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          FLOTHERM Advanced Training Course7-12

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          AdvancedTraining_8_Solver.pdf

          Solver
          -Discretized equations must be solved
          -Coefficients in equations are coupled
          -e.g. Velocities are influenced by pressure gradients
          -e.g. Velocities are influenced by temperature gradients (buoyancy)
          -Must therefore solve iteratively
          -Pressure and Temperature are
          evaluated at Cell Centres
          -Velocities are evaluated at Cell Faces
          -Staggered Grid
          -Gives correct pressure gradient terms in momentum equations
          -Velocities are evaluated where needed for convection-diffusion equations
          -At start of solution, velocity field and pressure field are unknown
          -FLOTHERM uses SIMPLEST algorithm to evaluate coupled velocity and pressure field
          -SIMPLEST is based on the Semi-
          Implicit Method for Pressure-Linked Equations (developed by Patankar and Spalding)

          -Solution of the equations proceeds as follows:
          -A pressure field p* is guessed
          -The discretized momentum equation is solved, to give velocity components, u* and v*

          -Our second constraint on the velocity field is that it must satisfy continuity
          -We use this constraint to determine the pressure correction, p’

          -Solver continues until the imbalances in the equations are less than that specified by the termination criteria
          -There are two methods for controlling convergence:
          -Linear relaxation
          -False time step

          -The central coefficient is adjusted using the false time step
          -Mass of cell / false time step is added to central coefficient

          False Time Step
          -False time step should be based on physical time scale of problem
          -Residence time in domain
          -Residence time in average cell

          Solver
          -Residence time in domain = Mean domain size / average velocity
          -Residence time in cell = Mean cell size/ average velocity
          -Normally, will set false time step within these limits

          -Because pressure correction comes from the continuity equation, no false time step for pressure
          -Can use linear relaxation instead
          -Or use false time steps for velocities
          -Conduction only problems, no false time step is needed
          -Should solve in 1 outer iteration
          -More efficient to limit inner iterations and perform several outer iterations

          Linear Solver
          -The discretized equations for pressure, velocity and temperature must be solved
          -Need an linear solver to do this
          -FLOTHERM offers three options
          -Segregrated Solver
          -Segregrated Conjugate Residual
          -Multigrid
          -Segregated:
          -Uses Gauss-Seidel solver
          -Looks locally at flow field
          -Can be slow to capture trends
          -Segregrated Conjugate Residual
          -Based on Conjugate Gradient method
          -Considers whole-field interactions
          -Fast at resolving trends through whole domain m.16909.cc
          -Multigrid
          -Same as segregrated conjugate residual for velocities and pressure
          -For temperature, solves on progressively coarser grid
          -Potentially very fast to converge temperature field; removes need for block correction

          Solver
          -Block correction
          -Splits domain into blocks
          -Generates new discretized equations for each block
          -Solves equations
          -Should give fast convergence for systems with large conductivity variations

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