Monitoring geochemistry of the evolution of natural system: salar de Huasco (Chile)
Evaporation process affecting brines in salar of Huasco (Chile) has been reproduced at laboratory scale with the main objective of studying its geochemical evolving path.Natural brines have been evaporated under isothermal conditions, precipitating progressively calcite, gypsum, thenardite, and halite.This mineral sequence confirms the evolution of