Abstract

Dissipative particle dynamics is a Lagrangian particle-based mesoscopic technique with higher computation efficiency than microscopic numerical methods, originally conceived as a hybrid of lattice gas automata (LGA), Brownian dynamics (BD) and molecular dynamics (MD). As an improved version of this method, the energy-conservative dissipative particle dynamics (eDPD or DPD+E) allows for temperature-variation in fluid system and has great potential to solve hydrodynamics problem involving heat transfer in complex fluids such as biomagnetic fluid, ferrofluid, eletrorheological fluid and so on. Considering the both effects of ferrohydrodynamic and magnetohydrodynamic, the hydrodynamics behavior of biomagnetic fluid is rather complicated and has received considerable attention from various researchers. In this work, the fluid flow and heat transfer in a semi-annulus filled with biomagnetic fluid in presence of an external magnetic field is investigated systematically by the eDPD method for different conditions. The flow is steady, two-dimensional, laminar and incompressible. To begin with, a simple and practicable strategy is proposed to matchup the mesoscopic parameters in eDPD model with the transport coefficients of real fluid because the eDPD formlation has no direct relation to transport coefficients. In detail, the viscosity and thermal diffusivity for the eDPD fluid are calculated by numerically simulating the isothermal Poiseuille flow and two-dimensional heat conduct with uniform heat generation, respectively. To study the magnetostatic interactions regardless of the induced magnetic field, a model concerned with the magnetic field is introduced. The Kelvin force and Lorentz force on DPD particles are computed in the same way as the buoyance force; the heat source induced by the external magnetic is replaced by imposing an external heat flux on the DPD particles. Then the eDPD model is first validated against the finite volume method (FVM) results for the natural convection at a given Rayleigh number and Prandtl number to access the accuracy of the eDPD simulations and it is found that the eDPD model predict the temperature and flow fields throughout the convection domains properly. Finally the effects of Magnetic number and Hartmann number, which arise from ferrohydrodynamics and magnetohydrodynamics respectively, have been examined and presented via temperature isotherms and streamlines. The obtained results simply reveal that the thermomagnetic convection is very different from buoyance-driven natural convection. Three thermal plume and four vortexes appears over the hot wall and heat transfer drop a lot near the middle zone as Magnetic number increases. It can be also found that the local Nusselt number near the hot wall significantly decrease as Hartmann number increases.

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