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首页> 外文期刊>Minerals Engineering >Phosphorus recovery from high concentrations of low-grade phosphate rocks using the biogenic acid produced by the acidophilic bacteria Acidithiobacillus thiooxidans
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Phosphorus recovery from high concentrations of low-grade phosphate rocks using the biogenic acid produced by the acidophilic bacteria Acidithiobacillus thiooxidans

机译:使用由嗜酸性细菌酸酐产生的生物酸的高浓度低级磷酸盐岩的磷回收

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摘要

In this paper, we are presenting a two-step biological process to recover phosphorus solubilizing low-grade phosphate rocks. We start with a "growing" stage, where the biogenic acid produced by the acidophilic bacteria Acidithiobacillus thiooxidans endows the proper conditions for solubilization. It is followed by a "recovery" stage, where the phosphate rock is added to the culture once desired levels of acidity are reached. We varied the concentration of the phosphate rock and the bacterial growing time to elucidate optimal conditions and to get insight into the biological process. We found that 10% (w/v) of phosphate rock with 23 days of bacterial growth results in a recovery of 94%. FTIR spectrums and XRD-Rietveld quantification reveal that the high phosphorus solubilization is correlated with gypsum as the predominant phase, whereas, for less efficient conditions, a significant proportion of fluorapatite, predominant in the un-treated rock, is still observed. As a general trend, increasing the bacterial growing time results in higher amounts of phosphorus recovery. However, the biogenic acid is unable to efficiently solubilize rock concentrations higher than 20% due to an inhibition in the diffusion controlled reaction. We present a one-to-one comparison with a chemical acidulation using sulfuric acid. The biogenic acid shows better performance and achieves higher percentages of recovery at all conditions, thereby suggesting that additional metabolites in the A. thiooxidans culture enhance the bioleaching. Finally, we delineated an economical viability that indicates that the chemical recovery is four times more expensive than the biogenic method. From a technological perspective, our process offers fertile grounds for non-conventional and efficient phosphorus recovery in tropical soils or for low-grade phosphate rock reservoirs.
机译:在本文中,我们正在提出两步生物过程,以回收磷溶解低级磷酸盐岩石。我们从“生长”阶段开始,其中嗜酸性细菌酸噻吩硼硫胺产生的生物酸赋予溶解的适当条件。随后是“恢复”阶段,其中达到培养物后磷酸盐岩石一旦达到所需水平的酸度。我们改变了磷酸盐岩的浓度和细菌生长时间,以阐明最佳条件,并对生物过程深入了解。我们发现10%(w / v)磷酸盐岩,细菌生长23天导致回收率为94%。 FTIR光谱和XRD-RIETVELD定量揭示了高磷溶解与石膏作为主要阶段相关,而对于较少的有效条件,仍然观察到未处理的岩石中的荧光磷酸盐的显着比例较大。作为一般趋势,增加细菌生长时间导致较高量的磷恢复。然而,由于在扩散控制反应中的抑制,生物酸不能有效地溶解高于20%的岩石浓度。我们使用硫酸与化学酸化一度相比。生物酸表现出更好的性能,并且在所有条件下达到更高的恢复百分比,从而提示A.硫代氧酰胺培养物中的额外代谢物增强了生物浸出。最后,我们描绘了经济的存活率,表明化学回收率比生物方法昂贵四倍。从技术角度来看,我们的过程为热带土壤中的非常规和有效的磷恢复提供了肥沃的基础,或用于低级磷酸盐岩储层。

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