derivation of heat equation
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(Derivation)
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Let us consider the heat conduction in a homogeneous matter with density and specific heat capacity . Denote by
the temperature in the point
at the time . Let be a simple closed surface in the matter and the spatial region restricted by it.
When the growth of the temperature of a volume element in the time is , the element releases the amount
of heat, which is the heat flux through the surface of . Thus if there are no sources and sinks of heat in , the heat flux through the surface in is
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(1) |
On the other hand, the flux through in the time must be proportional to , to and to the derivative of the temperature in the direction of the normal line of the surface element , i.e. the flux is
where is a positive constant (because the heat flows always from higher temperature to lower one). Consequently, the heat flux through the whole surface is
which is, by the Gauss's theorem, same as
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(2) |
Equating the expressions (1) and (2) and dividing by , one obtains
Since this equation is valid for any region in the matter, we infer that
Denoting
, we can write this equation as
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(3) |
This is the differential equation of heat conduction, first derived by Fourier.
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"derivation of heat equation" is owned by pahio.
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See Also: derivation of wave equation
This object's parent.
Cross-references: differential equation, theorem, flux, volume, temperature, conduction, heat
This is version 1 of derivation of heat equation, born on 2009-01-20.
Object id is 417, canonical name is DerivationOfHeatEquation.
Accessed 385 times total.
Classification:
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Pending Errata and Addenda
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