Lithium during Brine Evaporation and KCl Production Plants

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Lithium during Brine Evaporation and KCl Production Plants ( lithium-during-brine-evaporation-and-kcl-production-plants )

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Figure 2 shows lithium distribution during brine evaporation process in both the simulation experiment and field sampling from different salt ponds. As brine concentrating lithium in aqueous phase was enrichened, the average concentration of lithium could reach a level of 500 mg/L. In residual brine, this was more than double the concentration in the original brine. The simulation experiments showed that the vast majority of lithium was retained in the aqueous phase and there Minerals 2017, 7, 57 5 of 12 was a positive correlation between lithium concentrations with brine enrichment degree. Figure 2. Lithium distribution during the brine evaporation process. Figure 2. Lithium distribution during the brine evaporation process. Table 2. Identification results of solid phase during the brine evaporation process. Lithium content in solid phase had no evident change (p > 0.05) during the brine concentration process until bischofite was precipitated. Although brine was more concentrated by natural Density (g/cm3) Halite (%) 95 94 44 24 24 70 2 0 0 0 0 1 0 Bischofite (%) 5 6 7 5 8 0 85 100 100 100 100 99 100 Carnallite (%) 0 0 49 71 68 30 13 0 0 0 0 0 0 1.2602 1.2768 1.2944 1.3218 1.3373 1.3559 1.3579 1.3634 1.3648 1.3654 1.3668 1.3891 1.3692 The relationship of magnesium-lithium ratio between brine densities during the evaporation process is given in Figure 3. It shows that the Magnesium-lithium ratio does not changed much in early evaporation stage (depicted in magenta and violet colors), but a larger change appears when the brine density value is more than 1.285 g/cm3 (depicted in blue and green colors). The magnesium-lithium ratio decreases sharply in the later stage of evaporation, especially when brine density is more than 1.345 g/cm3. Brine magnesium-lithium ratio decreases almost to half of initial value when the brine density is around 1.372 g/cm3 (depicted in red). The brine density value could represent the degree of brine concentration because brine density is proportional to the degree of evaporation. The greater the density value, the higher the degree of brine evaporation and lithium enrichment. As shown in Figure 3, the magnesium-lithium ratio remains at about the same level in the early evaporation stage, but a slight decrease appears when the brine density value is more than 1.28 g/cm3, almost the moment when carnallite crystalized. Thus, it can be deduced that the brine magnesium-lithium ratio decrease was caused by carnallite precipitation. This is because carnallite is a double salt that contains 8.64% magnesium and the precipitation led the magnesium ions to migrate to solid from aqueous. The magnesium-lithium ratio decreased sharply in the later stage of evaporation, especially when brine density was more than 1.34. The brine magnesium-lithium ratio value almost decreased half of its original value when the brine density reached 1.37 g/L. However,

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Salt water or brine are huge sources for lithium. Most of the worlds lithium is acquired from a brine source. It's even in seawater in a low concentration. Brine is also a byproduct of huge powerplants, which can now use that as an electrolyte and a huge flow battery (which allows storage at the source).

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