The equilibrium between the solid solution of NaCl-KCl and the ternary
liquid NaCl-KCl-H2O is both scientifically interesting and geological
ly important. Equations of the Margules type have been derived for the
two phases that accurately reproduce the extensive array of published
measurements, together with recent measurements of Chou for the liqui
dus of the ternary and the solidus of the NaCl-KCl binary. The range o
f validity of the equations extends to 1200 K, to 5 kbar, but for the
aqueous system it is limited to compositions on the salt saturation su
rface. Of particular interest is the transition in the liquid-solid eq
uilibrium of the ternary from the pattern at high temperatures where t
he solid is a solution of composition near that of the liquid to that
at lower temperatures where the solid is nearly pure NaCl or KCl. The
phase compositions for anhydrous NaCl-KCl are consistent with the heat
of mixing data of Hersh and Kleppa and yield a new expression for the
entropy of mixing.