Abstract
It is shown that the heat flow in a single homogeneous medium of thermal conductivity σ(T), between boundaries at temperatures T2 and T1 is the same as that for the same geometry in a medium of unit thermal conductivity and boundary ``thermal potentials'' Σ(T2) and Σ(T1), where Σ(T)=∫0Tσ(T′)dT′ . Some applications are given, as well as a short table of Σ(T) for common cryogenic temperatures and materials.