Accepted Manuscript CFD-DEM solution verification: Fixed-bed studies
William D. Fullmer, Jordan Musser PII: DOI: Reference:
S0032-5910(18)30674-0 doi:10.1016/j.powtec.2018.08.044 PTEC 13629
To appear in:
Powder Technology
Received date: Revised date: Accepted date:
11 November 2017 28 June 2018 12 August 2018
Please cite this article as: William D. Fullmer, Jordan Musser , CFD-DEM solution verification: Fixed-bed studies. Ptec (2018), doi:10.1016/j.powtec.2018.08.044
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ACCEPTED MANUSCRIPT CFD-DEM solution verification: Fixed-bed studies
William D. Fullmera,b, Jordan Mussera National Energy Technology Laboratory, Morgantown, WV 26507, USA
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AECOM, Morgantown, WV 26507, USA
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Email address:
[email protected] (William D. Fullmer),
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[email protected] (Jordan Musser)
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August 16, 2018
ACCEPTED MANUSCRIPT Abstract Fixed (frozen) particle configurations are used to study CFD-DEM convergence behavior in the limit of infinite grid resolution. A
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Gaussian filtering scheme based on solving a diffusion equation is used
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to interpolate particle information to the continuum grid, free of cell
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size limitations. A regression method is used for Richardson extrapolation of the discrete solutions to the grid-free solution. The
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regression method is shown to predict accurate extrapolation curves in
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the presence of the observed oscillatory convergence behavior. The
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extrapolation curve is used to complete the solution verification
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process by quantifying the numerical uncertainty present in the calculations. Several numerical and model parameters are studied
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including the spatial discretization method, the filter width and the
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mean drag law. A manageable level of discretization error is found
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with relative discretization errors generally less than 4%. Keywords: CFD-DEM, Solution verification, MFiX
ACCEPTED MANUSCRIPT 1 Motivation and Background Solution verification is an important aspect in the emerging field of verification, validation and uncertainty quantification (VVUQ). Solution verification deals with the
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quantification or estimation of numerical errors that arise when a mathematical model is
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solved computationally. Often, discretization error is most important of the numerical
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errors and the present study has been devised to specifically isolate and study spatial
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discretization error. The most general procedure is similar to informal convergence tests. First, a system response quantity of interest (SRQoI) is computed at several grid
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resolutions. Richard extrapolation is then used to approximate an exact or grid-free solution, i.e., what the SRQoI would be in the limit of infinite grid resolution. Finally, the
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numerical error (signed) or numerical uncertainty (unsigned) can be quantified based
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primarily on the difference the computed solution on a given grid and the (approximate) exact solution. Other methods exist, e.g., numerical method refinement, error transport
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equation and adjoint methods, among others, [1], however, methods based on grid-
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refinement remain the most popular in scientific computing and are used in this work.
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Solution verification procedures have been primarily developed for and largely applied to single-phase flows and, more specifically, steady Reynolds-averaged Navier-Stokes (RANS)-type models. Even in single-phase flows, solution verification based on grid refinement is challenged in the case of Large-Eddy Simulations (LES). In LES, the subgrid scale (SGS) viscosity model typically depends on the grid size, so, changing the grid essentially changes the model [2].
ACCEPTED MANUSCRIPT A similar issue arises in the case of the multiphase numerical method known as computational fluid dynamics-discrete element method (CFD-DEM). The CFD-DEM method couples a traditional RANS- or LES-type CFD model for the gas-phase with a Lagrangian method for the solid particle phase where the position and velocity of each
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particle are solved using Newton’s laws of motion and every collision is captured [3, 4].
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Filtering or interpolating schemes must be applied to transfer particle information, like
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drag and particle volume, to the continuum grid and vice versa. There are essentially two
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“philosophical” approaches to the transfer function: grid-coupled or grid-independent.
In practice, most CFD-DEM models typically use grid-coupled methods, e.g., see Garg
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et al. [5] and references therein. However, the grid-coupled approach presents a unique
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challenge to grid-refinement based solution verification methods. If the CFD grid is
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refined below the scale of the particle, the interpolated values are mapped to a physical space smaller than the representative particle itself. In the case of solids volume fraction,
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some cells will have unrealistically large values which may even exceed unity. This places a lower bound on how fine a grid-coupled interpolation-based CFD-DEM method
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can be refined which is approximately * 1 [6], where * (Vtot / N xyz )1/3 / d p is the
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dimensionless grid size, Vtot is the volume of the computational domain, Nxyz is the total number of grid points (cells) in the domain and dp is the particle diameter. Superficially, setting limitations on the level of refinement that a solution verification study may explore is dissatisfying at best and, more critically, could be seriously problematic if the asymptotic region cannot be reached for a particular solution outside of this limitation. The concern is compounded by the fact that many studies have shown that the CFD-grid
ACCEPTED MANUSCRIPT must be refined to a level of * 2 in order to achieve grid-insensitive results, e.g., see [7, 8].
The troubling resolution limitations of grid-coupled filtering leads us to conclude that grid-independent filtering is the most appropriate method for depositing particle
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information on the Eulerian grid. A grid-independent filtering method uses a kernal
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specifying a weighted spatial distribution that is independent of the underlying CFD-grid. The graphical abstract qualitatively shows how the solids concentration changes as a
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filtering kernal is applied in the present work.
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function of CFD grid resolution for the hypothetical bursting bubble case. A Gaussian
Solution verification of CFD-DEM is a largely unexplored topic for a variety of reasons.
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For one, CFD-DEM is a computationally intensive method, limiting the amount of
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simulations practitioners are willing to undertake. Additionally, grid-coupled methods
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compound the challenge by i) limiting the range of viable grids and ii) effectively changing the solution method with each new grid. Finally, there is a general belief within
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the community, not without merit, that other uncertainties including steady drag force model, neglected interfacial force and energy transfer terms, collision model, particle
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shape and neglected micro-structure, etc., all contribute to larger uncertainties in CFDDEM results than the numerical grid–so long a reasonable grid is applied ( * 3 ).
In this work, we explore the topic of solution verification of CFD-DEM with gridindependent filtering. In this preliminary study, we avoid the complications associated with time-averaging by considering only fixed particle configurations (PCs), i.e., the particles are frozen in space and do not move with time. Therefore, a steady-state result is
ACCEPTED MANUSCRIPT computed and the change in the solution is attributable to the change in numerical (truncation) error associated with the change CFD-grid resolution. The numerical method briefly outlined in Sec. 2. The particle configurations are created in two ways: i) a prescribed, “fictitious” bursting bubble configuration by a particle generator, Sec. 3 and
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ii) taken from instantaneous results of a previous, transient simulation, Sec. 4. Each case
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is studied on several different grids and a regression-based Richardson extrapolation
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method is used to calculate the grid-free solution and the numerical uncertainty [9].
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Finally the conclusions and future outlook are briefly provided in Sec. 5.
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2 Methods
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The results reported in this work were generated with the CFD-DEM model available in
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the open source MFiX code (https://mfix.netl.doe.gov/) version 2016.1. The governing equations and their numerical implementation are omitted for the sake of brevity and can
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aspects of the model.
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be found elsewhere [10, 11]. The remainder of this section outlines the most important
The MFiX CFD model is a finite volume implementation which uses a staggered grid and
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a SIMPLE-type iterative pressure-velocity coupling. Gradients are computed from face values extrapolated with a flux-limiter scheme [12], Superbee being considered the baseline method. Second-order center differencing is used for second-order derivatives. The time stepping is first order Euler, however, the time marching in this case is applied only to relax from an initial guess to a steady-state solution. In order to operate in a pseudo-steady mode, the call to the main DEM subroutine within the CFD iteration is
ACCEPTED MANUSCRIPT removed. This implementation results in three numerical tolerances: i) the linear equation solver, ii) the iterative time-step convergence, and, iii) the transient convergence. The linear equation solver tolerance is set to 10 – 8 for all equations except the Gaussian filter diffusion equation (see below) which is 10 – 10 . The value of the remaining tolerances are
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set at 10– 5 following an extensive study which revealed that these settings produced
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negligible error relative to the discretization error for the range of CFD grids considered
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[13].
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As mentioned in Sec. 1, we apply a grid-independent interpolation scheme, such as Gaussian filtering. While grid-independent filtering schemes do not have grid resolution
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limitations, there is a practical computational challenge associated with the inverse
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relationship between the size of the grid and the number of cells contained in the stencils
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surrounding the particles. For distributed memory parallelism, the challenge is compounded by the relationship between the stencil and the domain decomposition
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strategy. Fortunately, grid-independent Gaussian filtering can be achieved by a diffusion method rather than an explicit interpolation stencil based on the distance between the
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CFD grid and the particle centroid, see [14, 15] for details. Briefly, data associated with
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the discrete particles, α, is deposited to the continuous fluid grid. In the present work, we simply use a particle-centroid deposition scheme. Then, the data is filtered by solving a diffusion equation, f 2 , (1)
ACCEPTED MANUSCRIPT τ is an artificial time and ν f is a viscosity associated with the diffusion length through the artificial time,
16ln 2
(2)
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f f
max 2f 2 , 0
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where δf is the Gaussian filter full width at half maximum (FWHM). In MFiX, Eq. 1 is
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3 Fictitious bursting bubble
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considered as the baseline condition in this work.
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integrated in artificial time from τ = 0 to f 1 . A filter width of *f 6 is
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The first case studied is a simple, hypothetical problem which resembles a dilute bubble
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about to burst at the surface of a dense bed. The problem is completely fictional and created using a particle generator script. The geometry of the domain is
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L*x 30, L*y 200 , and L*z 10 . The particles of diameter d p 0.01 cm only occupy the
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lower quarter of the domain and are separated into three regions: a dilute (1%) “freeboard” region above the surface, a “dense bed” (30%) region below the surface, and
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a single dilute (1%) “bubble” inside the bed near the surface. A visualization of the baseline randomization PC1 is provided in the Graphical Abstract. The x- and zdimensions are periodic BCs. In the y-direction, the inlet is a uniform mass inflow BC and the outlet is a pressure outflow BC. The inlet gas velocity is set to U 0 = 20 cm/s. The 3 4 gas-phase material properties are g 1 10 g/cm3 , g 2 10 g/cm-s. Gravity is set
to zero. A uniform initial condition is set with a solids concentration of 0.18 and gas
ACCEPTED MANUSCRIPT velocity of ug (t 0) 0, vg (t 0) 24.4 cm/s, and wg (t 0) 0 . Finally, we select as “baseline” conditions: i) the Superbee flux-limiter for its favorable properties with discontinuous data (Waterson and Deconinck 2007), ii) the DNS-based mean drag law of Beetstra, van der Hoef and Kuipers [16] (BVK), and, iii) a diffusion filter width (FWHM)
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of *f 6 .
pg ( y* y1* ) pg ( y* y2* )
gU 02
(3)
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f DP1* 2
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elevations averaged over the bed cross-sectional area,
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The SRQoI, f, is taken to be the nondimensional pressure drop between two vertical
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We set y1* 4 and y2* 104 . The choice of y1* intentionally avoids the first row of grids
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cells adjacent to the inlet and does not lie along the cell centerline of any of the grids
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studied. Linear interpolation is used between the two rows of cells adjacent to y1* and y2* . DP1* 2 calculated on 18 different CFD-grids ranging in size from * 3.3 down to 0.16
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is displayed in Fig. 1. Perhaps the most important result of Fig. 1 is that the pressure drop
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does appear to converge to a unique solution in the limit of infinite resolution termed the grid-free or (approximate) exact solution
f 0 f * 0 .
(4)
From Fig. 1 it can be qualitatively observed that the exact solution, f 0 , occurs at DP1* 2 1159 . Another welcome result is that the maximum relative difference among all
solutions is less than 0.5% even though the grid has been refined from a modest CFD-
ACCEPTED MANUSCRIPT DEM grid size ( * 3 ) down to the boundary of DNS grid size ( * 1/ 6 ) [17]. Finally, it is observed that while the “global” convergence trend is well-behaved, the “local” or grid-to-grid behavior is oscillatory. An inherent grid dependency that arises from depositing particle data on the grid prior applying the diffusion operator may be
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responsible for the local oscillations.
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The oscillatory convergence behavior may likely be washed out by time-averaging in a transient simulation. However, the oscillatory pattern observed in the fixed bed studied
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here presents a challenge to traditional (determined) methods of Richardson extrapolation. If any two or three adjacent grid points are used to extrapolate the grid-free
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solution, f 0 , the result will vary wildly based on the data selected and the extrapolated
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solution may be far from the computed results. Therefore, we employ the
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(overdetermined) regression based method of Eça and Hoekstra [9] in which the extrapolation variables are determined by an optimization problem minimizing the least-
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squares of the error between the regression curve and all of the data. Here, we restrict our
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focus to two regression functions: power-law,
(5)
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fˆ f0 c(* ) p ,
and mixed-order,
fˆ f0 c1* c2 (* )2 ,
(6)
here integer first- and second-order. In both cases, we use an inverse grid size weighting function,
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and wi Wi / Wi ,
Wi 1/ *i
(7)
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placing a higher value on the finer grid solutions. The solution procedure used to determine the regression constants is outlined in the Supplementary Material and more
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thoroughly covered in Appendix B of [9].
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Fig. 1 compares the results of the regression-based Richardson extrapolation curves to the discrete solution data. In the baseline case, the power-law and mixed-order methods yield
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very similar results, giving approximate exact solutions of 1158.80 and 1158.79,
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respectively. Additionally, the convergence rate, p = 1.03, given by the power-law regression is within the expected range, taken to be 0.5 to 2.1 following Eça and Hoekstra
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[9]. The regressions can then be used to quantify the numerical error, f 0 fi , present in
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each calculation. Here, we adopt a concise uncertainty estimator defined by,
i Fs f0 fi RE ,
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(8)
f 3
ng
ng
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RE
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where Fs is a factor of safety, σRE is the standard deviation of the regression,
ng
i
2
fˆi , (9)
i 1
ng is the number of grids and fˆi is the extrapolated solution at the i-level grid. The factor of safety is taken to be:
Fs max 1.25,3 RE / R f ,
(10)
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Rf
max fi min fi (11) ng 1
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is the data range parameter. The ratio RE / R f quantifies the goodness of fit, with values
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less than unity being considered good. In the following analysis, the regression method is
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In addition to the baseline case, we have also studied:
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taken as the power-law when 0.5 p 2.1 and mixed-order otherwise.
(FOU) First order upwind spatial discretization,
(MUSCL) MUSCL flux limiter [18],
( *f 4 ) Narrower diffusion filter width,
( *f 8 ) Wider diffusion filter width,
( *f 16 ) Much wider diffusion filter width,
(PC2) A second randomization of particle locations in the same general
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configuration,
(PC3) A third randomization of particle locations,
(PC3t) A small “thermal” particle velocity is imposed on the previously static
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PC3,
(GB) Applying the Gidaspow-blend drag law [19, 20],
(WY) Applying the Wen and Yu drag law [21],
(HKL) Applying the Hill, Koch and Ladd drag law [22–24].
ACCEPTED MANUSCRIPT The relative discretization error (RDE),
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/ f 0 , results for all cases listed above have been
agglomerated into Fig. 2 with the baseline case. In general, most of the DP1* 2 results and their corresponding extrapolation curves are quite similar to the baseline case in Fig. 1 [13], making it difficult to distinguish the RDEs from one case to another. However, the
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key takeaway from Fig. 2 is the relatively small error observed in all cases with RDE below 4%. In most cases, grids with * 2 have less than 2% discretization error. The
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one major exception is the *f 4 case; the FOU case also has slightly higher
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discretization error than the other cases. Although for different reasons, these two cases
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present a similar regression challenge of a globally nonmonotonic convergence behavior while remaining locally oscillatory. Although the RDEs are quite similar in most cases,
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the normalization by f 0 hides the differences between the cases. For instance, the relative
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difference, 2 f0a f0b / f0a f0b , is 1.5% between the cases PC1 and PC2, 5% between
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cases *f 4 and *f 8 , 14% between cases *f 4 and *f 16 , 30% between cases GB and HKL and nearly 50% between cases WY and HKL. It is important to note that
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solution verification (verification in general) only provides an estimate of a solution at
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infinite resolution. Verification does not give any insight into which solution (from the different modeling options) is the best or most appropriate. This is a validation question and beyond the scope of the present work.
4 SSCP-I In this section, we wish to determine if the conclusions reached in Sec. 3 hold for more realistic yet still frozen particle configurations. To achieve this, the particle locations are
ACCEPTED MANUSCRIPT taken here from a previous transient CFD-DEM simulation of the NETL Small Scale Challenge Problem (SSCP-I) [25]. The geometry is quite similar to the previous fictitious case except the vertical BCs are now no-slip walls and the particle count is almost 20 times larger (Np = 92,948). The simulated geometry, particle and fluid properties are
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those measured experimentally [25]. The flow condition corresponds to the 2U mf case,
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U 0 219 cm/s. The original simulation used the Wen and Yu [21], the Superbee flux
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limiter, a grid-coupled interpolation method [11] and a CFD-grid of
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N x N y N z 18 96 6 or * 3.89 .
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Only the particle positions and (frozen) particle velocities are used for the fixed bed simulations. The fluid domain is reinitialized to a uniform condition as in the fictitious
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case. Six instances are considered corresponding t = 5, 6, 7, 8, 9 and 10 s. Several grid
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resolutions ranging from * 4.67 to 0.58 are studied using the same baseline condition
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as before in addition to the GB drag law [19, 20]. The nondimensional pressure drop, DP1* 2 , is again taken as the SRQoI, however, the locations y1* and y2* are set to the
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elevations of the pressure taps in the experiment [25]. Generally, the trends of the
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convergence behavior are quite similar to those observed in the fictitious bursting bubble case. However DP1* 2 does not flatten out quite as much, leading to slightly larger RDEs, though still less than 4% by and large. The discretization uncertainty for a typical CFDDEM resolution of * 3 is shown in Fig. 3 superimposed on the complete transient solution of the original simulation. In this scale, it can be observed that the discretization error is less impactful than the choice of a drag law (model form uncertainty) and the natural transient variations (related to time-averaging uncertainty [26]).
ACCEPTED MANUSCRIPT 5 Conclusions This preliminary study investigated grid refinement based solution verification techniques for fixed particle configurations likely encountered instantaneously in more
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general (transient) CFD-DEM simulations. A diffusion filter was applied for particle
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interpolation to remove any grid refinement restrictions. The nondimensional, area-
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averaged pressure drop was shown to converge to a unique solution in the limit * 0 .
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However, significant oscillatory behavior from one grid to another necessitated the use of regression-based Richardson extrapolation techniques [9] which proved to be very
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effective. Overall, the discretization was found to be rather small in these fixed bed cases with typical RDEs of only a few percent. Only a few instances studied had RDEs above
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3%, namely the coarsest grids of the FOU scheme in Fig. 3 and at times t = 9 and 10 s in
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Fig. 3. Qualitatively similar convergence behavior can be observed with different
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modeling choices, quantitatively, however, the choice of drag model, filter width, etc.
* 4 .
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appear to have a bigger impact on the solution than the numerical grid, at least for
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In closing, we suggest exercising caution using this study as a more general path forward for CFD-DEM solution verification. That is, for a given problem: freeze the simulation at several random instances, perform grid refinement, calculate the uncertainty in the SRQoIs, average the uncertainties over an ensemble of frozen instances and attribute the resulting ensemble average uncertainty to the full, time-averaged solution. This may be an accurate means to capture spatial grid discretization error alone, however, such a method cannot quantify uncertainties related to temporal discretization nor time-
ACCEPTED MANUSCRIPT averaging [26]. The results of this could may be used in the ranking of numerical errors and modeling uncertainties in future CFD-DEM studies. In general, it is somewhat encouraging that modeling uncertainties, e.g., drag, appear to be much more significant than discretization, provided a modest ( *
4 ) resolution is applied. Future work will
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aim to study solution verification of transient CFD-DEM and the challenge of calculating
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numerical error in the presence of time-averaging error. Finally, this work along with Sun
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and Xiao [15] and Patel et al. [27] have shown that CFD-DEM solutions depend on the
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size of the diffusion filter. Future validation studies comparing CFD-DEM to DNS or high-fidelity experimental data to determine the most appropriate filtering method would
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be valuable result.
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Acknowledgment
This technical effort was performed in support of the National Energy Technology
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Laboratorys ongoing research under the RES contract DE-FE0004000.
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This project was funded by the Department of Energy, National Energy Technology
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Laboratory, an agency of the United States Government, through a support contract with AECOM. Neither the United States Government nor any agency thereof, nor any of their employees, nor AECOM, nor any of their employees, makes any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or
ACCEPTED MANUSCRIPT otherwise, does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States
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Government or any agency thereof.
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Fig. 1 (Color online.)
Convergence behavior of the bed nondimensional pressure drop
in the fictional bursting bubble case for the baseline model parameters compared to the predicted Richardson extrapolation curves for power-law (red) and mixed-order (blue).
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Relative discretization error in the fictional bursting bubble case
for: baseline (black [filled]), FOU (black ×), MUSCL (black +), *f 4 (red ),
*f 8 (red ×), *f 16 (red +), PC2 (green ), PC3 (green ×), PC3t (green +), GB (blue
Fixed bed nondimensional pressure drop with discretization
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uncertainty for the six frozen particle configurations on a grid of * 3 for the BVK
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(blue) and GB (red) drag laws compared to the complete transient of the original
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simulation (black line).
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Highlights Solution verification based on grid-refinement is considered for CFD-DEM
Fixed-bed particle arrays and grid-independent Gaussian filter interpolation is used
The pressure drop converges to a unique solution in the limit of infinite resolution
Regression-based Richardson extrapolation works well with oscillatory convergence
Discretization error of the fixed-beds studies is quite small, generally <4%
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