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Large
Eddy Simulations with STAR-CCM+ The requirement to successfully simulate mean and fluctuating surface pressure distributions on the surface of buildings in the atmospheric boundary layer is a challenging problem, which has occupied wind engineers for at least two decades. To date LES and more recently DES methods are regarded as being the only methods with a practical chance of resolving the large scale instabilities that dominate flows in the built environment. For wind loading purposes, the large Reynolds numbers, geometrical extent and complexity of groups of buildings, imply that the computing power required to calculate these flows to an accuracy comparable with wind tunnel experiments, makes their resolution currently uneconomical by around two orders of magnitude. Several benchmark problems are used to test new developments, of which vortex shedding from a square cylinder is probably the most universal. It is usually considered that correctly modeling the velocity gradients perpendicular to the wall is a necessary condition for the prediction of flow separation. However sharp edged bluff bodies have well defined flow separation points at their corners, creating shear layers that are highly unstable and drive vortex shedding. The upside to this situation is that resolution of the near wall perpendicular velocity gradients is less important. The downside is the resulting instability requires time dependent simulation to resolve the unstable flow close to the body and vortex shedding in the wake. The surface pressure distribution is dominated by these large scale structures. Tensys Dynamics have been investigating the combined use of embedded polyhedral meshes and time dependent laminar simulations in STAR-CCM+ to resolve these flows. The level of mesh refinement used in this study implies the size of eddies resolvable does not qualify the method to be called Direct Numerical Simulation (DNS) it is rather a LES model with no explicit sub grid scale model, with implicit sub-grid viscosity arising from the advection scheme upwinding. Simulation
Details The simulations were run on a series of three progressively refined meshes consisting of 40k, 260k and 620k polyhedral cells, each employing refined embedded regions within them. The height of the first cell from the surface was kept, constant at 0.025D for all cases. The embedded meshes were created in STAR-Design utilizing a recursive method of imprinting nested sub domains which captured the cylinder and its wake. The imprinting method has the flexibility to create sub domains of any shape with arbitrary levels of refinement. This has advantages over traditional hexahedral trimmed cell embedding where only rectangular blocks of meshes refined in multiples of two are possible. The unusual choice of not using a sub-grid scale model was motivated by a desire to firstly assess the extent to which numerical diffusion contributed to the solution of conventional LES simulations. Secondly to simultaneously assess the inherent numerical diffusion resulting from the use of polyhederal mesh and STAR-CCM+¡¯s 2nd order spatial discretization, as a implicit sub-grid scale model. The time step used for all the simulations was 0.1 units of non-dimensional time (D/V) giving a maximum Courant number on the fine grid of 4. Second order spatial and temporal discretization schemes were used for all calculations. Each simulation was run for at least 50 non-dimensional time units before vortex shedding became sufficiently regular. After this time mean Cp profiles and rms Cp profiles were extracted on the intersection of the centre plane with the cylinder using four line probes at 500 time steps corresponding to about 7 vortex shedding periods. The laminar time dependent method was compared with simulations using unsteady k-w, DES and inviscid models on the coarsest grid only. Results On the coarse mesh the laminar predictions are closer to the experimental values than the other models. In particular the k-w URANS and DES models add additional unnecessary damping which reduce all parameters. It is quite possible that the seven vortex shedding cycles over which the integrated parameters were extracted over, is an insufficient period. However time constraints on the finest mesh made this necessary. The effect of grid refinement is seen to steadily increase the magnitude of both the rms and mean Cp values. The increase in the rms values is consistent with the reduction of numerical diffusion originating from the spatial and temporal discretization. The mechanism which correlates an increase in rms Cp values with an increase in mean Cp values in the experimental results is unclear but appears to be mimicked in the numerical results. The mean and particularly the rms Cp profile from the medium 260K mesh matches the experimental values well, indicating that this amount of numerical dissipation acts as an effective sub grid scale model for this level of inlet turbulence. The coarser mesh solution clearly adds more numerical diffusion and suppresses the rms and mean Cp values further while the finer mesh adds less resulting in increased wind loadings. The effect of various turbulence models on the 40k coarse mesh is shown in figures 4 and 5. Clearly the addition of more turbulent viscosity worsens the result, which is especially true of the k-w URANS model. This implies there is already too much damping present in the solution from the inherent numerical diffusion. Conclusions For
this benchmark flow we have found that LES simulations with no explicit
sub grid model using embedded polyhedral refinement gives results
accurate enough for wind loading purposes with a simulation time
equivalent to 50 hrs on a 3.00 MHz PC (260k mesh). Without imposing
turbulent fluctuations on the velocity inlet profile equivalent
to the experimental values, further mesh refinement may lead to
an over estimation of magnitudes of mean and rms pressure coefficients,
however in the wind loading context this is no bad thing and can
be interpreted as a worst case scenario. |
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