Jpn. J. Appl. Phys. 12 (1973) pp. 1160-1164 |Next Article| |Table of Contents|
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(Received July 30, 1971)
The equations are derived for giving the temperature of parallelepiped, when heat waves are applied to the surfaces perpendicular to the x-coordinate, and heat losses of the second kind of boundary condition are found an the other surfaces perpendicular to the y and z-coordinates. The results show that there is no change of phase in the plane perpendicular to the x-coordinate and only the amplitude reduction of the heat-wave occurs towards the edge of the y and z-coordinates.
URL:
http://jjap.jsap.jp/link?JJAP/12/1160/
DOI: 10.1143/JJAP.12.1160