Abstract
The electric-field g shift of Yb3+ in the scheelite series CaWO4, SrWO4, and BaWO4 has been measured. In SrWO4, and especially in BaWO4, the Yb ion is much smaller than the cation, and we find a substantial increase in the g shifts, which indicates less restraint to ionic motion. The lattice restoring forces for loose ions are investigated through the use of the Born-Mayer theory of ionic bonding. We find that the predicted ionic g shift is considerably larger than that observed. This may be due to substantial local distortion near a Yb impurity. Several other mechanisms for increasing the restoring forces on small ions are also considered.