Brines, containing a variety of useful components, such as alkali metal (IA), alkaline earth metal (type IIA), halogen elements (such as VIIA), are naturally occurring complex electrolyte solution. Although rubidium is not the main component of the brine, while in the brine exploiting process, rubidium ion is continuously enriched in the mother liquid to form an aqueous system containing lithium, potassium, rubidium, magnesium, and chloride. In chloride solution, rubidium and potassium are easily formed into solid solution because of their similar ion radius: potassium, 1.33·10 -10 m, and rubidium, 1.49·10 -10 m. Besides that, the hydrated salts of MgCl 2 and double salts can be easily formed, which increase the difficulty to the comprehensive utilization of the brine.The phase equilibria and phase diagram of aqueous systems of alkali halides are required not only in process design in the chemical industry, but they are of interest to a wider variety of geochemistry and salt chemistry. Up to now, some paper described phase equilibria aiming at rubidium and potassium coexist system have been reported. Kalinkin et al. have studied ternary system K 2 SO 4 + Rb 2 SO 4 + H 2 O at 298 K (Kalinkin and Rumyantsev, 1996), the system is of complex type with the continuous solid solutions between K 2 SO 4 and Rb 2 SO 4 . Merbach et al. have studied the quaternary system KCl + RbCl + H 2 O at 298 K (Merbach and Gonella, 1969), results shown that there was only solid solution [(K, Rb)Cl] formed. The quaternary system KCl + RbCl + (CsCl) + MgCl 2 + H 2 O and its subsystems at 298 K have been done by J. D'Ans et al. (D'Ans and Brsch, 1937), results shown that there were single salts KCl, RbCl and solid solution [(K, Rb)Cl] formed in the Fig. 1. Metastable phase diagram of ternary system KCl + RbCl + H 2 O at (298, 323 and 348) K.