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Boussinesq-approksimationen×Stefan-Maxwell Diffusion×
FagområdeTermodynamikTermodynamik
FamilieProcess / pipelineProcess / pipeline
Oprindelsesår19031871
OphavspersonJoseph BoussinesqJosef Stefan and James Clerk Maxwell
TypeApproximation techniqueDiffusion equation
Oprindelig kildeBoussinesq, J. (1903). Théorie Analytique de la Chaleur. Gauthier-Villars. link ↗Reid, R. C., Prausnitz, J. M., & Poling, B. E. (1987). The Properties of Gases and Liquids (4th ed.). McGraw-Hill. ISBN: 978-0071247009
Aliasserbuoyancy approximation, Boussinesq modelStefan-Maxwell equation, multicomponent diffusion
Relaterede33
ResuméThe Boussinesq Approximation simplifies the governing equations for natural convection by treating density as constant except in the buoyancy term. This approximation is valid when temperature variations produce small density changes and allows researchers to solve coupled heat-fluid flow problems without solving the full, nonlinear compressibility equations. The Boussinesq Approximation is fundamental to analyzing buoyancy-driven flows in buildings, enclosures, and geophysical applications.The Stefan-Maxwell diffusion equation describes how multiple chemical species diffuse through each other in a mixture, accounting for interactions between all species pairs. Unlike Fick's law, which assumes species diffuse independently, Stefan-Maxwell theory captures the coupling that occurs when species with different diffusivities move at different rates. This is essential for analyzing gas separation, combustion, catalytic processes, and reactive distillation.
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ScholarGateSammenlign metoder: Boussinesq Approximation · Stefan-Maxwell Diffusion. Hentet 2026-06-17 fra https://scholargate.app/da/compare