Formation processes and evolution model of high-fluoride groundwater in a granitic basin under complex geological conditions

Key Points

• High-fluoride groundwater concentrations are influenced by complex geological conditions, and this relationship needs to be understood for better water management.
• Groundwater evolution models reveal significant insights into the formation processes of fluoride in granitic basins over time.
• Analysis of geological data highlights the specific conditions leading to high fluoride levels, with implications for environmental health.
• Further studies are needed to explore the broader effects of these geological factors on groundwater systems worldwide.