Journal of Fluid Mechanics · 2006 · 326 citations · 22 references
EngineeringMaterials EngineeringMaterials ScienceFluid DynamicsSolid MechanicsSolidificationAlloy SolidificationFluid-flow In Porous MediaInterfacial HydrodynamicsSolid-liquid InterfacesSolidification ModelingSolidification Of MetalsAlloy Solidification BehaviorBinary Alloy SolidificationMacrosegregationMushy Zone DynamicsMushy Zone FormationMushy Zone ModelingTransition Zone AnalysisTransition Zone Structure
The study investigates how flow–solidification coupling in the mushy layer of binary alloy solidification affects macrosegregation patterns in corner flow. The authors compare a single‑domain Darcy–Brinkman model with a multiple‑domain Stokes–Darcy model and introduce a viscous transition zone inside the porous domain to enforce continuity of pressure and velocity. Macrosegregation predictions are highly sensitive to interfacial conditions; the newly proposed viscous transition zone yields agreement between single‑ and multiple‑domain models when porosity varies continuously across the interface.
The single-domain Darcy–Brinkman model is applied to some analytically tractable flows through adjacent porous and pure-fluid domains and is compared systematically with the multiple-domain Stokes–Darcy model. In particular, we focus on the interaction between flow and solidification within the mushy layer during binary alloy solidification in a corner flow and on the effects of the chosen mathematical description on the resulting macrosegregation patterns. Large-scale results provided by the multiple-domain formulation depend strongly on the microscopic interfacial conditions. No satisfactory agreement between the single- and multiple-domain approaches is obtained when using previously suggested conditions written directly at the interface between the liquid and the porous medium. Rather, we define a viscous transition zone inside the porous domain, where the Stokes equation still applies, and we impose continuity of pressure and velocities across it. This new condition provides good agreement between the two formulations of solidification problems when there is a continuous variation of porosity across the interface between a partially solidified region (mushy zone) and the melt.
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Dynamics of Fluids in Porous Media
Jacob Bear · Soil Science · 1975 · 9.8K citations
Dynamics of fluids in Porous Media
E. C. Childs · Engineering Geology · 1973 · 6.2K citations
Boundary conditions at a naturally permeable wall
G. S. Beavers, Daniel D. Joseph · Journal of Fluid Mechanics · 1967 · 3.1K citations
Engineering, Physics, Fluid Dynamics +16