Multiple steady flows in confined gaseous double diffusion with discrete thermosolutal sources
From MaRDI portal
Publication:5303573
DOI10.1063/1.2770518zbMath1182.76872OpenAlexW2059798928MaRDI QIDQ5303573
Di Liu, Fu-Yun Zhao, Guang-Fa Tang
Publication date: 18 March 2010
Published in: Physics of Fluids (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1063/1.2770518
Related Items
Convection driven by temperature and composition flux with the same diffusivity ⋮ Direct and inverse mixed convections in an enclosure with ventilation ports ⋮ Non-unique convection in a three-dimensional slot-vented cavity with opposed jets ⋮ Determining boundary heat flux profiles in an enclosure containing solid conducting block ⋮ Transitions and oscillations in a thermohaline deep ocean circulation model ⋮ Numerical determination of boundary heat fluxes in an enclosure dynamically with natural convection through Fletcher-Reeves gradient method ⋮ Natural convection in an enclosure with localized heating and salting from below
Cites Work
- Unnamed Item
- Application issues of the streamline, heatline and massline for conjugate heat and mass transfer
- A consistently formulated QUICK scheme for fast and stable convergence using finite-volume iterative calculation procedures
- Cooperating thermosolutal convection in enclosures. I: Scale analysis and mass transfer. II: Heat transfer and flow structure
- The nature of vertical natural convection flows resulting from the combined buoyancy effects of thermal and mass diffusion
- Multiplicity of equilibrium states in laterally heated thermosolutal systems with equal diffusivity coefficients
- Double diffusive convection in a cubic enclosure with opposing temperature and concentration gradients
- Double diffusion natural convection in a rectangular enclosure filled with binary fluid saturated porous media: The effect of lateral aspect ratio
- Bifurcation phenomena in confined thermosolutal convection with lateral heating: Commencement of the double-diffusive region
- Double diffusion in a vertical fluid layer: Onset of the convective regime
- Three-dimensional double-diffusive convection in a porous cubic enclosure due to opposing gradients of temperature and concentration