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Yubin Sun, Qian Zhang, Shuming Wen, Yongchao Miao, and Ping Zhang, Mechanistic insights into the synergistic depression of pyrite by H2O2 and Fe3+ in low-alkalinity Cu–S flotation separation, Int. J. Miner. Metall. Mater., (2026). https://doi.org/10.1007/s12613-025-3334-0
Yubin Sun, Qian Zhang, Shuming Wen, Yongchao Miao, and Ping Zhang, Mechanistic insights into the synergistic depression of pyrite by H2O2 and Fe3+ in low-alkalinity Cu–S flotation separation, Int. J. Miner. Metall. Mater., (2026). https://doi.org/10.1007/s12613-025-3334-0
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低碱度铜硫浮选分离中H2O2与Fe3+协同抑制黄铁矿的机理研究

摘要: 硫化铜矿浮选分离中传统使用的石灰抑制剂长期受结垢、腐蚀以及目标金属回收率下降等问题的限制,因此亟需开发高效、绿色的替代抑制剂。本研究证实了低碱度条件下H2O2/Fe3+体系对黄铁矿具有协同抑制作用,并通过单矿物与混合矿物浮选试验、表面分析及溶液分析等多尺度表征技术,系统阐明了该体系的互补作用机制。浮选试验结果表明,H2O2/Fe3+复合抑制剂体系可实现黄铜矿与黄铁矿的高效分离。在0.025vol% H2O2和2 × 10–5 mol/L Fe3+的最佳混合矿物分离条件下,人工混合矿物浮选试验获得的铜精矿中黄铜矿品位达到30.51wt%,同时黄铜矿回收率稳定保持在88%以上。抑制机理与表面疏水性研究表明,H2O2可选择性地将二硫化物( \mathrmS_2^2- )氧化为硫酸盐( \textSO_4^2- ),同时促进Fe2+转化为Fe3+,生成亲水性的Fe–SO4/Fe–OOH/Fe–OH覆盖层,破坏了黄铁矿的天然表面疏水性。同时,Fe3+水解生成羟基络合物(Fe(OH)2+和Fe(OH)3),这些络合物通过静电吸附和化学键合作用附着在经H2O2氧化的黄铁矿表面,形成致密的亲水性层。黄铁矿氧化速率更快源于其自身的基本结构特性,具体表现为较高的表面电子活性和相对较弱的Fe–S键,这使得黄铁矿更易受到H2O2的氧化攻击;而黄铜矿具有稳定的晶格和强共价性的Cu–S键,因此氧化抗性更强。因此,黄铜矿中牢固的共价Cu–S键可有效抵抗氧化,同时其对Fe3+的吸附能力有限,有利于乙基黄原酸钠(SEX)在铜活性位点上的吸附。综上,H2O2/Fe3+体系对黄铜矿仅产生微弱的抑制作用,为硫化铜矿石的选择性分离提供了坚实的理论基础和实用的技术策略。此外,本研究结果有助于开发低碱度、高选择性的硫化矿处理工艺,展现出巨大的工业应用潜力。

 

Mechanistic insights into the synergistic depression of pyrite by H2O2 and Fe3+ in low-alkalinity Cu–S flotation separation

Abstract: Conventional lime depressants used in copper sulfide flotation separation are limited by persistent challenges of scaling, corrosion, and compromised target-metal recovery, which necessitates the development of efficient and green alternatives. This study demonstrates the synergistic depression of pyrite by H2O2/Fe3+ under low-alkalinity conditions. The complementary action pathways were systematically elucidated by multiscale characterization techniques including mono- and mixed-mineral flotation tests and surface and solution analysis. Flotation test results showed that the combined depressant system H2O2/Fe3+ enabled efficient separation of chalcopyrite and pyrite. Under the optimal mixed-mineral separation conditions of 0.025vol% H2O2 and 2 × 10−5 mol/L Fe3+, the artificial mixed-mineral flotation test yielded a copper concentrate with a chalcopyrite grade of 30.51wt%, while chalcopyrite recovery remained stably above 88%. Investigations into the depression mechanism and surface hydrophobicity revealed that H2O2 selectively oxidized disulfide ( \mathrmS_2^2- ) to sulfate ( \textSO_4^2- ) while facilitating Fe2+ conversion to Fe3+, generating hydrophilic Fe–SO4/Fe–OOH/Fe–OH coatings that disrupted natural surface natural hydrophobicity. Simultaneously, Fe3+ hydrolyzed to hydroxyl complexes (Fe(OH)2+ and Fe(OH)3), which electrostatically adsorbed onto and chemically bonded to H2O2-oxidized pyrite surfaces, forming dense hydrophilic layers. The faster oxidation of pyrite resulted from its fundamental structural properties, specifically its high surface electronic activity and relatively weak Fe–S bonds, which collectively rendered it more susceptible to H2O2 attack, unlike chalcopyrite with its stable lattice and strong covalent Cu–S bonds. Consequently, the robust covalent Cu–S bonds of chalcopyrite effectively resisted oxidation, while its limited Fe3+ adsorption capacity favored the adsorption of sodium ethyl xanthate (SEX) at copper-active sites. As a result, the H2O2/Fe3+ system exerted only minimal depression on chalcopyrite, providing a sound theoretical basis and a practical technical strategy for the selective separation of copper-sulfide ores. Furthermore, the findings of this study contribute to the development of low-alkalinity, high-selectivity sulfide-ore processing methods, demonstrating considerable potential for industrial application.

 

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