INAUGURAL–DISSERTATION zur Erlangung der Doktorwürde der ...
INAUGURAL–DISSERTATION zur Erlangung der Doktorwürde der ...
INAUGURAL–DISSERTATION zur Erlangung der Doktorwürde der ...
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2.3. Euler – Euler Approach 25<br />
of the unknown moments applying the Wheeler algorithm are explained in Chapter 3.<br />
2.3.4 Direct Quadrature Method of Moments (DQMOM)<br />
In DQMOM, the NDF is approximated as sum of the Dirac-delta functions. Substitution<br />
of this assumed NDF in Williams’ spray equation yields transport equations in<br />
terms of the phase-space [60]. For the present study, a joint droplet radius-velocity<br />
number density function is consi<strong>der</strong>ed, which is approximated in DQMOM as a sum<br />
of the product of weighted Dirac-delta functions [53] of radii and velocities [60],<br />
f(r, v) =<br />
N∑<br />
w n δ(r − r n )δ(v − v n ), (2.25)<br />
n=1<br />
where w n and r n are chosen as N representative quantities of weights and radii, and v n<br />
are the corresponding velocities. Such an approximation with a three-node (N = 3) closure<br />
can be depicted as shown in Fig. 2.4. Application of DQMOM to Williams’ spray<br />
equation results in closed transport equations in terms of droplet weights or number<br />
densities, radii and velocities, which are written as<br />
∂w n<br />
∂t<br />
∂(w n ρ l r n )<br />
∂t<br />
+ ∂(w nv n )<br />
∂x<br />
+ ∂(w nρ l r n v n )<br />
∂x<br />
= a n , (2.26)<br />
= ρ l b n , (2.27)<br />
and<br />
∂(w n ρ l r n v n )<br />
+ ∂(w nρ l r n v n v n )<br />
= ρ l c n , (2.28)<br />
∂t<br />
∂x<br />
where a n , b n and c n are the source terms that account for droplet evaporation, forces<br />
on droplet (drag, buoyancy, lift, basset and virtual mass effect and gravity etc.), coalescence<br />
and breakup. These Eqs. (2.26) – (2.28) form a set of coupled hyperbolic<br />
partial differential equations, which can be solved simultaneously by using appropriate<br />
initial and boundary conditions to find w n (x, t), r n (x, t) and v n (x, t), and thereby the<br />
evolution of droplet distribution function f can be computed.<br />
Fig. 2.4: NDF approximation in DQMOM.