各种金属离子在独居石表面的作用机理研究

IF 16.4 1区 化学 Q1 CHEMISTRY, MULTIDISCIPLINARY
Rongxiang Liu, Zhanfeng Yang, Jie Li, Zhao Cao, Qiang Li, Jichuan Li
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引用次数: 0

摘要

通过研究磨矿过程中释放的各种金属离子,并利用zeta电位测量法和傅立叶变换红外光谱分析法对独居石和共生矿进行浮选试验,得出金属离子对独居石表面的影响及作用机理。结果表明,独居石浮选环境中的主要金属离子为 Ca2+、Ba2+ 和 Fe3+。当矿浆pH值为8时,Ca2+、Fe3+和Ba2+浓度分别为3×10-4 mol/dm3、3×10-5 mol/dm3和2×10-4 mol/dm3,OHA捕收剂用量为5×10-4 mol/dm3,而独居石、方解石和萤石的浮选回收率均在95%以上。在 Ca2+ 和 Fe3+ 存在下,重晶石和韧皮石的回收率分别低于 54.32 % 和 38.68 %,并获得了独居石和共生矿的有效分离。zeta电位测量结果表明,当只向独居石中添加金属离子时,独居石(IEP)向右移动,独居石表面的负电荷减少,这可能是由于独居石表面吸附了金属离子的正电荷,增加了独居石表面的正电荷。当在独居石矿浆中加入 Ca2+、Ba2+、Fe3+ 和 OHA 时,独居石的 IEP 向左移动,独居石的负电荷整体向正方向移动,说明 Ca2+、Ba2+ 和 Fe3+ 被吸附在独居石表面,增加了独居石表面的正电荷。当 pH 值为 7 ~ 10 时,独居石表面与药剂作用前后相同,都带负电荷。此时,OHA 仍能吸附在方解石上,即化学亲和力克服了同电斥力而吸附,使作用后的独居石电位降低,即化学吸附。傅立叶变换红外光谱显示,当加入金属离子 Ca2+、Ba2+ 和 Fe3+ 活化独居石表面时,有机官能团-CH2-CH3 在 3000-2800 cm-1 处的峰面积增强,并在 1382 cm-1 处出现一个新峰。原因是 OHA 收集器的 N-O-H 官能团被吸附在蒙脱石表面,发生了红移(44 cm-1),并在 1454 cm-1 处出现了新的峰值。原因是 OHA 收集器的 C-N 官能团吸附在独居石表面。OHA 中酰胺基氮原子的孤电子对与 Ca2+、Ba2+ 和 Fe3+ 原子形成螯合物,从而进一步增加了 OHA 的吸附量。这表明金属离子在独居石表面的吸附为 OHA 收集器的吸附提供了活性位点。这些现象表明,OHA 在 Ca2+、Ba2+ 和 Fe3+ 活化的独居石表面的吸附能力增强,并形成稳定的五元环金属螯合物。结合浮选结果和 zeta 电位数据、红外光谱分析,Ca2+、Ba2+ 和 Fe3+ 活化独居石表面的吸附容量为Fe3+>Ca2+>Ba2+。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study on the mechanism of action of various metal ions on the surface of monazite
By studying the various metal ions released from the grinding process, and conducting the flotation test of monazite and symbiotic ore, using zeta potential measurements and FTIR infrared spectrum analysis methods, the influence of metal ions on the surface of monazite and the mechanism of action are obtained. The results showed that the main metal ions in the flotation environment of monazite are Ca2+, Ba2+, and Fe3+. When the pulp pH value was 8, Ca2+, Fe3+, and Ba2+ concentration was 3×10-4 mol/dm3, 3×10-5 mol/dm3, and was 2×10-4 mol/dm3 respectively, and OHA collector dosage was 5×10-4 mol/dm3, while the flotation recoveries of monazite, calcite. And fluorite was above 95 %, 40.43 %, and below 45.32 %, and the recovery rate of barite and bastnaesite in the presence of Ca2+ and Fe3+ is below 54.32 % and 38.68 %, respectively and the effective separation of monazite and symbiotic ore was obtained. The zeta potential measurements showed that when only metal ions are added to monazite, monazite (IEP) shifts to the right, and the negative charge on the surface of monazite decreases, which may be due to the positive charge of metal ions adsorbed on the surface of monazite, increasing the positive charge on the surface of monazite. When Ca2+, Ba2+, Fe3+, and OHA were added to the monazite pulp, the IEP of monazite moved to the left, and the negative charge of monazite shifted to the positive direction as a whole, indicating that Ca2+, Ba2+, and Fe3+ were adsorbed on the surface of monazite and increase the positive charge on the surface of monazite. When the pH value was 7 ~ 10, the surface of monazite was the same as that before and after the action of the agent, and both were negatively charged. At this time, OHA can still adsorb on the calcite, that was, the chemical affinity overcomes the same electric repulsion and adsorbs, so that the potential of the monazite after the action is reduced, which is chemical adsorption. The FTIR showed that when the metal ions Ca2+, Ba2+, and Fe3+ are added to activate the surface of monazite, the peak area of the organic functional group-CH2−CH3 at 3000-2800 cm−1 was enhanced, and a new peak appears at 1382 cm−1. The reason is that the N-O-H functional group of OHA collector was adsorbed on the surface of monazite, and a red shift (44 cm−1) occurs, and a new peak appears at 1454 cm−1. The reason is that the C-N functional group of OHA collector is adsorbed on the surface of monazite. The lone electron pair of the nitrogen atom of the amide group in the OHA forms chelates with Ca2+, Ba2+, and Fe3+ atoms, which further increases the adsorption amount of OHA. This showed that the adsorption of monazite surface by metal ions provides active sites for the adsorption of OHA collectors. These phenomena indicate that the adsorption capacity of OHA on the surface of monazite activated by Ca2+, Ba2+, and Fe3+ is enhanced and a stable five-membered ring metal chelate is formed. Combined with flotation results and zeta potential data, infrared spectroscopy analysis, the adsorption capacity of Ca2+, Ba2+, and Fe3+ activated monazite surface: Fe3+>Ca2+>Ba2+.
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来源期刊
Accounts of Chemical Research
Accounts of Chemical Research 化学-化学综合
CiteScore
31.40
自引率
1.10%
发文量
312
审稿时长
2 months
期刊介绍: Accounts of Chemical Research presents short, concise and critical articles offering easy-to-read overviews of basic research and applications in all areas of chemistry and biochemistry. These short reviews focus on research from the author’s own laboratory and are designed to teach the reader about a research project. In addition, Accounts of Chemical Research publishes commentaries that give an informed opinion on a current research problem. Special Issues online are devoted to a single topic of unusual activity and significance. Accounts of Chemical Research replaces the traditional article abstract with an article "Conspectus." These entries synopsize the research affording the reader a closer look at the content and significance of an article. Through this provision of a more detailed description of the article contents, the Conspectus enhances the article's discoverability by search engines and the exposure for the research.
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