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The Development of Fine Microgram Powder Electrode System and Its Application in the Analysis of Chalcopyrite Leaching Behavior

机译:精细微克粉末电极系统的开发及其在黄铜矿浸出行为分析中的应用

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摘要

An electrode system to study the mechanism of fine microgram powder sulfide mineral dissolution was developed by using a relatively simple method that enables the attachment of micrograms of fine powder to a platinum plate surface. This system yields highly reproducible results and is sensitive compared with conventional electrode systems for various sulfide minerals such as pyrite, chalcopyrite, chalcocite, enargite, and tennantite. The leaching behavior of chalcopyrite was re-examined in a test of the application of this electrode system. Chalcopyrite dissolution is enhanced in specific potential regions because it is believed to be reduced to leachable chalcocite, but this result is inconclusive because it is difficult to detect the intermediate chalcocite. Powder chalcopyrite in the new powder electrode system was held at 0.45 V in the presence of copper ion and sulfuric acid media followed by an application of potential in the anodic direction. Besides the chalcopyrite oxidation peak, a small peak resulted at ?¢????0.55 V; this peak corresponds to reduced chalcocite, because it occurs at the same potential as the chalcocite oxidation peak.
机译:通过使用一种相对简单的方法开发了一种电极系统,用于研究微克级粉末状硫化物矿物溶解的机理,该方法可以将微克级的粉末状粉末附着到铂板表面。与传统的电极系统相比,该系统可产生高度可重复的结果,并且对各种硫化物矿物(如黄铁矿,黄铜矿,黄铜矿,辉绿岩和球铁矿)敏感。在对该电极系统的应用测试中,再次检查了黄铜矿的浸出行为。黄铜矿的溶解在特定的潜在区域得到增强,因为据信它会还原为可浸出的菱锰矿,但由于难以检测到中间的菱锰矿,该结果尚不确定。在存在铜离子和硫酸介质的情况下,新粉末电极系统中的粉末黄铜矿保持在0.45 V,然后在阳极方向施加电势。除黄铜矿的氧化峰外,在0.55V时产生一个小峰。该峰对应于还原的方球石,因为它出现在与方球石氧化峰相同的电位上。

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