Abstract
The schematic model is extended to open-shell nuclei. The quasiparticle random-phase approximation plus core polarization are used to calculate multipole matrix elements Mn and Mp. Calculated trends in the ratio of deformation parameters βnβp are compared with experimental ratios for several sets of isotopes and isotones. The systematics indicate a rather abrupt change toward equality of βn and βp when N or Z is changed from a closed-shell value.