: by posing<br />

. w=<br />

v all transport terms vanish<br />

2. Implicit Lagrangian phase (see details<br />

below) whereby the pressure is<br />

iteratively refined (this stabilizes the<br />

solution)<br />

3. Convective flux phase whereby<br />

the transport term contributions<br />

are added<br />

• This scheme is not as limpid as the purely Lagrangian one.<br />

Second-order accuracy guaranteed only for phase 1.<br />

Λ<br />

v<br />

Λ p ← f( p)<br />

Λ<br />

w<br />

15<br />

Time integration (2)<br />

n+ 1/2 n−1/2<br />

0. First compute v = v +∆ta n , where:<br />

F old t<br />

momentum transport forces at the end of<br />

previous step<br />

n<br />

Fp<br />

pressure forces<br />

n<br />

F b<br />

body forces<br />

n<br />

F s<br />

a<br />

n<br />

F + F + F + F<br />

=<br />

M<br />

old n n n<br />

t p b s<br />

surface forces<br />

1. Obtain new “Lagrangian” configuration:<br />

x = x +∆t⋅v +<br />

L n n 1/2<br />

2. Evaluate L-volume and L-density (mass M is constant!):<br />

L L L<br />

L n L<br />

V = V ( x ) ρ = M / V<br />

3. From the internal energy eqn. without the transport term, using the<br />

divergence theorem:<br />

d<br />

( ρ iV ) =− ( p + q) v ndS<br />

dt<br />

∫ i<br />

S<br />

pseudo-viscous pressure<br />

16<br />

8

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