openfoam/tutorials/verificationAndValidation/atmosphericModels/HargreavesWright_2007/README
Kutalmis Bercin 336fb3bddf ENH: improve/verify atmBoundaryLayerInlet conditions
ENH: add generalised log-law type ground-normal inflow boundary conditions for
  wind velocity and turbulence quantities for homogeneous, two-dimensional,
  dry-air, equilibrium and neutral atmospheric boundary layer (ABL) modelling

  ENH: remove `zGround` entry, which is now automatically computed

  ENH: add `displacement height` entry, `d`

  ENH: add generalised atmBoundaryLayerInletOmega boundary condition

  ENH: add a verification case for atmBoundaryLayerInlet BCs

  DOC: improve atmBoundaryLayerInlet header documentation

  BUG: fix value-entry behaviour in atmBoundaryLayerInlet (fixes #1578)
  Without this change:
  - for serial-parallel computations, if `value` entry is available in
    an `atmBoundaryLayerInlet` BC, the theoretical ABL profile expressions
    are not computed, and the `value` entry content is used as a profile data
  - for parallel computations, if `value` entry is not available, `decomposePar`
    could not be executed.
  With this change:
  - assuming `value` entry is always be present, the use of `value` entry for
    the ABL profile specification is determined by a flag `initABL`
  - the default value of the optional flag `initABL` is `true`, but whenever
    `initABL=true` is executed, `initABL` is overwritten as `false` for the
    subsequent runs, so that `value` entry can be safely used.
  Thanks Per Jørgensen for the bug report.

  BUG: ensure atmBoundaryInlet conditions are Galilean-invariant (fixes #1692)

  Related references:

      The ground-normal profile expressions (tag:RH):
        Richards, P. J., & Hoxey, R. P. (1993).
        Appropriate boundary conditions for computational wind
        engineering models using the k-ε turbulence model.
        In Computational Wind Engineering 1 (pp. 145-153).
        DOI:10.1016/B978-0-444-81688-7.50018-8

    Modifications to preserve the profiles downstream (tag:HW):
        Hargreaves, D. M., & Wright, N. G. (2007).
        On the use of the k–ε model in commercial CFD software
        to model the neutral atmospheric boundary layer.
        Journal of wind engineering and
        industrial aerodynamics, 95(5), 355-369.
        DOI:10.1016/j.jweia.2006.08.002

    Expression generalisations to allow height
    variation for turbulence quantities (tag:YGCJ):
        Yang, Y., Gu, M., Chen, S., & Jin, X. (2009).
        New inflow boundary conditions for modelling the neutral equilibrium
        atmospheric boundary layer in computational wind engineering.
        J. of Wind Engineering and Industrial Aerodynamics, 97(2), 88-95.
        DOI:10.1016/j.jweia.2008.12.001

    The generalised ground-normal profile expression for omega (tag:YGJ):
        Yang, Y., Gu, M., & Jin, X., (2009).
        New inflow boundary conditions for modelling the
        neutral equilibrium atmospheric boundary layer in SST k-ω model.
        In: The Seventh Asia-Pacific Conference on Wind Engineering,
        November 8-12, Taipei, Taiwan.

  Reproduced benchmark:
      Rectangular prism shown in FIG 1 of
        Hargreaves, D. M., & Wright, N. G. (2007).
        On the use of the k–ε model in commercial CFD software
        to model the neutral atmospheric boundary layer.
        Journal of wind engineering and
        industrial aerodynamics, 95(5), 355-369.
        DOI:10.1016/j.jweia.2006.08.002
  Benchmark data:
      HW, 2007 FIG 6

  TUT: update simpleFoam/turbineSiting tutorial accordingly
2020-06-05 14:40:53 +01:00

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#------------------------------------------------------------------------------
Overview
"By setting appropriate profiles for wind velocity and the turbulence
quantities at the inlet, it is often assumed that the boundary layer will
be maintained up to the buildings or obstructions in the flow." (HW:p. 355).
However, it was quantified by (HW:p. 355) that "even in the absence of
obstructions, ..., the velocity and turbulence profiles decay along the
fetch" (HW:p. 355). It was shown by (HW:p. 355) that a set of modifications
were required to maintain a neutral atmospheric boundary layer throughout
an empty and long computational domain of a RANS computation.
Aim:
Verification of the following boundary conditions in terms of the
maintenance of inlet quantities downstream within a RANS computation:
- atmBoundaryLayerInletVelocity
- atmBoundaryLayerInletK
- atmBoundaryLayerInletEpsilon
- atmBoundaryLayerInletOmega
Benchmark (Physical phenomenon):
The benchmark is an empty fetch computational domain, steady-state
RANS simulation involving the following traits:
- External flow
- The surface layer portion of the neutral-stratified equilibrium
atmospheric boundary layer (no Ekman layer)
- Dry air
- Homogeneous, smooth terrain
- Spatiotemporal-invariant aerodynamic roughness length
- No displacement height
- Newtonian, single-phase, incompressible, non-reacting
Benchmark scenario:
- Computational domain: (HW:Fig. 1)
- Benchmark dataset: (HW:Fig. 6) (Obtained by the WebPlotDigitizer-4.2
(Rohatgi, 2019))
Resources:
Computational study (tag:HW):
Hargreaves, D. M., & Wright, N. G. (2007).
On the use of the kε model in commercial CFD software
to model the neutral atmospheric boundary layer.
Journal of wind engineering and
industrial aerodynamics, 95(5), 355-369.
DOI:10.1016/j.jweia.2006.08.002
Wind profile (tag:RQP):
Richards, P. J., Quinn, A. D., & Parker, S. (2002).
A 6 m cube in an atmospheric boundary layer flow-Part 2.
Computational solutions. Wind and structures, 5(2_3_4), 177-192.
DOI:10.12989/was.2002.5.2_3_4.177
Physical modelling:
- The governing equations for:
- Steady-state, Newtonian, single-phase, incompressible fluid flows,
excluding any thermal chemical, electromagnetic and scalar
interactions
- Mathematical approach for the turbulence modelling:
- Reynolds-averaged Navier-Stokes simulation (RANS)
- Turbulence closure model:
- kEpsilon and kOmegaSST linear eddy viscosity closure models
- The sets of input (HW:Table 1):
- Reference height, Zref = 6 [m]
- Aerodynamic roughness height, z0 = 0.01 [m]
- Displacement height, d = 0 [m]
- Reference mean wind speed, Uref = 10 [m/s]
Computational domain modelling:
- Rectangular prism
- (x1, x2, x3)
= (5000, 100, 500) [m]
= (streamwise, spanwise, ground-normal) directions
Computational domain discretisation:
- Spatial resolution:
- (x1, x2, x3) = (500, 5, 50) [cells]
- Refer to the `system/blockMeshDict` for the grading details
- Temporal resolution: Steady state
Equation discretisation:
- Spatial derivatives and variables:
- Convection: Second order
- Others: Second order with various limiters
- Temporal derivatives and variables: First order
Numerical boundary/initial conditions:
- Refer to `0.orig`
Pressure-velocity coupling algorithm:
- SIMPLEC
Linear solvers:
- Refer to `system/fvSolution`
Initialisation and sampling:
- No initialisation/averaging
- Sampling at the end of the simulation via `system/sampleDict`
- Refer to `system/controlDict` for further details
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