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Direct numerical simulations for liquid metal applications        227

           6.1.1.3   Boundary and initial conditions


           6.1.1.3.1 Periodic boundary conditions
           In hydrodynamically and thermally fully (time) developed conditions and also for
           periodically fully developed conditions (Stalio and Piller, 2007), where homogeneity
           of the flow in the streamwise direction can be assumed (see Section 6.1.1.1), periodic
           BCs can be implemented on all variables along the streamwise direction, including
           pressure and temperature.
              One of the most frequently used geometries in DNS, where periodic BCs are
           imposed, is the channel flow. Simulations of a turbulent flow in a channel of infinite
           length (x) and width (z) are performed by approximating the infinite extent of the
           domain in the streamwise and spanwise directions with a computational domain of
           finite length (also called unit cell) and by applying periodic BCs in these directions.
           Such conditions theoretically entail the dependent variable fields to be periodic along
           the selected direction. In practice, their implementation depends on the specific
           method itself: for instance, periodicity is inherent to the basis functions of spectral
           methods, while in finite volume/finite difference methods, it is achieved by imposing
           a circular topology of the computational stencils at the two ends of the domain. Special
           care should be taken when choosing the extent of the unit cell, which should be large
           enough to encompass the largest scales of the flow. If these conditions are satisfied,
           the flow in the computational domain can be considered as an accurate representation
           of the flow in the infinite channel. Section 6.1.1.4 reports some qualitative criteria for
           the choice of the channel length and width.



           6.1.1.3.2 Inflow open boundary conditions
           Periodic BCs can be applied in the streamwise direction to the computed variables
           when fully developed conditions are met. In case the interest is a spatially developing
           flow, the DNS approach requires resorting to an inflow turbulence generation method
           for both the velocity and the temperature fields. Inflow turbulence generation methods
           for the velocity field have been recently classified and reviewed by Wu (2017). A short
           auxiliary periodic domain, where turbulence is computed in parallel to the main cal-
           culation, is providing results that are used as inflow condition for the target simulation.
           This type of inflow BCs is known as a recycling method. Synthetic methods represent
           an alternative attempt to fully model the inflow.



           6.1.1.3.3 Outflow open boundary conditions
           Devising appropriate BCs at open boundaries when the mean flow is exiting the
           domain can be a difficult task (Sani and Gresho, 1994). The most common problems
           of outflow open BCs is that they produce spurious reflection of the velocity and of
           transported scalars, they tend to produce wiggles at the domain boundary and might
           affect the stability of the solution algorithm.
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