The heat transfer coefficient for conduction is k/[Δ]x
where k is the thermal conductivity and [Δ]x the thickness of the layer.
The th. conductivity is given, for example, in W/(m.K) which when divided by the thickness, in m, gives W/(m
2.K), the units of the coefficient of heat transfer.
Following Fourier's law, the heat flow, expressed in W, through the layer of thickness [Δ]x would be:
Q = k*A*[Δ]T/[Δ]x
where A is the unit surface; [Δ]T, is the temperature gradient T
2-T
1.
This is for the case when the thermal conductivity is considered constant. If the thermal conductivity varies linearly with temperature as, for example, k = k
o(1+[β]T), the equation for heat flow becomes:
Q = (ko*A[÷][Δ]x)[(T2-T1) + ([β]/2)(T22-T12)]