Fluoride Action Network

Geochemical controls on the enrichment of fluoride in the mine water of the Shendong mining area, China

Source: Chemosphere 284:131388. | June 30th, 2021 | Authors: Zhang Z, Li G, Su X, Zhuang X, Wang L, Fu H, Li L.
Location: China


  • 51% of mine water samples exceed the Chinese drinking water limit for fluoride (1 mg/L).
  • The overall mine water quality is influenced by cation exchange, dissolution of minerals and so on.
  • NaHCO3 type mine water possesses the highest average fluoride concentration.
  • Fluoride concentrations are overall proportional to higher pH, TDS, and EC levels.
  • Fluoride enrichment is related to ion exchange, mineral precipitation, and evaporation.


Underground coal mining produces large amounts of mine water annually in the Shendong mining area of China. Due to the severe scarcity of water resources, mine water is extensively used for productive, domestic, and ecological demands. However, mine water exhibits high fluoride levels. For water-use security, reduction of fluoride exposure and environmental protection, knowledge of sources and geochemical controls of fluoride enrichment in mine water is required. The results showed that F? concentrations of mine waters vary from 0.05 to 11.65 mg/L, with a mean value of 1.96 mg/L, and 51% of the mine waters contain F? concentrations exceeding the Chinese drinking water standard (1 mg/L). The overall mine water quality is influenced by cation exchange, mineral dissolution, pyrite oxidation, silicate weathering and so on. The high-fluoride mine waters are all associated with Na–type, with a remarkable cation composition feature of higher Na+ and lower Ca2+ and Mg2+ concentrations. Overall, the high-fluoride mine waters are well-matched with the water environment with higher pH, TDS, and EC levels. PCA reveals that the geochemical controls on the enrichment of F? in mine waters include dissolution of fluoride-bearing minerals and F?-OH? ion exchange; the former process is mainly caused by the decrease in Ca2+ concentrations resulting from Na + -Ca2+ cation exchange and mineral precipitation, and the latter process benefits from a highly alkaline water environment, facilitating the substitution of OH? in the mine water for F? within or absorbed on the minerals. Evaporation also controls F? enrichment in local areas.