Origin and enrichment mechanisms of salinity and fluoride in sedimentary aquifers of datong basin, northern china

HIGHLIGHTS

  • who: Xianguo Wang and collaborators from the Sedimentary Aquifers of Datong Basin, Northern China School of Environmental Studies, China University of Geosciences, Wuhan, China have published the research work: Origin and Enrichment Mechanisms of Salinity and Fluoride in Sedimentary Aquifers of Datong Basin, Northern China, in the Journal: (JOURNAL)
  • what: The study area has a large spatial heterogeneity of groundwater chemistry.

SUMMARY

    High fluoride concentrations are naturally occurred in groundwater based on the hydrogeological and geochemical characteristics, buried depth of the aquifers, hydrochemical characteristics, underlying temperature, and the effect of weathering . . .

     

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