Journal
ACTA GEOCHIMICA
Volume 33, Issue 3, Pages 277-279Publisher
SPRINGER INTERNATIONAL PUBLISHING AG
DOI: 10.1007/s11631-014-0688-9
Keywords
fluorine; soil; clay mineral; enrichment; leaching; adsorption; desorption
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Funding
- Key Project of International Cooperation of the Ministry of Science and Technology of China [2010DFB30530]
- Social Development Project of Guizhou Province, China [SZ[2009]3045]
- Science and Technology Foundation of Guizhou Province, China [J[2008]2312]
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Fluorine is in the dynamic balance of two geochemical processes, enrichment and leaching, reflecting the adsorption and desorption of fluoride by clay minerals, respectively. The two geochemical processes of fluorine in soil are influenced by factors including geochemical characteristics of soil and clay minerals, pH and sanity of soil solutions, climate, grazing and agriculture activities. Main factors controlling enrichment and leaching process of fluorine in soil can be found with interaction consideration.
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