Geochemical process of fluorine in soil | |
Xiaojing Liu; Binbin Wang; Baoshan Zheng | |
2014 | |
Source Publication | Chinese Journal of Geochemistry |
Volume | 33Issue:3Pages:277-279 |
Abstract | 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. |
Keyword | Fluorine soil Clay mineral enrichment leaching adsorption desorption |
Indexed By | EI |
Language | 英语 |
Document Type | 期刊论文 |
Identifier | http://ir.gyig.ac.cn/handle/42920512-1/9285 |
Collection | 环境地球化学国家重点实验室 |
Affiliation | 1.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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Geochemical process (211KB) | 期刊论文 | 作者接受稿 | 开放获取 | CC BY-NC-SA | View Application Full Text |
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