Discrete Ordinates Method(DOM)is a model for thermal radiation exchange in opaque media.In this study,the DOM formulation is employed within the framework of the Discrete Element Method coupled with Computational Flui...Discrete Ordinates Method(DOM)is a model for thermal radiation exchange in opaque media.In this study,the DOM formulation is employed within the framework of the Discrete Element Method coupled with Computational Fluid Dynamics(DEM-CFD),thus including full radiative heat exchange among the phases involved.This is done by adjusting the absorption coefficient,emission coefficient,and net radiative heat flux of particles by incorporating local porosity into equations.A key objective is to represent radiation propagation for different packing densities in packed beds accurately.The model is validated by comparing the results with available data from the literature for simulations with a P1 radiation model and corresponding experiments.The validation configuration is a heated box filled with spherical particles under vacuum conditions.As an application example,the radiative heat exchange between an enclosure at high temperature and moving layers of spherical particles concurrently passed by a gas in crossflow is studied.Three packing densities(dilute,moderate,and dense)are examined to evaluate radiation penetration into the particle ensemble.Convective and contact heat transfer are also considered.The DEM-CFD coupling is a non-resolved approach,where the influence of particles on the flow field is accounted for by momentum and energy source terms together with a porosity field(Averaged Volume Method(AVM)).Effect of convective,conductive and radiative heat transfer is analysed based on the evolution of incident radiation flux,spatial distributions of particle surface and fluid temperatures,and particle temperature histograms.It becomes obvious that radiation dominates the system,and that packing density defines the penetration depth of radiation.Conduction mainly leads to a smoothening of particle temperature distribution in the system.展开更多
基金funded by the Deutsche Forschungsgemeinschaft(DFG,German Research Foundation)–Project-ID 422037413–TRR 287Gefördert durch die Deutsche Forschungsgemeinschaft(DFG)–Projektnummer 422037413–TRR 287.
文摘Discrete Ordinates Method(DOM)is a model for thermal radiation exchange in opaque media.In this study,the DOM formulation is employed within the framework of the Discrete Element Method coupled with Computational Fluid Dynamics(DEM-CFD),thus including full radiative heat exchange among the phases involved.This is done by adjusting the absorption coefficient,emission coefficient,and net radiative heat flux of particles by incorporating local porosity into equations.A key objective is to represent radiation propagation for different packing densities in packed beds accurately.The model is validated by comparing the results with available data from the literature for simulations with a P1 radiation model and corresponding experiments.The validation configuration is a heated box filled with spherical particles under vacuum conditions.As an application example,the radiative heat exchange between an enclosure at high temperature and moving layers of spherical particles concurrently passed by a gas in crossflow is studied.Three packing densities(dilute,moderate,and dense)are examined to evaluate radiation penetration into the particle ensemble.Convective and contact heat transfer are also considered.The DEM-CFD coupling is a non-resolved approach,where the influence of particles on the flow field is accounted for by momentum and energy source terms together with a porosity field(Averaged Volume Method(AVM)).Effect of convective,conductive and radiative heat transfer is analysed based on the evolution of incident radiation flux,spatial distributions of particle surface and fluid temperatures,and particle temperature histograms.It becomes obvious that radiation dominates the system,and that packing density defines the penetration depth of radiation.Conduction mainly leads to a smoothening of particle temperature distribution in the system.
