Hostname: page-component-cd9895bd7-gbm5v Total loading time: 0 Render date: 2024-12-23T11:36:47.434Z Has data issue: false hasContentIssue false

A discrete random walk model for diffusion in media with double diffusivity

Published online by Cambridge University Press:  17 February 2009

James M. Hill
Affiliation:
Department of Mathematics, University of Wollongong, Wollongong, New South Wales 2500
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Diffusion in the presence of high-diffusivity paths is an important issue of current technology. In metals, high-diffusivity paths are identified with dislocations, grain boundaries, free surfaces and internal microcracks. In pourous media such as rocks, fissures provide a system of high-flow paths. Recently, based on a continuum approach, these phenomena have been modelled, resulting in coupled systems of partial differential equations of parabolic type for the concentrations in bulk and in the high-diffusivity paths. This theory assumes that each point of the medium is simultaneously occupied by more than one diffusion or flow path. Here a simple discrete random walk model of diffusion in a medium with double diffusivity is given.

Type
Research Article
Copyright
Copyright © Australian Mathematical Society 1980

References

[1]Aifantis, E. C., “Introducing a multiporous medium”, Developments in mechanics, Proc. 15th Midwestern Mech, Conf. 8 (1977), 209211.Google Scholar
[2]Aifantis, E. C., “A new interpretation of diffusion in high-diffusivity paths—a continuum approach”, Acta Metall. 27, (1979), 683691.CrossRefGoogle Scholar
[3]Aifantis, E. C., “Continuum basis for diffusion in regions with multiple diffusivity”, J. Appl. Phys. 50 (1979), 1334–338.CrossRefGoogle Scholar
[4]Aifantis, E. C. and Hill, J. M., “On the theory of diffusion in media with double diffusivity. Part I. Basic mathematical results”, Quart. J. Mech. Appl. Math. 33 (1980).CrossRefGoogle Scholar
[5]Barenblatt, G. I., Zheltov, lu. P. and Kochina, I. N., “Basic concepts in the theory of seepage of homogenous liquids in fissured rocks [strata]”, J. Appl. Math. Mech. 24 (1960), 12861303.CrossRefGoogle Scholar
[6]Barnett, V. D., “A simple random walk on parallel axes moving at different rates”, J. Appl. Prob. 12 (1975), 466476.CrossRefGoogle Scholar
[7]Crank, J., Mathematics of diffusion (Oxford University Press, 2nd edition, 1967).Google Scholar
[8]Eidelman, S. D., Parabolic systems (North-Holland Pub. Co. Amsterdam, 1969).Google Scholar
[9]Feller, W., An introduction to probability theory and its applications, Vol. 2 (Wiley, 1966).Google Scholar
[10]Friedman, A., Partial differential equations of parabolic type (Prentice-Hall, 1964).Google Scholar
[11]Frisch, H. L. and Hammersley, J. M., “Percolation processes and related topics”, J. Soc. Indut. Appl. Math. 11 (1963), 894918.CrossRefGoogle Scholar
[12]Hill, J. M. and Aifantis, E. C., “On the theory of diffusion in media with double diffusivity. Part II. Boundary value problems”, Quart. J. Mech. Appl. Math. 33 (1980).CrossRefGoogle Scholar
[13]McNabb, A., “Comparison and existence theorems for multicomponent diffusion systems”, J. Math. Anal. Applics. 3 (1961), 133144.CrossRefGoogle Scholar
[14]Prabhu, N. U., Stochastic processes (Macmillan, 1966).Google Scholar
[15]Szarski, J., Differential inequalities (PWN, Warsaw, 1968).Google Scholar