The slow acceptance by the scientific community of only ferromagnetic ordering below
TC in
UCu2Ge2, and the general acceptance of the same magnetic situation in
UCu2Si2, both with
the BCT ThCr2Si2-type crystallographic structure, are reviewed chronologically.
Observations by neutron diffraction on annealed polycrystalline samples of
UCu2Ge2
have finally overcome many conclusions of antiferromagnetic (AF) ordering at low
temperatures (LT), deduced from the magnetization overlooking the ferromagnetic
domain structure. Observations by magnetization measurements on Cu-flux-grown
UCu2Si2
single crystals, claiming ‘a 50 K AF transition below the 100 K ferromagnetic transition’,
published recently in this journal (2003 J. Phys.: Condens. Matter 15 S1917), are shown to
have been misinterpreted by omitting any reference to ferromagnetic domain
structure. Comments are made on other features disputing the LT ferromagnetism of
UCu2Si2.