Modeling two-phase flow in a micro-model with local thermal non-equilibrium on the Darcy scale. (September 2015)

• Record Type: Journal Article
• Authors: Nuske, Philipp; Ronneberger, Olaf; Karadimitriou, Nikolaos K.; Helmig, Rainer; Hassanizadeh, S. Majid
• Is Part Of: International journal of heat and mass transfer. Volume 88(2015:Sep.)
• Page Start: 822
• Page End: 835
• Publication Date: 2015-09
• Subjects: Two-phase flow in porous media -- Local thermal non-equilibrium -- Image analysis -- Determination of constitutive relations -- Local equilibrium assumptions -- Model calibration -- Macro-scale non-equilibrium model; Heat -- Transmission -- Periodicals; Mass transfer -- Periodicals; Chaleur -- Transmission -- Périodiques; Transfert de masse -- Périodiques; Electronic journals; 621.4022
• DOI: 10.1016/j.ijheatmasstransfer.2015.04.057
• Languages: English
• ISSNs: 0017-9310

Abstract

Highlights: Proof of concept: macro-scale local thermal non-equilibrium model and experiment. Phase specific temperature measurements in a porous medium. Image analysis procedure for determining all interfacial areas. Providing all employed source code to the scientific community. Abstract: Loosening local equilibrium assumptions in two-phase flow in porous media gives rise to new, unknown variables. More specifically, when loosening the local thermal equilibrium assumption, one has to describe the heat transfer between multiple phases, present at the same mathematical point. In this paper, we calibrate a macro-scale mathematical model which is free of local equilibrium assumptions to experimental observations. We emphasize the correct determination and upscaling of necessary input parameters from the experimental data achieved by image analysis. By choosing an appropriate scaling parameter, we are able to reproduce experimental measurements satisfactorily. This is a first step towards quantifying heat transfer in two-phase flow in porous media. Ultimately, our aim is to find the limits of the applicability of local equilibrium assumptions in two-phase flow in porous media.