学术文献库

Fully resolved simulations are used to quantify the effects of heat transfer in the presence of buoyancy on the drag of a spatially fixed heated spherical particle at low Reynolds numbers ($Re$) in the range $10^{-3} \le Re \le 10$ in a variable property fluid. The amount of heat addition from the sphere encompasses both, the heating regime where the Boussinesq approximation holds and the regime where it breaks down. The particle is assumed to have a low Biot number which means that the particle is uniformly at the same temperature and has no internal temperature gradients. Scaling buoyancy with inertial and viscous forces yields two related non-dimensional quantities, called Buoyancy Induced Viscous Reynolds Number ($Re_{BV}$) and Buoyancy Induced Inertial Reynolds Number ($Re_{BI}$). For ideal gases, $Re_{BV}$ is analogous to the Grashof number ($Gr$). No assumptions are made on the magnitude of $Re_{BI}$ (or equivalently $Re_{BV}$). The effects of the orientation of gravity relative to the free-stream velocity are examined. Large deviations in the value of the drag coefficient are observed when the Froude number ($Fr$) decreases and/or the temperature of the sphere increases. Under appropriate constraints on $Re_{BI}$ and $Re$, the total drag on a heated sphere in a low $Re$ flow in the presence of buoyancy (mixed convection) is shown to be, within 10% error, the linear superposition of the drag computed in two canonical setups: one being the drag on a steadily moving heated sphere in the absence of buoyancy (forced convection) and the other being natural convection. However, the effect of temperature variation on the drag of a sphere in both, forced and natural convection, is significant.