FSP-DDF coupling model of LBM for the fluid flow and heat transfer in porous media

Shao, Baoli; Wang, Shuyan; Tian, Ruichao; Qiao, Zhenxuan; Chen, Yujia; Sun, Qiji

doi:10.1016/j.applthermaleng.2019.04.108

Cited by 9 publications

(1 citation statement)

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“…The derivation of a new effective thermal conductivity model in closed form is then presented. Baoli et al 13 proposed the finite‐size particle method (FSP) and double‐distribution‐function (DDF) coupling model of the lattice Boltzmann method for fluid flow and heat transfer in porous media. The above research can simulate the heat‐flow coupling process of fractured rock mass at a macroscopic level.…”

Section: Introductionmentioning

confidence: 99%

Effects of fracture parameters and roughness on heat‐flow coupling in rock masses with two‐dimensional fracture networks

Fan

Yao

Zhang

et al. 2021

Energy Science & Engineering

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Discrete fracture network (DFN) is an effective means of describing the coupling of heat flow in an underground fractured rock mass. In this paper, an improved DFN is proposed by introducing the correlation function of fracture trace length and aperture, which is more consistent with the real fracture data. Next, based on the improved model, the influence of fracture roughness on the fluid flow and heat transmission was evaluated, and the relationship between the fracture aperture and the joint roughness coefficient (JRC) is established. Finally, based on the exponential function between confining pressure and aperture, the influence of confining pressure on the heat‐flow coupling process is considered in the improved model. Besides, the reliability of the model was verified by comparing with the analytical solution of the two‐dimensional single‐fracture heat‐flow coupling problem. The results show that under the same conditions, considering the correlation between the geometric parameters of the fracture, the seepage and heat transfer rates of the model increased, the outlet boundary flow reached the maximum value, and the average outlet temperature dropped rapidly. However, the fracture roughness reduces the outlet flow rate and the decline rate of average temperature. The confining pressure will lead to a decrease of about 3.5% in the outlet flow of the model, which is consistent with the seepage law in practical engineering. The model presented in this paper is an effective supplement to the two‐dimensional fracture network heat‐flow coupling model and can provide a theoretical basis and a numerical calculation tool for related underground rock mass engineering.

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Section: Introductionmentioning

confidence: 99%