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Geochemical process of fluorine in soil
Xiaojing Liu;  Binbin Wang;  Baoshan Zheng
2014
发表期刊Chinese Journal of Geochemistry
卷号33期号:3页码:277-279
摘要

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.

关键词Fluorine soil Clay mineral enrichment leaching adsorption desorption
收录类别EI
语种英语
文献类型期刊论文
条目标识符http://ir.gyig.ac.cn/handle/42920512-1/9285
专题环境地球化学国家重点实验室
作者单位1.Guizhou Appraisal Center for Environment & Engineering, Guiyang 550002, China
2.Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China
推荐引用方式
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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