Abstract
Abstract
Mössbauer spectra taken from almandite show that the orthorhombic symmetry around Fe2+ (24c position) is maintained in the magnetically ordered state. At 4.2°K the magnetic field at the nucleus is 228 ± 4 kG, and for the electrical field gradient we find (− 2.21 ± 0.06), (1.24 ± 0.04) and (0.97 ± 0.04) × 1018 V/cm2 along the three proper axes, respectively.
Subject
Inorganic Chemistry,Condensed Matter Physics,General Materials Science
Cited by
18 articles.
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