Gaseous mass transport in porous media through a stagnant gas
An analysis is presented for gas-phase mass transport in porous media through a stagnant gas. The natural flux ratio rule for isobaric conditions, which requires that the fluxes be inversely proportional to the square roots of the molecular weights, is not met in this system. Accordingly, a pressure difference develops and this superimposes viscous flow upon diffusion. Equations are derived for the flux and the pressure difference, and it is shown that even when the pressure difference is small, the contribution of viscous flow to the flux can be considerable. Flux and pressure difference measurements carried out on the transport of carbon dioxide through stagnant nitrogen in a septum of coarse pores (average pore size 2.5 ..mu..m) are in agreement, within experimental error, with those predicted by the equations.
- Research Organization:
- Dept. of Metallurgy and Materials Science, Imperial College of Science and Technology, London SW7 2BP
- OSTI ID:
- 6227137
- Journal Information:
- Ind. Eng. Chem. Res.; (United States), Vol. 26:1
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
ORGANIC
PHYSICAL AND ANALYTICAL CHEMISTRY
CARBON DIOXIDE
FLOW MODELS
VISCOUS FLOW
POROUS MATERIALS
GAS FLOW
MASS TRANSFER
DIFFUSION
EQUATIONS
MOLECULAR WEIGHT
NITROGEN
PRESSURE GRADIENTS
CARBON COMPOUNDS
CARBON OXIDES
CHALCOGENIDES
ELEMENTS
FLUID FLOW
MATERIALS
MATHEMATICAL MODELS
NONMETALS
OXIDES
OXYGEN COMPOUNDS
400201* - Chemical & Physicochemical Properties