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Transient Conduction into a Semi-infinite Solid: Screencasts

The equation for the transfer of heat into a semi-infinite solid is derived, and several related concepts are discussed.

We suggest that after watching this screencast, you list the important points as a way to increase retention.

This screencast shows simulations of six semi-infinite heat transfer scenarios. The boundary conditions and governing equations are discussed for each scenario.

We suggest that after watching this screencast, you list the important points as a way to increase retention.

Important Equations:

There are a number of ways to characterize a semi-infinite surface. A common approach is to assume the temperature at the surface is a constant. In this case, the temperature as a function of depth and time, \(T(x,t)\)  is:

\[T(x,t) = (T_0\, -\, T_S)erf\left( \frac{x}{\sqrt{4\alpha t}} \right)\,+\,T_S\]

where \(T_0\) (sometimes known as \(T_i\)) = initial temperature of the solid (°C),

\(T_S\) = constant surface temperature (°C),

\(x\) = depth below the surface (m),

\(\alpha\) = materials thermal diffusivity (m2/s), and

\(t\) = elapsed time (s).

A second approach is to assume heat transfer at the surface arises from convection. In this case, \(T(x,t)\) is:

\[T = T_0 \,+\, (T_{\infty} \, – \, T_0) \left[1 \,-\, erf \left( \frac{x}{\sqrt{4\alpha t}} \right) \,- \,exp \left( \frac{hx}{k} \, + \, \frac{h^2 \alpha t}{k^2}\right) \left( 1\,-\, erf\left( \frac{x}{\sqrt{4 \alpha t}} \,+\,\frac{h}{k} \sqrt{\alpha t}\right) \right) \right]\]

where \(T_{\infty}\) = temperature of the fluid (°C),

\(h\) = fluid’s heat transfer coefficient (W/m2-K),

and \(k\) = material’s thermal conductivity (W/m-K)

A third approach is to assume a constant heat flux at the surface. Not that \(T(x,t)\) in this equation will eventually go to inifinity. This is not realistic for long times:

\[T = T_0 \,+\, \frac{q”}{k} \left( \sqrt{\frac{4 \alpha t}{\pi}} exp\left( – \frac{x^2}{4 \alpha t} \right) -x \left(1 \,-\, erf\left( \frac{x}{\sqrt{4 \alpha t}} \right) \right) \right)\]

where \(q”\) = constant heat flux at the surface (W/m2)

Note there are several other approaches, which will not be reproduced here.

Important Definitions:

Error function: \(erf(z)\) is defined as \[erf(z) =\frac{2}{\sqrt{\pi}}\, \int^z _0 e^{-t^2} dt\] It must be calculated using software or looked up in a table. Note that \(erf(0) = 0\) and \(erf(\infty) = 1\).