Heat diffusion at the boundary of stratified media - Homogenized temperature field and thermal constriction

被引：15

作者：

Fudym, O

Batsale, JC

Lecomte, D

机构：

[1] Univ Santiago Chile, Dept Ingn Mecan, Santiago, Chile

[2] CNRS, ENSAM, LEPT UMR 8508, F-33405 Talence, France

[3] CNRS, EMAC, LGPSD, UMR 2392, F-81013 Albi, France

来源：

INTERNATIONAL JOURNAL OF HEAT AND MASS TRANSFER | 2004年 / 47卷 / 10-11期

关键词：

This work was funded by the chilean FONDECYT program (Award # 1020349). The authors also gratefully acknowledge the support of the French Embassy in Santiago de Chile;

D O I：

10.1016/j.ijheatmasstransfer.2003.11.014

中图分类号：

O414.1 [热力学];

学科分类号：

摘要：

Heat diffusion in stratified materials with the layers running parallel to the main heat flux direction is analyzed with special emphasis on the temperature field near the boundaries. In a previous work, a semi-analytical general solution was proposed as an extension of the thermal quadrupole method for heat conduction in heterogeneous media. In this paper, the steady solution is separated into an homogenized transfer in series with a constriction term, and a conductive boundary layer is defined. The same decomposition method is implemented for the semi-infinite transient case, and some simplified models are obtained from asymptotic expansions. For long times, the transient averaged signal is found to be superposed to the steady constriction matrix effect. The main application is to better envision experimental temperature field analysis for thermal non-destructive evaluation methods. (C) 2003 Elsevier Ltd. All rights reserved.

引用

页码：2437 / 2447

页数：11

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