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Geochemical process of fluorine in soil
Xiaojing Liu;  Binbin Wang;  Baoshan Zheng
Source PublicationChinese Journal of Geochemistry

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.

KeywordFluorine soil Clay mineral enrichment leaching adsorption desorption
Indexed ByEI
Document Type期刊论文
Affiliation1.Guizhou Appraisal Center for Environment & Engineering, Guiyang 550002, China
2.Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China
Recommended Citation
GB/T 7714
Xiaojing Liu;Binbin Wang;Baoshan Zheng. Geochemical process of fluorine in soil[J]. Chinese Journal of Geochemistry,2014,33(3):277-279.
APA Xiaojing Liu;Binbin Wang;Baoshan Zheng.(2014).Geochemical process of fluorine in soil.Chinese Journal of Geochemistry,33(3),277-279.
MLA Xiaojing Liu;Binbin Wang;Baoshan Zheng."Geochemical process of fluorine in soil".Chinese Journal of Geochemistry 33.3(2014):277-279.
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