中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Interactions between variable-charge soils and acidic solutions containing fluoride: an investigation using repetitive extractions

文献类型:期刊论文

作者Zhu, MX; Jiang, X; Ji, GL
刊名JOURNAL OF COLLOID AND INTERFACE SCIENCE
出版日期2004-08-01
卷号276期号:1页码:159-166
关键词ali-haplic acrisol ferrali-haplic acrisol pH value protonation aluminum dissolution surface charge
ISSN号0021-9797
DOI10.1016/j.jcis.2004.03.033
通讯作者Zhu, MX(zhumaoxu@mail.ouc.edu.cn)
英文摘要The reaction between two variable-charge soils and acidic solutions containing F was investigated with a repetitive extraction method. When added IF concentration was 10(-4) mol/L, F did not markedly enhance solution pH in the whole prolonged extractions, in comparison with F-free acidic solution extractions. Most of the added F was adsorbed on soil surfaces and Al-F complexes were the dominant F species in solution. With increasing extractions, the fraction of AI-F slightly increased, arising from dissolution and/or desorption of Al. In comparison with F-free acidic solution extractions, F-induced At dissolution did not significantly increase At release, probably because of the modest reactivity of metal-F surface complexes at terminal sites at low F loading. The gradual decrease in Al release in the following extractions was due to the gradual depletion of readily reactive Al-containing mineral phases. In contrast to the low F loading, at an F concentration of 10(-3) mol/L, the pH was enhanced dramatically in the initial extraction and a high pH was maintained in the following extractions. In the initial extraction, the increase in negative surface charges and solution pH seemingly depressed proton-induced Al dissolution and enhanced readsorption of some positively charged AI-F complexes, resulting in low amounts of Al and F in solution. In the following several extractions, F-induced At dissolution and desorption of Al-F complexes substantially enhanced the amounts of Al and F, and the fraction of Al-F complexes in solution. Several interconnected mechanisms such as ligand exchange, the release of OH- ions from soluble hydroxylated At groups, desorption of At as AI-F complexes, and F-induced breakdown of soil minerals were responsible for the alteration in pH, At release, and the fraction of Al-F complexes in the later extractions. A molecular-level interpretation is needed in order to address the different impacts of varying F concentration levels on soil chemistry and environments. (C) 2004 Elsevier Inc. All rights reserved.
收录类别SCI
WOS关键词ORGANIC-MATTER ; ALUMINUM SPECIATION ; DISSOLUTION KINETICS ; SOLUBILITY ; MECHANISMS ; MINERALS ; SULFATE ; PH ; AL ; PRECIPITATION
WOS研究方向Chemistry
WOS类目Chemistry, Physical
语种英语
WOS记录号WOS:000222537800022
出版者ACADEMIC PRESS INC ELSEVIER SCIENCE
URI标识http://www.irgrid.ac.cn/handle/1471x/2558430
专题南京土壤研究所
通讯作者Zhu, MX
作者单位1.Ocean Univ China, Dept Chem & Chem Engn, Qingdao 266003, Peoples R China
2.Chinese Acad Sci, Inst Soil Sci, Nanjing 210008, Peoples R China
推荐引用方式
GB/T 7714
Zhu, MX,Jiang, X,Ji, GL. Interactions between variable-charge soils and acidic solutions containing fluoride: an investigation using repetitive extractions[J]. JOURNAL OF COLLOID AND INTERFACE SCIENCE,2004,276(1):159-166.
APA Zhu, MX,Jiang, X,&Ji, GL.(2004).Interactions between variable-charge soils and acidic solutions containing fluoride: an investigation using repetitive extractions.JOURNAL OF COLLOID AND INTERFACE SCIENCE,276(1),159-166.
MLA Zhu, MX,et al."Interactions between variable-charge soils and acidic solutions containing fluoride: an investigation using repetitive extractions".JOURNAL OF COLLOID AND INTERFACE SCIENCE 276.1(2004):159-166.

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来源:南京土壤研究所

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