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首页> 外文期刊>International Journal of Electrochemical Science >An Electrochemical Study of Surface Oxidation and Collectorless Flotation of Pyrite
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An Electrochemical Study of Surface Oxidation and Collectorless Flotation of Pyrite

机译:硫铁矿表面氧化和无集电极浮选的电化学研究

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Pyrite is a common sulfide mineral and its surface oxidation and natural hydrophobicity play animportant role in determining flotation performance for many minerals, particularly for sulfides andcoal. In this study freshly fractured electrodes have been used to investigate the surface oxidation offresh pyrite surface and collectorless microflotation tests were performed to study its naturalhydrophobicity. Chronoamperometry performed on in-situ fractured electrodes demonstrated thatpyrite oxidation takes place at potentials of -0.28 V (SHE) at pH 9.2 and 0 V at pH 4.6, considerablylower than previously assumed. Incipient oxidation at slightly more positive potentials produce ahydrophobic sulfur-rich species, most likely a polysulfide or metal-deficient sulfide, which impartsnatural surface hydrophobicity to pyrite. Collectorless microflotation test results have indicated thatpyrite acquires considerable floatability upon superficial oxidation. The collectorless flotationrecovery of pyrite is determined by the relative amounts of polysulfide, soluble species, and insolublespecies produced during oxidation, which depends on solution pH and potential.
机译:黄铁矿是一种常见的硫化矿物,其表面氧化和天然疏水性在决定许多矿物(尤其是硫化物和煤)的浮选性能中起着重要作用。在这项研究中,新近破碎的电极已用于研究表面氧化脱硫黄铁矿表面,并进行了无捕集器微浮选试验以研究其天然疏水性。在原位断裂电极上进行的计时安培分析表明,黄铁矿氧化在pH 9.2时为-0.28 V(SHE)且在pH 4.6时为0 V,比以前假定的要低得多。在稍高的正电势下开始氧化会产生疏水性富硫物质,最有可能是多硫化物或金属缺乏的硫化物,从而使黄铁矿具有天然的表面疏水性。无收集器微浮选试验结果表明,黄铁矿在表面氧化后具有相当大的漂浮性。黄铁矿的无捕收剂浮选回收率取决于氧化过程中产生的多硫化物,可溶物质和不溶物质的相对量,这取决于溶液的pH和电势。

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