Partial Differential Equations - Modelling and ... - ResearchGate
Partial Differential Equations - Modelling and ... - ResearchGate
Partial Differential Equations - Modelling and ... - ResearchGate
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214 J. Hao et al.<br />
where u <strong>and</strong> p denote velocity <strong>and</strong> pressure, respectively, the boundary conditions<br />
for the velocity field g 0 (t) is0 at the bottom of Ω <strong>and</strong> (c, 0) t at the<br />
top of Ω with a fixed speed c for shear flow, λ is a Lagrange multiplier,<br />
D(v) =[∇v +(∇v) t ]/2, g is gravity, F is the pressure gradient pointing in<br />
the x 1 -direction, V G is the translation velocity of the particle B, <strong>and</strong>ω is the<br />
angular velocity of B. We suppose that the no-slip condition holds on ∂B. We<br />
also use, if necessary, the notation φ(t) for the function x → φ(x,t).<br />
Remark 1. The hydrodynamical forces <strong>and</strong> torque imposed on the rigid body<br />
by the fluid are built in (1)–(6) implicitly (see [GPHJ99, GPH + 01] for details),<br />
thus we do not need to compute them explicitly in the simulation. Since in<br />
(1)–(6) the flow field is defined on the entire domain Ω, it can be computed<br />
with a simple structured grid.<br />
The forces obtained from those Hookean springs in the model for cell<br />
adhesion has been splitted from the above equations <strong>and</strong> will be used when<br />
predicting <strong>and</strong> correcting the motion <strong>and</strong> positions of cells with the short<br />
repulsion force as discussed in the next section. ⊓⊔<br />
Remark 2. In (3), the rigid body motion in the region occupied by the particle<br />
is enforced via Lagrange multipliers λ. To recover the translation velocity<br />
V G (t) <strong>and</strong> the angular velocity ω(t), we solve the following equations:<br />
{<br />
〈ei , u(t) − V G (t) − ω(t) −→ Gx ⊥ 〉 B(t) =0, for i =1, 2,<br />
〈 −→ Gx ⊥ , u(t) − V G (t) − ω(t) −→<br />
(7)<br />
Gx ⊥ 〉 B(t) =0.<br />
⊓⊔<br />
Remark 3. In (1), 2 ∫ Ω D(u) :D(v) dx can be replaced by ∫ ∇u : ∇v dx<br />
Ω<br />
since u is divergence free <strong>and</strong> in W 0,p . Also the gravity g in (1) can be absorbed<br />
into the pressure term. ⊓⊔<br />
3.2 Space Approximation <strong>and</strong> Time Discretization<br />
Concerning the space approximation of the problem (1)–(6) by a finite element<br />
method,wehavechosenP 1 -iso-P 2 <strong>and</strong> P 1 finite elements for the velocity field<br />
<strong>and</strong> pressure, respectively (like in [BGP87]). More precisely, with h, aspace<br />
discretization step, we introduce a finite element triangulation T h of Ω <strong>and</strong><br />
then T 2h a triangulation twice coarser. (In practice, we should construct T 2h<br />
first <strong>and</strong> then T h by joining the midpoints of the edges of T 2h , dividing thus<br />
each triangle of T 2h into four similar subtriangles as shown in Figure 3.)<br />
We approximate then W g0,p, W 0,p , L 2 <strong>and</strong> L 2 0 by the following finite dimensional<br />
spaces, respectively: