The phase coexistence behavior of the solvent primitive model (SPM) is stud
ied by constant pressure and temperature Gibbs ensemble Monte Carlo simulat
ions. In the SPM, the ions are modeled with charged hard spheres, while the
solvent molecules are represented by neutral hard spheres. Fluid-fluid pha
se separation into a salt poor and salt rich phase is found. At constant pr
essure, the critical temperature increases with respect to the critical tem
perature of the primitive model (PM) where no hard spheres are present. At
constant temperature and for low pressures, the phase separation of the SPM
transforms into the phase separation of the PM. For high pressures, it rem
ains an open question whether there is an upper critical immiscibility pres
sure or whether a solid-fluid phase transition occurs first. (C) 2000 Ameri
can Institute of Physics. [S0021-9606(00)52541-0].