By Yehuda Bachmat, Jacob Bear (auth.), Jacob Bear, M. Yavuz Corapcioglu (eds.)
This quantity comprises the lectures offered on the NATO complex learn INSTITUTE that happened at Newark, Delaware, U. S. A. , July 14-23, 1985. the target of this assembly was once to offer and talk about chosen subject matters linked to shipping phenomena in porous media. by way of their very nature, porous media and phenomena of shipping of in depth amounts that occur in them, are very advanced. the forged matrix can be inflexible, or deformable (elastically, or following another constitutive relation), the void area can be occupied via a number of fluid levels. every one fluid section should be composed of multiple part, with a few of the elements able to interacting between themselves and/or with the forged matrix. The delivery procedure can be isothermal or non-isothermal, without or with section adjustments. Porous medium domain names within which large amounts, equivalent to mass of a fluid part, portion of a fluid part, or warmth of the porous medium as a complete, are being transported take place within the perform in numerous disciplines.
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Extra resources for Advances in Transport Phenomena in Porous Media
Wash with HN03 t GlOSS -J Polymerisecl photoresist ~ Silver ~ Glass Glass slide 10 \ D,D I Glass 01 MICROMODEL - drill and affix tubing In 1 drain Out Figure 2. Preparation of glass micromodel. 56 (a) Hand-drawn parallel layer model with serial heterogeneities. This was designed to yield realistic and predictable relative permeability and capillary pressure functions. (b) Computer drawn regular network of curved channels with reducing pore throat sizes, to investigate fines movement and entrapment.
By comparing Eq. 3) and Eq. 4) with Eqs. 13 we conclude that the case on hand is identical to Case B of Appendix, with T f = Ga and Ts = GS' Hence, making use of Eq. 5) An analogous expression, in terms of 8 s = 1 - nand 8 T* = S"s § - efI~ (see Eq. 15)) can be written for the macroscopic heat flux, in the solid phase. We have thus achieved our goal of expressing the macroscopic heat fluxes in terms of the macroscopic state variables. It is interesting to note the basic difference between Eq. 8) and Eq.
17) reduces to Eq. 11), corresponding to Case A. The same holds when AafAS' but G~ = G~ throughout the entire porous medium domain. 6. APPENDIX B: THE COEFFICIENT I~ The coefficient Ia* ' defined in Eq. 9 ) represents the . stat~c moment of oriented areal elements of Saa , with respect to planes passing through ~o' per unit volume of the a phase within (U o )' * ·, To obtain an estimate of the magnitude of the components Tai consider a spherical REV oL radiusR. Then, Eq. V aJ. on lS aa ). The term vaiv aj is a symmetric second rank tensor.