首页> 外文期刊>Langmuir: The ACS Journal of Surfaces and Colloids >Mechanism of Goethite Precipitation on Magnetite and Maghemite Nanoparticles Studied by Surface Complexation/Precipitation Modeling
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Mechanism of Goethite Precipitation on Magnetite and Maghemite Nanoparticles Studied by Surface Complexation/Precipitation Modeling

机译:表面络合/降水建模研究磁铁矿和磁石纳米粒子对磁铁矿和磁石纳米粒子的机制

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摘要

Precipitation of goethite on magnetic nanoparticles (MNPs) has been proposed as an effective means to separate goethite from calcium sulfate in the iron removal process of zinc hydrometallurgy, which allows reuse of the hazardous residues. This study focuses on investigating the underlying mechanisms of goethite precipitation on magnetite and maghemite MNPs, providing insights on Fe(III)(aq) adsorption and nucleation of goethite on MNPs. A predictive surface complexation/precipitation model of the system was developed based on the results from two different types of experiments: the potentiometric titration of MNPs to calculate proton binding constants (K-a) of discrete MNP surface functional groups and the corresponding site concentrations; and adsorption of Fe(III)(aq) onto MNP surfaces to determine metal binding constants (K-f). The composition of the surface complexes on MNPs was by time-of-flight secondary ion mass spectrometry. The results indicated the formation of polynuclear surface complexes. content of polynuclear surface complexes was found to be significantly higher on maghemite MNPs than on magnetite MNPs. This trend is consistent with our experimental results of a greater goethite precipitation on maghemite than on magnetite. Overall, the formation of Fe(III) polynuclear surface complexes correlates directly to the nucleation and precipitation of goethite on the surfaces of both types of MNPs.
机译:已经提出了在磁性纳米粒子(MNP)上的甲磺酸盐的沉淀作为一种有效的方法,以将来自硫酸钙的硫酸钙分离锌氢硫化的硫酸钙,这允许重复使用危险残留物。本研究致力于研究磁铁矿和磁性磁石MNP上的可粘散沉淀的潜在机制,提供对Fe(III)(AQ)吸附和甲磺酸盐的核心在MNP上的洞察力。系统的预测表面络合/降水模型是基于来自两种不同类型的实验的结果:MnP的电位滴定计算离散MNP表面官能团的质子结合常数(K-A)和相应的位点浓度;并吸附Fe(III)(AQ)在MNP表面上以确定金属结合常数(K-F)。通过飞行时间二次离子质谱法的表面复合物的组成。结果表明了多核表面配合物的形成。在磁沸石MNP上发现多核表面复合物的含量显着高于磁铁矿MNP。这种趋势与我们的实验结果一致,在磁性岩石上的更大的诙谐沉淀而不是磁铁矿。总的来说,Fe(III)多环表面复合物的形成直接与两种类型的MNP的表面上的核心成核和沉淀。

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    Cent S Univ Sch Minerals Proc &

    Bioengn Room 310 Shengwu Bldg 984 Lushannan Rd Changsha 410083 Hunan Peoples R China;

    Cent S Univ Sch Minerals Proc &

    Bioengn Room 310 Shengwu Bldg 984 Lushannan Rd Changsha 410083 Hunan Peoples R China;

    Cent S Univ Sch Minerals Proc &

    Bioengn Room 310 Shengwu Bldg 984 Lushannan Rd Changsha 410083 Hunan Peoples R China;

    Univ Alberta Dept Chem &

    Mat Engn Donadeo Innovat Ctr Engn 12-354 Donadeo Innovation Ctr Engn 9211-116 St Edmonton AB T6G 1H9 Canada;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 物理化学(理论化学)、化学物理学;化学;
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