Among cerium pnictides, the compound CeSb exhibits the most complex behavior. The magnetic structures of the numerous observed phases have been determined. The magnetic field has been applied along a fourfold axis of the rock salt structure. For all the phases the order consists of square-wave structures characterized by a propagation vector →k=(0, 0, k) of value commensurate with the crystallographic cell and by a strong anisotropy confining the moments along the k vector. All the structures can be generated by a periodic stacking of zero magnetized planes P and ferromagnetic planes with a magnetization parallel M↑ or antiparallel M_↓ to the applied field. Three types of structures can be distinguished: (a) at low temperature only M↑ and M_↓ planes exist, the structures k=4/7 (++--++-), k=2/3 (++-), and $k=0$ are successively observed when the field is increased. (b) at high temperature and low field M↑, M_↓, and P planes coexist leading to an "antiferroparamagnetic order." (c) at high temperature and high field only M↑ and P planes exists defining a ferroparamagnetic order. The phase diagram feature can be understood by a simple thermodynamic analysis considering an entropy S₀=kln2 for paramagnetic planes and a moment of 2.1 μB/Ce atom for magnetized planes.
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Rossat‐Mignod et al. (1977) studied this question.
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