2022
DOI: 10.1016/j.ijthermalsci.2022.107758
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A novel model for macroscopic simulation of oscillating heat and fluid flow in porous media

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Cited by 12 publications
(10 citation statements)
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“…The Nusselt number, as well as the permeability, slightly depends on the x-coordinate because the viscous and thermal penetration depths change with mean density/temperature. The complex permeability and Nusselt number, calculated as shown in previous work [5] and used in the macroscopic equations, are pictured in the following Figure 4. The results confirm that such a macroscopic model is suitable for modelling the thermoacoustic instability in a SWTAE, as proved by the comparison with microscopic results.…”
Section: Resultsmentioning
confidence: 99%
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“…The Nusselt number, as well as the permeability, slightly depends on the x-coordinate because the viscous and thermal penetration depths change with mean density/temperature. The complex permeability and Nusselt number, calculated as shown in previous work [5] and used in the macroscopic equations, are pictured in the following Figure 4. The results confirm that such a macroscopic model is suitable for modelling the thermoacoustic instability in a SWTAE, as proved by the comparison with microscopic results.…”
Section: Resultsmentioning
confidence: 99%
“…In this work, a macroscopic porous media model, derived from a previous article in case of isothermal case [4] and extended in subsequent work [5], has been applied for the first time to the stack of a SWTAE. The second section briefly reviews the governing equations of the "microscale" and "macroscale", and the third one describes the numerical setup employed in this work.…”
Section: Introductionmentioning
confidence: 99%
“…This approach has demonstrated the best agreement with analytical solutions, but it requires prior numerical simulations at the pore scale to be practically implemented (Bhatti and Öztop, 2022). According to the latest extension to the method, presented by Di Meglio et al (2022), the concept of the complex permeability trueκ˜c, in terms of its real and imaginary part, can be useful to separate the viscous effect, in which the pressure gradient is time-phased with velocity, and the oscillating inertial effects in which the pressure gradient is 90° out of phase with velocity by definition. The time-domain linear macroscopic governing equation, limited to the porous media zone, is the following, as demonstrated in a previous work (Di Meglio et al , 2022): …”
Section: Governing Equationsmentioning
confidence: 99%
“…where δv=2ν/ω is the viscous penetration depth ( v is the kinematic viscosity) and ℜ(ℑ) represents the real (imaginary) part operator. The complex permeability for a parallel plate stack is (Di Meglio et al , 2022): …”
Section: Governing Equationsmentioning
confidence: 99%
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