Abstract
Gd3+ in glasses exhibit sharp g approximately=6.0 features in the EPR spectra. It is demonstrated that these features can be adequately accounted for by using the 'rhombic' spin Hamiltonian H=gc beta H.S+D(Sz2-(S/3)(S+1))+E(Sx2-Sy2) in the strong crystal field case. Computer simulations of the experimental Gd3+ spectra in phosphate glasses result in the following estimates of mean values of D and E: mod D0 mod approximately=1 cm-1, mod E0 mod approximately=0.2 cm-1. The short-range order is rather well preserved at Gd3+ sites responsible for the g approximately=6.0 features.