With demand for lithium predicted to continue increasing in the coming years, lithium exploration and the development of recovery techniques to extract it will become increasingly important. Lithium is particularly important for the energy transition due to its use in lithium-ion batteries. A major source of lithium are Lithium-Caesium-Tantalum (LCT) pegmatites. Lithium is contained within spodumene crystals and these are therefore the focus of most extraction techniques. The main objective of this study was to create an overview of the lithium distribution in lithium pegmatites based on textural and mineralogical information, combined with elemental analysis using Laser Induced Breakdown Spectroscopy (LIBS). The purpose was to improve the understanding of spodumene characteristics in lithium pegmatites which could affect lithium exploration and recovery.
Six samples from two different lithium pegmatite fields were analysed. Four samples were from the Bergby pegmatite field in Sweden and two samples were from the Bougouni pegmatite field in Mali. Petrographic descriptions were made to understand the mineralogy and textures of spodumene and LIBS analysis was used to measure lithium concentrations across profiles on a micrometre scale. Notable features in the Bergby (Sweden) samples included recrystallised, fine grained spodumene in uneven rims around the primary spodumene crystals as well as in the finer grained groundmass. The average lithium content measured for spodumene from the block samples was between 1.4 to 2.1 wt % Li, which is lower than the commonly measured range for spodumene of 2.8 to 3.5 wt % Li (Aylmore et al., 2018). LIBS analysis on the thin sections was attempted and showed higher average lithium content in the micrometre-scale fractures in the spodumene than in the surrounding spodumene crystal. The results of this thesis show that the majority of the lithium remains contained within primary spodumene crystals in lithium pegmatites but lower concentrations are also present in certain locations in the surrounding rock. Additionally, it indicates that the Keyence EA-300 may not be suitable for Li detection in spodumene crystals due to the significant differences in lithium concentration between thin section and block sample measurements. In future it would be critical to consider factors such as matrix effects, sample preparation and calibration of the Keyence EA-300 for true quantitative analysis of lithium content in spodumene.