CONVECTIVE HEAT TRANSFER OF A SEDIMENTING MONODISPERSE SUSPENSION IN A FLAT CHANNEL UNDER BOUNDARY CONDITIONS OF THE SECOND KIND
Based on the phenomenological representations of interpenetrating continuums for phases moving without slippage in a laminar regime, a low concentration monodisperse suspension in a flat horizontal channel under conditions of sedimentation of solid particles, an analytical solution of the heat transfer problem is obtained for a known heat flow through wetted surfaces .