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In porous media

Capillary pressure gradients and Marongoni flow induce flow in porous media comprising glass beads or sand particles [40-42], Wetting and spreading processes are an important consideration in the development of inkjet inks and paper or transparency media [43] see the article by Marmur [44] for analysis of capillary penetration in this context. [Pg.470]

At the present time there exist no flux relations wich a completely sound cheoretical basis, capable of describing transport in porous media over the whole range of pressures or pore sizes. All involve empiricism to a greater or less degree, or are based on a physically unrealistic representation of the structure of the porous medium. Existing models fall into two main classes in the first the medium is modeled as a network of interconnected capillaries, while in the second it is represented by an assembly of stationary obstacles dispersed in the gas on a molecular scale. The first type of model is closely related to the physical structure of the medium, but its development is hampered by the lack of a solution to the problem of transport in a capillary whose diameter is comparable to mean free path lengths in the gas mixture. The second type of model is more tenuously related to the real medium but more tractable theoretically. [Pg.3]

The success of transport models must be measured by their ability to describe the results of flow and diffusion measurements in porous media. [Pg.4]

Ac Che limic of Knudsen screaming Che flux relacions (5.25) determine Che fluxes explicitly in terms of partial pressure gradients, but the general flux relacions (5.4) are implicic in Che fluxes and cheir solution does not have an algebraically simple explicit form for an arbitrary number of components. It is therefore important to identify the few cases in which reasonably compact explicit solutions can be obtained. For a binary mixture, simultaneous solution of the two flux equations (5.4) is straightforward, and the result is important because most experimental work on flow and diffusion in porous media has been confined to pure substances or binary mixtures. The flux vectors are found to be given by... [Pg.42]

Chapter 6. SOME IMPORTANT EXPERIMENTAL RESULTS ON GAS MOTION IN POROUS MEDIA And capillaries... [Pg.50]

Proposed flux models for porous media invariably contain adjustable parameters whose values must be determined from suitably designed flow or diffusion measurements, and further measurements may be made to test the relative success of different models. This may involve extensive programs of experimentation, and the planning and interpretation of such work forms the topic of Chapter 10, However, there is in addition a relatively small number of experiments of historic importance which establish certain general features of flow and diffusion in porous media. These provide criteria which must be satisfied by any proposed flux model and are therefore of central importance in Che subject. They may be grouped into three classes. [Pg.50]

Thus his experiments were the first to indicate the surprising result that relation (6,1) remains valid even in conditions where bulk diffusion resistance is completely dominant. Accordingly (6.1), perhaps the most important single experimental result on diffusion in porous media, will be referred to as Graham s relation. [Pg.52]

Chapter 8. MODELS OF FLOW AND DIFFUSION IN POROUS MEDIA... [Pg.63]

The WAG process has been used extensively in the field, particularly in supercritical CO2 injection, with considerable success (22,157,158). However, a method to further reduce the viscosity of injected gas or supercritical fluid is desired. One means of increasing the viscosity of CO2 is through the use of supercritical C02-soluble polymers and other additives (159). The use of surfactants to form low mobihty foams or supercritical CO2 dispersions within the formation has received more attention (160—162). Foam has also been used to reduce mobihty of hydrocarbon gases and nitrogen. The behavior of foam in porous media has been the subject of extensive study (4). X-ray computerized tomographic analysis of core floods indicate that addition of 500 ppm of an alcohol ethoxyglycerylsulfonate increased volumetric sweep efficiency substantially over that obtained in a WAG process (156). [Pg.193]

Sulfonates for Enhanced Oil Recovery. The use of hydrocarbon sulfonates for reducing the capillary forces in porous media containing cmde oil and water phases was known as far back as 1927—1931 (164,165). Interfacial tensions between 10 and 10 N/m or less were estabUshed as necessary for the mobilization and recovery of cmde oil (166—169). [Pg.82]

Figure 2.10 Capillary model for fluid flow in porous media... Figure 2.10 Capillary model for fluid flow in porous media...
Again, an alternative approaeh to the predietion of bed pressure drop and fluid flow in porous media is to use frietion faetors (the analogue of the drag eoeffieient developed for partiele flow above). [Pg.41]

Foscolo, P.U., Gibilaro, L.G. and Waldram, S.P., 1983. A unified model for particulate expansion of fluidised beds and flow in porous media. Chemical Engineering Science, 38, 1251-1260. [Pg.306]

V. Yamakov, D. Stauffer, A. Milchev, G. M. Foo, R. B. Pandey. Crossover dynamics for polymer simulation in porous media. Phys Rev Lett 79 2356-2358, 1997. [Pg.625]

For systems where the bulk freezing transition is well understood, one may want to go one step further and investigate the modifications of the phase transition and the sohd phases in the event of external influence on the system. Flow does freezing happen in a confined situation where external boundaries are present What is freezing in porous media like A related question is What does the interface between sohd and liquid look like This is an intrinsic inhomogeneity that the system builds up by itself (if, as usual, the transition is first order). Let us describe some papers dealing with freezing under external influence. [Pg.760]

The filtration, or superficial face, velocities used in fabric filters are generally in the range of 1 to 10 feet per minute, depending on the type of fabric, fabric supports, and cleaning methods used. In this range, pressure drops conform to Darcy s law for streamline flow in porous media, which states that the pressure drop is directly proportional to the flow rate. The pressure drop across the... [Pg.779]

For a while now, the problem of flow and heat transfer in heated capillaries has attracted attention from a number of research groups, with several applications to engineering. The knowledge of the thermohydrodynamic characteristics of capillary flow with evaporative meniscus allows one to elucidate the mechanism of heat and mass transfer in porous media, to evaluate the efficiency of cooling system of electronic devices with high power density, as well as to optimize MEMS. [Pg.349]

There are comparable incentives to develop new process-related materials that are more selective as catalysts, extractants, or separation membranes and more effective in controlling flow in porous media. In addition, the development of materials that are less energy intensive in terms of production and use is a goal equivalent to other means of energy conservation. [Pg.115]

The issues of selection of the spatial wavelength and the deterministic character of the fine scale features of the microstructure are closely related to similar questions in nonlinear transitions in a host of other physical systems, such as macroscopic models of immiscible displacement in porous media - - the Hele Shaw Problem (15) - and flow transitions in fluid mechanical systems (16). [Pg.300]

A number of different approaches have been taken to describing transport in porous media. The objective here is not to review all approaches, but to present a framework for comparison of various approaches in order to highlight those of particular interest for analysis of diffusion and electrophoresis in gels and other nanoporous materials. General reviews on the fundamental aspects of experiments and theory of diffusion in porous media are given... [Pg.562]

The objective of most of the theories of transport in porous media is to derive analytical or numerical functions for the effective diffusion coefficient to use in the preceed-ing averaged species continuity equations based on the structure of the media and, more recently, the structure of the solute. [Pg.565]

Many investigators have studied diffusion in systems composed of a stationary porous solid phase and a continuous fluid phase in which the solute diffuses. The effective transport coefficients in porous media have often been estimated using the following expression ... [Pg.566]


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See also in sourсe #XX -- [ Pg.815 , Pg.816 , Pg.818 , Pg.1155 , Pg.1171 ]

See also in sourсe #XX -- [ Pg.116 , Pg.139 , Pg.265 , Pg.266 , Pg.267 , Pg.268 ]




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Applications in Porous Media

Axial Dispersion and Mass Transfer Resistance in Porous Media

Capillary Imbibition of Surfactant Solutions in Porous Media and Thin Capillaries Partial Wetting Case

Classical Theory of Diffusion and Seepage Problems in Porous Media

Condensation in porous media

Coupling of transport and reaction in porous media

Darcy flow in porous media and polymer apparent viscosity

Determination of Pore Size Distribution in Porous Media

Diffusion Coefficients in Porous Media

Diffusion and Seepage Problem for a Multi-component Solution in Saturated Porous Media

Diffusion in porous media

Diffusion of Colloidal Fluids in Random Porous Media

Dissolution, in porous media

Effect of Curvature on Saturation. Pressure Condensation and Vaporization in Porous Media

Electrokinetic Flow in Porous Media

Electroosmosis in Porous Media

Electroosmotic Flow in Porous Media

Entropy Effects in Phase Distribution Porous Media

Evaporation in porous media

Experimental measurement of polymer retention in porous media

Fires in porous media natural and urban canopies

Flow and Dissolution in Porous Media

Flow in porous media

Fluid Friction in Porous Media

Fluid transport, in porous media

Foam flow in porous media

Foam flowing in porous media

Foam formation in porous media

Foam in porous media

Foam transport, in porous media

Formation in porous media

Gas-transport in porous media

HA for Diffusion Problems in Porous Media

Heat transfer in porous media

Homogenization Analysis of Diffusion in Porous Media

Impact Factors of Polymer Rheology in Porous Media

Introductory overview of polymer adsorption in porous media

Location of Adsorbates in Porous Media

Mass transfer resistance in porous media

Mass transport in porous media

Microscale processes in porous media

Migration of Liquids in Porous Media

Models of Mass Transport in Porous Media

Momentum Equation in Porous Media

Multiphase Mass Transport in Channels and Porous Media

Multiphase flow in porous media

Multiscale HA for Diffusion Problems in Porous Media

NMR Pore Size Measurements Using an Internal Magnetic Field in Porous Media

NMR in gels and porous media

Natural Convection and Diffusion in Porous Media

Natural convection in porous media

Network modelling of non-Newtonian fluids in porous media

Phase change in porous media

Polydispersity effects in polymer transport through porous media

Polymer retention in porous media

Polymer rheology in porous media

Polymer transport in porous media

Polymers adsorption in porous media

Porous media

Propagation in porous media

Quasi-Detonation in Porous Medium

SOME IMPORTANT EXPERIMENTAL RESULTS ON GAS MOTION IN POROUS MEDIA AND CAPILLARIES

Single-phase flow, in porous media

Species Movement and Transfer in a Porous Medium

The Freezing of Soils Ice in a Porous Medium and Its Environmental Significance

Thermal conductivity, in porous media

Transport Mechanisms in Porous Media

Transport in Porous Media

Two-phase flow, in porous media

Y. Ichikawa and A.P.S. Selvadurai, Transport Phenomena in Porous Media

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