The tendency of growing columnar dendrites to incline into the flow direction under the influence of some shear flow at the solidification front is a well-known phenomenon in directionally solidifying alloys. According to literature this effect is due to a deformation of the solute layer around a dendrite tip. It is assumed that solute-rich liquid is swept away from the upstream side of the dendrite tip to the downstream side, leading to a local enrichment of the solute and lowering of the solidus temperature on the downstream side. This gives preferential growth conditions on the upstream side, thus causing the crystal tips to incline upstream. On the basis of stirring experiments carried out at the Giesserei-Institut the deformation of the solute layer by forced convection at a 2-dimensional sine-wave-modulated interface and a 3-dimensional paraboloid of revolution was studied using a FEM-code (FIDAP) to solve the momentum and species transport equations under steady state conditions. The sine-wave-modulated interface could not account for the solute pile-up at the downstream side, especially after incorporating the influence of a solute partition coefficient at the interface. After adapting the 3-dimensional paraboloid to the analytic Ivantsov-solution describing the growth of an isoconcentrate dendrite tip a higher solute concentration could be observed at the downstream side of the dendrite tip. The results indicate that the sweep away effect actually occurs at the dendrite tip as long as the diffusion layers around the dendrite tips do not influence each other.
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