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 <title>the theory of heat radiation part 1</title>
 <name>TheoryOfHeatRadiationPart1</name>
 <created>2006-02-01 03:26:14</created>
 <modified>2006-02-01 03:27:06</modified>
 <type>Definition</type>
<parent id="110">the theory of heat radiation</parent>
 <creator id="1" name="bloftin"/>
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 <author id="1" name="bloftin"/>
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	<category scheme="msc" code="05.70.-a"/>
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	<object name="heat"/>
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 <content>\subsection{Chapter I: General Introduction}

{\bf 1.}  Heat may be propagated in a stationary medium in two entirely different ways, namely, by conduction and by radiation.  Conduction of heat depends on the temperature of the medium in which it takes place, or more strictly speaking, on the non-uniform distriution of the temperature in space, as measured by the temperature gradient.  In a region where the temperature of the medium is the same at all points there is no trace of heat conduction.


\subsection{References}

This entry is a derivative of [1], a public domain work.

[1] Planck, M. "The Theory of Heat Radiation" Translation by Morton Masius, P. Blakiston's Son \&amp; CO., Philadephia, 1914.</content>
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