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Partial Differential Equations - Modelling and ... - ResearchGate

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18 V. Girault <strong>and</strong> M.F. Wheeler<br />

5 DG Approximation of a Convection-Diffusion Equation<br />

Consider the convection-diffusion equation combining (24) <strong>and</strong> (15) in the<br />

domain Ω of the previous sections:<br />

− div(K∇c)+u ·∇c = f, in Ω, (51)<br />

K∇c · n Ω =0, on ∂Ω, (52)<br />

where f belongs to L 2 0(Ω), the tensor K satisfies the assumptions listed in<br />

Section 3 <strong>and</strong> u satisfies (16):<br />

div u =0 inΩ,<br />

u · n Ω =0 on∂Ω.<br />

This problem has a solution c ∈ H 1 (Ω), unique up to an additive constant<br />

under mild restrictions on the velocity u, for instance, when u belongs to<br />

H 1 (Ω) d . We propose to discretize it with a DG method when u is replaced<br />

by the solution u h ∈ X h of a flow problem that satisfies b h (u h ,q h ) = 0 for all<br />

q h ∈ M h :<br />

∑<br />

q h div u h dx −<br />

∑ ∫<br />

{q h } e [u h ] e · n e dσ =0.<br />

E∈E h<br />

∫E<br />

For an integer l ≥ 1, we define<br />

e∈Γ h ∪∂Ω<br />

e<br />

Y h = {c ∈ L 2 (Ω) :∀E ∈E h , c| E ∈ P l (E)}. (53)<br />

In view of (23) <strong>and</strong> (32), we discretize (51)–(52) by: Find c h ∈ Y h such that<br />

for all v h ∈ Y h :<br />

∑<br />

E∈E h<br />

∫E<br />

−<br />

+ ∑<br />

∑<br />

e∈Γ h ∪∂Ω<br />

E∈E h<br />

∫E<br />

K∇c h ·∇v h dx<br />

∫<br />

( )<br />

{K∇ch · n e } e [v h ] e + ε{K∇v h · n e } e [c h ] e dσ + J0 (c h ,v h )<br />

e<br />

(<br />

uh ·∇c h + 1 2 (div u )<br />

h)c h vh dx − 1 2<br />

− ∑ ∫<br />

{u h }·n E (c int<br />

h<br />

E∈E<br />

(∂E) − h<br />

where (∂E) − is defined by (20)<br />

∑<br />

e∈Γ h ∪∂Ω<br />

∫<br />

[u h ] e · n e {c h v h } e dσ<br />

e<br />

− c ext<br />

h )vh int dσ =<br />

(∂E) − = {x ∈ ∂E : {u h }·n E (x) < 0},<br />

∫<br />

Ω<br />

fv h dx, (54)<br />

<strong>and</strong> the parameters ε <strong>and</strong> σ e are the same as previously.<br />

To simplify, we introduce the form t h with the upwind approximation of<br />

the transport term in (54):

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