Abstract
Most of the rare earths are ferro- or antiferromagnetic at low temperatures. Due to this, their heat capacity has usually four different components: the lattice specific heat C L , the electronic specific heat C E , the magnetic specific heat C M , and the nuclear specific heat C N . A fairly large amount of work has recently been done for establishing the heat capacity of lanthanides in the liquid-helium region and, in particular, below 1°K. As a result, the nuclear specific heat, which is large below 1°K, is well understood.
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