Isopiestic measurements have been carried out for the quaternary systems H2O−Y(NO3)3−La(NO3)3−Pr(NO3)3, H2O−Y(NO3)3−La(NO3)3−Nd(NO3)3 and H2O−Y(NO3)3−Pr(NO3)3−Nd(NO3)3 at 298.15 K to near saturation. The measurements can be represented by a modified Pitzer ion–interaction model extending to C(3) within the experimental uncertainty over the full concentration range. In addition, these systems obey the Zdanovskii-Stokes-Robinson model or partial ideal solution model within isopiestic accuracy, indicating zero solute-solute interchange energy, which is consistent with the nature of salts of the trivalent rare earth ions.