作为地球化学屏障基底的机械化学修饰腐植酸和铁(III)复合物

IF 0.6 4区 化学 Q4 CHEMISTRY, APPLIED Russian Journal of Applied Chemistry Pub Date : 2024-06-10 DOI:10.1134/S107042722310004X
E. V. Linkevich, N. V. Yudina
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引用次数: 0

摘要

摘要 在pH值为12至2的条件下,通过共沉淀法制备了机械化学修饰腐植酸与Fe(ІІІ)的复合物。腐殖酸的离子酚基和羧基在 Н 8-12 时与 Fe3+ 结合。在 Н < 7.5 时,腐植酸芳香族片段的羧基与带正电荷的铁元素{[Fe(OH)2]aq}+ 和 {[Fe(OH)]aq}2+ 进行离子交换。改性腐植酸的吸附交换能力最多可保持 50%,这取决于复合物中腐植酸成分的比例。有机矿物质复合物的活性位点是改性腐植酸大分子中带负电荷的含氧官能团和带正电荷的胶束状 Fe(ІІІ)。含铁(Ⅲ)的腐殖质复合物可用作地球化学屏障的基底,以降低土壤中污染化学元素和有机生态毒物的浓度。
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A Complex Compound of Mechanochemically Modified Humic Acids and Fe(III) as a Base of a Geochemical Barrier

A complex of mechanochemically modified humic acids with Fe(ІІІ) was prepared by coprecipitation at pH varied from 12 to 2. Fe(ІІІ) interacts with humic acids via ionized groups. The ionized phenolic and carboxyl groups of humic acids at рН 8–12 bind Fe3+. At рН < 7.5, carboxyl groups of aromatic fragments of humic acids enter into the ion exchange with positively charged iron species {[Fe(OH)2]aq}+ and {[Fe(OH)]aq}2+. The sorption exchange capacity of the modified humic acids is preserved to up to 50% and depends on the fraction of the humic component in the complex. The active sites of the organomineral complex are negatively charged oxygen-containing functional groups of macromolecules of the modified humic components and positively charged micellar Fe(ІІІ) forms. The humic complex with Fe(III) can be used as a base of a geochemical barrier to reduce the concentration of polluting chemical elements and organic ecotoxicants in soil.

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来源期刊
CiteScore
1.60
自引率
11.10%
发文量
63
审稿时长
2-4 weeks
期刊介绍: Russian Journal of Applied Chemistry (Zhurnal prikladnoi khimii) was founded in 1928. It covers all application problems of modern chemistry, including the structure of inorganic and organic compounds, kinetics and mechanisms of chemical reactions, problems of chemical processes and apparatus, borderline problems of chemistry, and applied research.
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