Pressure-velocity coupling is achieved by using Equation 25.4-6 to derive an additional condition for pressure by reformatting the continuity equation (Equation 25.4-5). The pressure-based solver allows you to solve your flow problem in either a segregated or coupled manner. FLUENT provides the option to choose among five pressure-velocity coupling algorithms: SIMPLE, SIMPLEC, PISO, Coupled, and (for unsteady flows using the non-iterative time advancement scheme (NITA)) Fractional Step (FSM). All the aforementioned schemes, except the "coupled" scheme, are based on the predictor-corrector approach. See Section 25.9.1 for instructions on how to select these algorithms.
Note that SIMPLE, SIMPLEC, PISO, and Fractional Step use the pressure-based segregated algorithm, while Coupled uses the pressure-based coupled solver.
The SIMPLE algorithm uses a relationship between velocity and pressure corrections to enforce mass conservation and to obtain the pressure field.
If the momentum equation is solved with a guessed pressure field , the resulting face flux, , computed from Equation 25.4-6
does not satisfy the continuity equation. Consequently, a correction is added to the face flux so that the corrected face flux,
satisfies the continuity equation. The SIMPLE algorithm postulates that be written as
where is the cell pressure correction.
The SIMPLE algorithm substitutes the flux correction equations (Equations 25.4-8 and 25.4-9) into the discrete continuity equation (Equation 25.4-5) to obtain a discrete equation for the pressure correction in the cell:
where the source term is the net flow rate into the cell:
The pressure-correction equation (Equation 25.4-10) may be solved using the algebraic multigrid (AMG) method described in Section 25.6.3. Once a solution is obtained, the cell pressure and the face flux are corrected using
Here is the under-relaxation factor for pressure (see Section 25.4.4 for information about under-relaxation). The corrected face flux, , satisfies the discrete continuity equation identically during each iteration.
A number of variants of the basic SIMPLE algorithm are available in the literature. In addition to SIMPLE, FLUENT offers the SIMPLEC (SIMPLE-Consistent) algorithm [ 379]. SIMPLE is the default, but many problems will benefit from the use of SIMPLEC, as described in Section 25.9.1.
The SIMPLEC procedure is similar to the SIMPLE procedure outlined above. The only difference lies in the expression used for the face flux correction, . As in SIMPLE, the correction equation may be written as
However, the coefficient is redefined as a function of . The use of this modified correction equation has been shown to accelerate convergence in problems where pressure-velocity coupling is the main deterrent to obtaining a solution.
For meshes with some degree of skewness, the approximate relationship between the correction of mass flux at the cell face and the difference of the pressure corrections at the adjacent cells is very rough. Since the components of the pressure-correction gradient along the cell faces are not known in advance, an iterative process similar to the PISO neighbor correction described below is desirable. After the initial solution of the pressure-correction equation, the pressure-correction gradient is recalculated and used to update the mass flux corrections. This process, which is referred to as "skewness correction'', significantly reduces convergence difficulties associated with highly distorted meshes. The SIMPLEC skewness correction allows FLUENT to obtain a solution on a highly skewed mesh in approximately the same number of iterations as required for a more orthogonal mesh.
The Pressure-Implicit with Splitting of Operators (PISO) pressure-velocity coupling scheme, part of the SIMPLE family of algorithms, is based on the higher degree of the approximate relation between the corrections for pressure and velocity. One of the limitations of the SIMPLE and SIMPLEC algorithms is that new velocities and corresponding fluxes do not satisfy the momentum balance after the pressure-correction equation is solved. As a result, the calculation must be repeated until the balance is satisfied. To improve the efficiency of this calculation, the PISO algorithm performs two additional corrections: neighbor correction and skewness correction.
The main idea of the PISO algorithm is to move the repeated calculations required by SIMPLE and SIMPLEC inside the solution stage of the pressure-correction equation [ 155]. After one or more additional PISO loops, the corrected velocities satisfy the continuity and momentum equations more closely. This iterative process is called a momentum correction or "neighbor correction''. The PISO algorithm takes a little more CPU time per solver iteration, but it can dramatically decrease the number of iterations required for convergence, especially for transient problems.
For meshes with some degree of skewness, the approximate relationship between the correction of mass flux at the cell face and the difference of the pressure corrections at the adjacent cells is very rough. Since the components of the pressure-correction gradient along the cell faces are not known in advance, an iterative process similar to the PISO neighbor correction described above is desirable [ 104]. After the initial solution of the pressure-correction equation, the pressure-correction gradient is recalculated and used to update the mass flux corrections. This process, which is referred to as "skewness correction'', significantly reduces convergence difficulties associated with highly distorted meshes. The PISO skewness correction allows FLUENT to obtain a solution on a highly skewed mesh in approximately the same number of iterations as required for a more orthogonal mesh.
Skewness - Neighbor Coupling
For meshes with a high degree of skewness, the simultaneous coupling of the neighbor and skewness corrections at the same pressure correction equation source may cause divergence or a lack of robustness. An alternate, although more expensive, method for handling the neighbor and skewness corrections inside the PISO algorithm is to apply one or more iterations of skewness correction for each separate iteration of neighbor correction. For each individual iteration of the classical PISO algorithm from [ 155], this technique allows a more accurate adjustment of the face mass flux correction according to the normal pressure correction gradient.
Fractional-Step Method (FSM)
In the FSM, the momentum equations are decoupled from the continuity equation using a mathematical technique called operator-splitting or approximate factorization. The resulting solution algorithm is similar to the segregated solution algorithms described earlier. The formalism used in the approximate factorization allows you to control the order of splitting error. Because of this, the FSM is adopted in FLUENT as a velocity-coupling scheme in a non-iterative time-advancement (NITA) algorithm (Section 25.4.5).
As previously mentioned, the pressure-based solver allows you to solve your flow problem in either a segregated or coupled manner. Using the coupled approach offers some advantages over the non-coupled or segregated approach. The coupled scheme obtains a robust and efficient single phase implementation for steady-state flows, with superior performance compared to the segregated solution schemes. This pressure-based coupled algorithm offers an alternative to the density-based and pressure-based segregated algorithm with SIMPLE-type pressure-velocity coupling. For transient flows, using the coupled algorithm is necessary when the quality of the mesh is poor, or if large time steps are used.
The pressure-based segregated algorithm solves the momentum equation and pressure correction equations separately. This semi-implicit solution method results in slow convergence.
The coupled algorithm solves the momentum and pressure-based continuity equations together. The full implicit coupling is achieved through an implicit discretization of pressure gradient terms in the momentum equations, and an implicit discretization of the face mass flux, including the Rhie-Chow pressure dissipation terms.
In the momentum equations ( 25.4-3), the pressure gradient for component is of the form
Where is the coefficient derived from the Gauss divergence theorem and coefficients of the pressure interpolation schemes (Equation 25.4-4). Finally, for any th cell, the discretized form of the momentum equation for component is defined as
In the continuity equation, Equation 25.4-5, the balance of fluxes is replaced using the flux expression in Equation 25.4-6, resulting in the discretized form
As a result, the overall system of equations ( 25.4-16 and 25.4-17), after being transformed to the -form, is presented as
where the influence of a cell on a cell has the form
Note that Equation 25.4-18 is solved using the coupled AMG, which is detailed in Section 25.6.3.
The pressure-based coupled algorithm is not compatible with