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Sulfide-iron interactions in domestic wastewater from a gravity sewer

机译:重力下水道中生活污水中的硫化铁相互作用

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Interactions between iron and sulfide in domestic wastewater from a gravity sewer were investigated with particular emphasis on redox cycling of iron and iron sulfide formation. The concentration ranges of iron and total sulfide in the experiments were 0.4-5.4 mg Fe L~(-1) and 0-5.1 mg S L~(-1), respectively. During anaerobic conditions, iron reduction kinetics were investigated and reduction rates amounted on average to 1.32 mg Fe L~(-1) d~(-1). Despite the very low solubility of iron sulfide, the reduced iron reacted only partly with sulfide to produce iron sulfide, even when dissolved sulfide was in excess. When a ferric chloride solution was added to sulfide containing anaerobic wastewater, the ferric iron was quickly reduced to ferrous forms by oxidation of dissolved sulflde and the ferrous iron precipitated almost completely as iron sulfide. During aerobic conditions, iron sulfide was oxidized with a half-life period of 11.7h. The oxidation rate of iron sulfide was significantly lower than that reported for the oxidation of dissolved sulfide.
机译:研究了重力下水道中生活污水中铁和硫化物之间的相互作用,特别着重于铁和硫化铁形成的氧化还原循环。实验中铁和总硫化物的浓度范围分别为0.4-5.4 mg Fe L〜(-1)和0-5.1 mg S L〜(-1)。在厌氧条件下,研究了铁还原动力学,还原速率平均为1.32 mg Fe L〜(-1)d〜(-1)。尽管硫化铁的溶解度非常低,但是即使溶解的硫化物过多,还原铁也只能与硫化物部分反应生成硫化铁。当将氯化铁溶液添加到含硫化物的厌氧废水中时,三氧化二铁通过溶解的硫化物的氧化迅速还原为亚铁形式,并且亚铁几乎完全作为硫化铁沉淀。在有氧条件下,硫化铁被氧化,半衰期为11.7h。硫化铁的氧化速率明显低于溶解的硫化物的氧化速率。

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