2022
DOI: 10.1088/1361-648x/ac623e
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Analysis of the boundary integral equation for the growth of a parabolic/paraboloidal dendrite with convection

Abstract: The growth of a parabolic/paraboloidal dendrite streamlined by viscous and potential flows in an undercooled one-component melt is analyzed using the boundary integral equation. The total melt undercooling is found as a function of the P\'eclet, Reynolds, and Prandtl numbers in two- and three-dimensional cases. The solution obtained coincides with the modified Ivantsov solution known from previous theories of crystal growth. Varying P\'eclet and Reynolds numbers we show that the melt undercooling practically c… Show more

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Cited by 3 publications
(6 citation statements)
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“…At a → 1 (figure 2) we might have expected the transition to the 2D case. However, in 2D with the same Péclet number p, the undercooling is larger than in 3D, and we have the opposite situation [11]. Namely, the undercooling in figure 2 becomes lower with increasing the ellipticity parameter a.…”
Section: Resultsmentioning
confidence: 66%
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“…At a → 1 (figure 2) we might have expected the transition to the 2D case. However, in 2D with the same Péclet number p, the undercooling is larger than in 3D, and we have the opposite situation [11]. Namely, the undercooling in figure 2 becomes lower with increasing the ellipticity parameter a.…”
Section: Resultsmentioning
confidence: 66%
“…Note that a = 0 corresponds to the previously studied case of the paraboloid of revolution [10,11]. The theory under consideration has a limiting transition at a → 0 to this simpler case of the convective BIE.…”
Section: Resultsmentioning
confidence: 99%
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“…(i) A numerical simulation of dendritic growth in an inclined liquid flow should be carried out, taking into account the conductive and convective heat and mass transfer on various (with respect to the flow) sides of the dendrite. Such simulations can be done using a direct solution of the heat and mass transfer problem with flow (e.g., the phase-field or enthalpy methods) [53][54][55][56], as well as using the convective boundary integral equation [57][58][59]; (ii) Intense convective currents on the upstream side of the dendrite are a potential source of morphological instability on its surface. It is therefore necessary to study the surface stability of the dendrite crystal to small morphological perturbations on its upstream side.…”
Section: Discussionmentioning
confidence: 99%