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Mechanisms of bio-dephosphorization from phosphorous iron ore

机译:磷铁矿生物脱磷的机理

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Mechanisms of bio-dephosphorization from iron ore was investigated in this Paper. The results show that there are two bio-dephosphorization ways from iron ore, the one is that Acidithiobacillus ferrooxidans directly derive phosphorus from the ore, the other is phosphorus is able to be leached acid produced during metabolizing of Acidithiobacillus ferrooxidans, and the latter is more important than the other. Adding suitable pyrite can enhance the bio-dephosphorization process through providing nourishment and producing acid directly due to S oxidized or indirectly due to Fe~(3+) as oxidant. The potential varies in the range of 0.434~0.498V and pH is in the range of 2.5~1.25 during bio-leaching process. It can be founded that, according to the E-pH graph of Fe-H_2O system, Fe~(2+) wouldn't be oxidized under sterile system in this potential and pH ranges. It can be obviously concluded that the Acidithiobacillus ferrooxidans are able to reduce the potential for the oxidization of Fe~(2+) and make the oxidization occur in the above pH and potential zone, so the bio-leaching process can proceed, the investigation of E-pH graph of P-H_2O system show that H_3PO_4 can exist steadily.
机译:本文研究了铁矿石生物脱磷的机理。结果表明,铁矿石有两种生物脱磷的方式,一种是酸性铁硫氧化亚铁直接从矿石中提取磷,另一种是磷能够被酸性铁硫氧化亚铁代谢过程中产生的酸浸出,而后者更多。比其他重要。添加合适的黄铁矿可通过提供营养和直接由于S氧化而产生酸或间接由于Fe〜(3+)作为氧化剂而产生酸来增强生物脱磷过程。生物浸出过程中电势在0.434〜0.498V范围内变化,pH在2.5〜1.25范围内变化。可以发现,根据Fe-H_2O体系的E-pH图,在该电位和pH范围内,Fe〜(2+)在无菌体系下不会被氧化。可以很明显地得出结论,酸性硫杆菌铁氧体能够降低Fe〜(2+)的氧化电位,并使氧化发生在上述pH值和电位区域内,因此生物浸出过程可以继续进行,对P-H_2O系统的E-pH图表明,H_3PO_4可以稳定存在。

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