A multiscale analysis of heat transfer in porous media

Thermal convection;Porous media;Multi-scale analysis;Lattice-Boltzmann method;Fractional-order thermal dispersion;Linear stability analysis;Basin stability analysis.

Ghazizadeh Karani, Hamid Reza ; Huber, Christian Earth and Atmospheric Sciences Dufek, Joe Simon, Sven Ferrier, Ken Magin, Richard L ; Huber, Christian

University:Georgia Institute of Technology

Department:Earth and Atmospheric Sciences

关键词: Thermal convection;    Porous media;    Multi-scale analysis;    Lattice-Boltzmann method;    Fractional-order thermal dispersion;    Linear stability analysis;    Basin stability analysis.;   

Others  :  https://smartech.gatech.edu/bitstream/1853/59236/1/GHAZIZADEHKARANI-DISSERTATION-2017.pdf

美国|英语

来源: SMARTech Repository

【 摘 要 】

The modeling of thermal convection in porous media is a challenging task due to the inherent structural and thermophysical heterogeneities that permeate over several scales. In the present thesis, I address several issues relevant to buoyancy-driven thermal convection in porous media. The central question we address is how to develop a macroscopic model of heat transfer in porous media that incorporates the pore-scale physics in a consistent manner. Our approach is based on establishing a multi-scale framework built on knowledge accrued by theoretical, numerical and experimental methods.In Chapter 2, we develop a pore-scale computational tool based on a lattice Boltzmann (LB) model. This computational tool enables us to tackle thermal convection from a pore-scale perspective and to provide benchmarks for the development of an appropriate continuum-scale models. In Chapter 3, we use our LB model and conduct high-resolution direct numerical simulation at the pore scale. The objective is to evaluate the underlying assumptions of upscaled thermal models and to assess the role of thermophysical heterogeneties on heat transfer. We benefit from the insights gained from our pore-scale results and propose a new upscaled energy model for thermal convection in Chapter 4. The proposed model is based on a fractional-order advective term, which models the influence of thermal heterogeneities in a flexible and consistent way. In Chapter 5, we used a combination of theoretical and experimental approaches to calculate a new metric, basin stability, for quantifying the respective relative stability of coexisting convection modes in porous media. We show that transition between convective modes predicted by the basin stability analysis agrees well with the experiments from our IR thermography visualization setup.