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Аннотация:The magnetic resonance method is actively used to determine the ground state of
magnetic systems, which depends on the symmetry of the immediate environment.
Taking into account the crystal field and exchange bonds, the values of hyperfine
fields and the parameters of the quadrupole interaction can be determined theoretically
and compared with the values experimentally determined based on the analysis
of magnetic resonance spectra.
Magnetometry methods are integral and do not allow the unambiguous identification
and analysis of contributions from various phases under conditions of the phase
separation in a sample. The magnetic resonance method has all the advantages in
this case, since the magnetic phase separation in a sample leads to the observation
of new lines in the magnetic resonance spectrum, the interpretation of which makes
it possible to reveal the magnetic features of the emerging phases.