Comparar métodos

	Leis de Fick	Aproximação de Boussinesq	Difusão de Stefan-Maxwell
Área	Termodinâmica	Termodinâmica	Termodinâmica
Família	Process / pipeline	Process / pipeline	Process / pipeline
Ano de origem	1855	1903	1871
Autor original	Adolf Fick	Joseph Boussinesq	Josef Stefan and James Clerk Maxwell
Tipo	Diffusion law	Approximation technique	Diffusion equation
Fonte seminal	Fick, A. (1855). On liquid diffusion. Philosophical Magazine, 10(63), 30-39.	Boussinesq, J. (1903). Théorie Analytique de la Chaleur. Gauthier-Villars.	Reid, R. C., Prausnitz, J. M., & Poling, B. E. (1987). The Properties of Gases and Liquids (4th ed.). McGraw-Hill. ISBN: 978-0071247009
Outros nomes	diffusion equation, Fickian diffusion	buoyancy approximation, Boussinesq model	Stefan-Maxwell equation, multicomponent diffusion
Relacionados	3	3	3
Resumo	Fick's Laws describe how species diffuse through media due to concentration gradients. The First Law (steady-state) relates diffusion flux to concentration gradient, while the Second Law (transient) describes how concentration changes over time. These laws are fundamental to mass transfer analysis, applying to gases, liquids, and solids. Fick's Laws are analogous to Fourier's Law of heat conduction, replacing temperature with concentration.	The 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.