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Competition between commensurate and incommensurate phases in rare-earth systems: Effects on H-T magnetic phase diagrams.

Some features common to many rare-earth intermetallic compounds with complex magnetic phase diagrams are explained using a realistic mean-field model, which takes into account the periodic-exchange-field and crystal-field effects which favor an easy magnetization axis, i.e.: (i) the change of an incommensurate or long-period commensurate structure near T N toward a simple commensurate one at loss temperature, with and without intermediate structures of intermediate propagation vectors; (ii) the loss-temperature metamagnetic process during which the high-temperature propagation vector(s) tend to be recovered; (iii) the trend for the propagation vectors to lock onto commensurate values, except near T N