2009
DOI: 10.1016/j.ijheatmasstransfer.2009.04.014
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Eigenfunction expansions for transient diffusion in heterogeneous media

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Cited by 59 publications
(83 citation statements)
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“…The Sturm-Liouville eigenvalue problems presented in Table 3 are solved by the GITT itself (Cotta, 1993;Naveira-Cotta, 2009). For this purpose, two auxiliary eigenvalue problems with known analytical solution are required and proposed according to Table 4:…”
Section: Solution Methodologymentioning
confidence: 99%
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“…The Sturm-Liouville eigenvalue problems presented in Table 3 are solved by the GITT itself (Cotta, 1993;Naveira-Cotta, 2009). For this purpose, two auxiliary eigenvalue problems with known analytical solution are required and proposed according to Table 4:…”
Section: Solution Methodologymentioning
confidence: 99%
“…The integral transformation for the main eigenvalue problems presented in Table 3 is accomplished by multiplying the respective normalized auxiliary eigenfunction given in Table 4 for each eigenvalue problem, followed by integration over the domain [0,1] in the Y direction, and then substituting the inversion formula for the original eigenfunctions (Cotta, 1993;Naveira-Cotta, 2009). After the described integral transformation, the following algebraic systems for calculating the eigenvalues and corresponding eigenvectors are obtained:…”
Section: Solution Methodologymentioning
confidence: 99%
“…The approach here employed in the direct problem solution for forced convection in micro-channels, is borrowed from a recent work on diffusion in heterogeneous media, with arbitrarily space variable thermophysical properties [13]. In this sense, the dimensionless velocity fields are mathematically equivalent to space variable thermal capacitances, and the formal solution procedure is here briefly described.…”
Section: Direct Problem Solutionmentioning
confidence: 99%
“…We consider a general formulation on steady or quasi-steady state hydrodynamically fully developed and thermally developing convection, that governs the temperature field T(x, z), dependent on the position x on the transversal plane and on the longitudinal coordinate z, defined in the transversal region V with boundary surface S. The formulation includes the convection term, the diffusion operator, a linear dissipation term, and an independent source term [13], as shown in problem (1) below. The coefficients w(x), k(x), and d(x), are responsible for the information related to the velocity field, geometry and eventually even heterogeneity of the medium.…”
Section: Direct Problem Solutionmentioning
confidence: 99%
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