Kharon theory manual
Conservation of Mass
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Steady one-dimensional conservation of mass (of phase q) is given through the following relation
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(1)
Equation 1 is discretized for an interior cell, shown in Figure 1, by volume integration over cell P.
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(2)
The divergence term on the left-hand side of the equation is transformed into a surface integral over the cell faces using the divergence theorem.
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(3)
Throughout this document upwind discretization is used to evaluate the face mass flow rates, even though any discretization scheme could be chosen. The final discretized form reduces to
-
(4)
where:
volume fraction of phase q [-], volumetric mass transfer rate from phase p to q [kg/m3s], mass transfer rate from phase p to q [kg/s], porosity, fluid fraction of cell volume [-], density of phase q [kg/m3], face area [m2], face mass flow rate [kg/s], face normal pointing out of the cell (1 for east face, -1 for west face), volumetric mass source to phase q [kg/m3s], mass source to phase q [kg/s], velocity of phase q [m/s], subscript e east face (the face in the negative x-direction), subscript w west face (the face in the positive x-direction), subscript q current phase for which the equation is written (1 = primary, 2 = secondary), subscript p the other phase (p = 2 for q = 1 and p = 1 for q = 2), subscript pq indicates exchange between phases (e.g. mass transfer from phase p to q).
Conservation of Momentum
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Steady one-dimensional conservation of momentum (of phase q) is solved from the following relation
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(5)
Equation 5 is discretized for an interior cell, shown in Figure 2, by volume integration over cell P. The diffusion term has been moved to the left-hand side, since it will be developed together with the divergence of momentum.
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(6)
As with the conservation of mass equation above, the divergence terms on the left-hand side of the equation are transformed into surface integrals over the cell faces using the divergence theorem.
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(7)
Developing the left-hand side terms first
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(8)
Adopting upwind discretization for the momentum fluxes on the cell faces
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(9)
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(10)
and rearranging terms
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(11)
Denoting and
and modifying the central coefficient slightly, since
and
, Equation 11 reduces to
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(12)
Identifying the coefficients of neighboring velocities
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(13)
-
(14)
leads to a general form
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(15)
Conservation of Total Enthalpy
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