Abstract:Direct numerical simulations (DNS) indicate that at large values of the Rayleigh number (Ra) convection in porous media self-organizes into narrowly-spaced columnar flows, with more complex spatiotemporal features being confined to boundary layers near the top and bottom walls. In this investigation of high-Ra porous media convection in a minimal flow unit, two reduced modeling strategies are proposed that exploit these specific flow characteristics. Both approaches utilize the idea of decomposition since the … Show more
“…A remarkable property of this algorithm is that it eliminates the requirement of numerical continuation (Plasting & Kerswell 2003). As the two-step algorithm can be implemented at any value of the flow parameter, this flexibility has led to wider usage in several other studies of the background method to obtain the optimal bound numerically (Wen et al 2015;Wen & Chini 2018;Ding & Marensi 2019;Lee, Wen & Doering 2019;Souza, Tobasco & Doering 2020). The first step of the algorithm uses a pseudo-time stepping scheme in which the Euler-Lagrange equations (A28a-d) are converted into a time-dependent system of partial differential equations (PDEs) as follows:…”
This paper is concerned with the optimal upper bound on mean quantities (torque, dissipation and the Nusselt number) obtained in the framework of the background method for the Taylor–Couette flow with a stationary outer cylinder. Along the way, we perform the energy stability analysis of the laminar flow, and demonstrate that below radius ratio
$0.0556$
, the marginally stable perturbations are not the axisymmetric Taylor vortices but rather a fully three-dimensional flow. The main result of the paper is an analytical expression of the optimal bound as a function of the radius ratio. To obtain this bound, we begin by deriving a suboptimal analytical bound using analysis techniques. We use a definition of the background flow with two boundary layers, whose relative thicknesses are optimized to obtain the bound. In the limit of high Reynolds number, the dependence of this suboptimal bound on the radius ratio (the geometrical scaling) turns out to be the same as that of numerically computed optimal bounds in three different cases: (1) the perturbed flow only satisfies the homogeneous boundary conditions but need not be incompressible; (2) the perturbed flow is three-dimensional and incompressible; (3) the perturbed flow is two-dimensional and incompressible. We compare the geometrical scaling with the observations from the turbulent Taylor–Couette flow, and find that the analytical result indeed agrees well with the available direct numerical simulations data. In this paper, we also dismiss the applicability of the background method to certain flow problems and therefore establish the limitation of this method.
“…A remarkable property of this algorithm is that it eliminates the requirement of numerical continuation (Plasting & Kerswell 2003). As the two-step algorithm can be implemented at any value of the flow parameter, this flexibility has led to wider usage in several other studies of the background method to obtain the optimal bound numerically (Wen et al 2015;Wen & Chini 2018;Ding & Marensi 2019;Lee, Wen & Doering 2019;Souza, Tobasco & Doering 2020). The first step of the algorithm uses a pseudo-time stepping scheme in which the Euler-Lagrange equations (A28a-d) are converted into a time-dependent system of partial differential equations (PDEs) as follows:…”
This paper is concerned with the optimal upper bound on mean quantities (torque, dissipation and the Nusselt number) obtained in the framework of the background method for the Taylor–Couette flow with a stationary outer cylinder. Along the way, we perform the energy stability analysis of the laminar flow, and demonstrate that below radius ratio
$0.0556$
, the marginally stable perturbations are not the axisymmetric Taylor vortices but rather a fully three-dimensional flow. The main result of the paper is an analytical expression of the optimal bound as a function of the radius ratio. To obtain this bound, we begin by deriving a suboptimal analytical bound using analysis techniques. We use a definition of the background flow with two boundary layers, whose relative thicknesses are optimized to obtain the bound. In the limit of high Reynolds number, the dependence of this suboptimal bound on the radius ratio (the geometrical scaling) turns out to be the same as that of numerically computed optimal bounds in three different cases: (1) the perturbed flow only satisfies the homogeneous boundary conditions but need not be incompressible; (2) the perturbed flow is three-dimensional and incompressible; (3) the perturbed flow is two-dimensional and incompressible. We compare the geometrical scaling with the observations from the turbulent Taylor–Couette flow, and find that the analytical result indeed agrees well with the available direct numerical simulations data. In this paper, we also dismiss the applicability of the background method to certain flow problems and therefore establish the limitation of this method.
“…They find a lower prefactor c for the unit optimal scaling exponent in the F -Ra relationship. Moreover, these upper-bound variational analysis also yields a set of a priori eigenfunctions which can be used to construct low-/reduced-order models for porous media convection [50][51][52].…”
We briefly review the investigations of pattern formation and transport properties of RayleighDarcy convection (or the Elder Problem), including laboratory experiments, theoretical analysis and numerical simulations. It is shown that the flow exhibits power-law-scaling characteristics at large Rayleigh-Darcy number Ra, a dimensionless parameter representing the ratio of the driving buoyancy forces to the diffusive forces. Namely, the mean spacing between neighboring interior plumes shrinks as Ra −α with the scaling exponent α ≤ 1/2 and the convective flux increases linearly with Ra. However, more laboratory experiments are needed to validate these scalings. Additionally, many conditions, e.g. the inclination of the layer and hydrodynamic dispersion, etc., may lead to a large uncertainty in the flow pattern and transport efficiency.
Motivated by Malkus' marginally stable boundary layer theory, we design an optimization problem to predict the heat transport through a two-dimensional, horizontal porous layer heated from the below and cooled from above. We solve the optimization problem numerically using a implemented package in Matlab. Our results show that the linear stability constraint well captures the unit-scaling property of flux at large values of Rayleigh number. Moreover, the predicted mean temperature profile shares many features exhibited by the long-time mean temperature profile from DNS.
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