“…The brine of Zabuye Salt Lake in Tibet is famous for its abundance of lithium, potassium, and boron resources, which has significant exploitation value, and it is classified as a carbonate-type alkaline brine; the main composition of this salt lake brine can be attributed to Li + , Na + , K + , Mg 2+ ∥SO 4 2– , Cl – , CO 3 2– , B 4 O 7 2– – H 2 O system. To understand the thermodynamics behavior of the system mentioned above, a series of water–salt systems containing elemental borate have been studied, such as the ternary system K + ∥BO 2 – , OH – – H 2 O at 263 K, K + ∥Cl – (SO 4 2– ), B 4 O 7 2– – H 2 O at 308.15 K, Mg 2+ (K + )∥Cl – , B 4 O 7 2– – H 2 O, Na + ∥B 4 O 7 2– , SO 4 2– – H 2 O, and Li + , Na + ∥B 4 O 7 2– – H 2 O at 273.15 K, and the quaternary system Na + , K + ∥Cl – , borate – H 2 O at 308.15 K, K + ∥Cl – , SO 4 2– , B 4 O 7 2– – H 2 O at 298.15 and 308.15 K, and Li + , Na + ∥SO 4 2– , B 4 O 7 2– – H 2 O at 273.15 K . Commonly, the crystalloid form of the borate is affected by the coexisting ions.…”