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Journal ArticleDOI

A special case of spatial averaging of the diffusion coefficient

Yu. I. Babenko
- 01 Jan 2005 - 
- Vol. 39, Iss: 1, pp 98-102
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TLDR
In this article, it is shown that if the coordinate dependence of the diffusion coefficient is described by the product of functions depending on different coordinates, then the surfaces of equal concentration coincide with the coordinate planes.
Abstract
Steady-state mass transfer through a heterogeneous layer formed by coordinate planes of an orthogonal coordinate system is considered under the assumption that the boundary conditions at both layer boundaries are independent of coordinates. It is established that, if the coordinate dependence of the diffusion coefficient is described by the product of functions depending on different coordinates, then the surfaces of equal concentration (isohalines) coincide with the coordinate planes. It is shown that, in this case, the diffusion problem has an exact solution and the averaging of the diffusion coefficient is performed by elementary methods.

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Citations
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Inequalities constraining the value of the averaged diffusion coefficient in a heterogeneous layer

TL;DR: In this paper, the steady-state diffusion in a heterogeneous medium bounded by parallel planes with fixed concentrations at the boundaries is studied and an analytical solution in terms of a small-parameter power series taking into account a quadratic expansion term is obtained.
References
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Book

Momentum, Energy and Mass Transfer in Continua

TL;DR: Momentum, energy, and mass transfer in continua, Momentum and energy, mass transfer and energy transfer in continuous continua, this paper,...,.
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An averaged-equation approach to particle interactions in a fluid suspension

TL;DR: In this article, the same prescription is applied to fields averaged with one particle fixed, and equations are produced containing a term averaged with two particles fixed and so on up an infinite hierarchy.
Journal ArticleDOI

Asymptotic solution of the problem of unsteady heat transfer into a stratified medium

TL;DR: In this article, an asymptotic expression for the heat flux at the boundary of a semi-infinite region at long times under the assumption that the temperature at this boundary is a function of time is derived.
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