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Mechanism of charging of the pyrite/aqueous interface as deduced from the surface potential measurements

机译:由表面电势测量推导的黄铁矿/水界面的充电机理

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Surface potential of pyrite in an aqueous environment was measured by means of a single crystal pyrite electrode. The effect of the activity of S~(2-) and Fe~(2+) ions as well as of pH, was examined. The results show that S~(2-) and Fe~(2+) ions are the dominant potential determining ions. These ions are bound to surface sites with the extent depending on their activity in the bulk of the solution. Adsorption affinity of S~(2-) ions is significantly higher than that of Fe~(2+) ions so that in most cases the pyrite surface is negatively charged. The results were explained on the basis of the surface complexation model. It was found that the surface potential depends also on pH.
机译:借助于单晶黄铁矿电极测量水环境中黄铁矿的表面电势。研究了S〜(2-)和Fe〜(2+)离子的活性以及pH的影响。结果表明,S〜(2-)和Fe〜(2+)离子是主要的势能决定离子。这些离子结合到表面部位的程度取决于它们在溶液整体中的活性。 S〜(2-)离子的吸附亲和力明显高于Fe〜(2+)离子,因此在大多数情况下,黄铁矿表面带负电。在表面络合模型的基础上解释了结果。发现表面电势还取决于pH。

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