Abstract
Measurements of the gamma-ray resonant absorption in oriented slabs of FeF2 have been used to determine the magnitude and direction of the magnetic field at the iron nucleus in the antiferromagnetic state (3.40×105 oe at 0°K) and the quadrupole splitting in the paramagnetic state (31.2 Mc/sec) of this material. The observed electric and magnetic hfs in the antiferromagnetic state is interpretable in terms of an asymmetric electric field gradient tensor with its major axis perpendicular to the c axis, an asymmetry parameter of 0.33, and a quadrupole splitting of 30.3 Mc/sec at 45°K.