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3.2. Spray Modeling 51<br />

application and numerical accuracy, a second or<strong>der</strong> explicit finite difference scheme is<br />

applied to solve steady state form of Eqs. (2.26) – (2.28) [192], which are represented<br />

by Eq. (3.21). Thus the solution formula may be written as [193]<br />

U j+1<br />

n,i<br />

= U j n,i − ∆x [<br />

1.5E<br />

j<br />

i<br />

∆z<br />

− 2Ej i−1 + ] 0.5Ej i−2 + ∆xS<br />

j<br />

i , (3.23)<br />

where i and j are grid nodes in radial and axial directions, respectively.<br />

The above formulation is applied to an equidistant rectangular grid, where the size<br />

of each grid cell is 1.5 × 10 −3 m in radial direction and 1.0 × 10 −4 m in axial<br />

direction, resulting in a maximum of 80 × 1000 grid nodes. The initial data to start<br />

simulations in both the configurations, i.e, one and two-dimensional cases is generated<br />

from the experimental data provided by Dr. R. Wengeler, BASF Ludwigshafen (onedimensional<br />

water spray in nitrogen) and Prof. G. Brenn, TU Graz (two-dimensional<br />

water and PVP/water spray in air) using Wheeler algorithm (see Subsection 3.2.3). The<br />

experimental data closest to the nozzle exit is taken for generating the initial data and<br />

the procedure for calculating this initial data from experiment is explained in Chapter<br />

4 along with brief description about the experimental setup. The boundary conditions<br />

in solving DQMOM include (1) if droplets hit the axis of symmetry, they are reflected,<br />

and (2) Neumann boundary is applied for the lateral sides of the computational domain<br />

and exit plane. The experimental data available at other cross sections away from the<br />

nozzle exit is used to validate the simulation results. The flowchart of the computational<br />

code is illustrated in Fig. 3.1.<br />

3.2.3 Wheeler Algorithm<br />

The Wheeler algorithm developed by Sack and Donovan [136], requires 2N +1 moments<br />

to compute N weights (number density) and N abscissas (droplet radii or velocities).<br />

The moment set is represented as M = [M(0), M(1), ...M(2N + 1)] T . This algorithm<br />

is used to generate the initial data in DQMOM whereas in QMOM it is used to compute<br />

the unknown moments. The first step in Wheeler algorithm is to compute the<br />

coefficients π α based on these 2N + 1 moments of the distribution function n(ξ), given<br />

as<br />

π α+1 (ξ) = ξπ α (ξ). (3.24)<br />

The above recursive relation has the properties of π −1 (ξ) = 0 and π 0 (ξ) = 1. Here, α<br />

is a subset of number of moments 2N + 1, i.e., α ∈ 0, 1, 2..N − 1. From these coefficients<br />

π α (ξ), a symmetric tridiagonal matrix is computed through some intermediate<br />

quantities:<br />

∫<br />

σ α,β = n(ξ)π α (ξ)π β (ξ)dξ, (3.25)

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