In
addition to the common sodium salt, potassium salt, magnesium
salt, and sulfate, salt lake brine is also rich in trace components
in varying degrees, such as lithium, bromine, rubidium, cesium, and
so forth, which is of great industrial value. These trace components
are further concentrated and enriched in old brine during the process
of evaporation and concentration of brine resources. In view of the
coexistence characteristics of lithium, potassium, bromine, and other
ions in old halide, the phase equilibria of quinary system Li+, Na+, K+/Br–, and
SO4
2––H2O were studied
by the isothermal dissolution equilibrium method at 298.15 K. The
solubility data of the equilibrium liquid phase were measured, and
the compositions of the solid phase as well as the crystal forms of
the equilibrium solid phase were identified when the equilibrium was
achieved. The corresponding 3D and dry-base phase diagrams (Na2SO4·10H2O, K2SO4, LiBr·2H2O, Li2SO4·H2O, KBr, and NaBr·2H2O saturated) were drawn
based on the phase equilibrium experimental data. The research results
of phase equilibria and phase diagrams reveal that the phase relations
and crystallization–dissolution law of each component in solution
lay a certain foundation for further research on multi-temperature
phase equilibrium and thermodynamic properties of the high-component
brine system and to provide basic thermodynamic data for guiding the
rational development and comprehensive utilization of brine resources.