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首页> 外文期刊>Minerals Engineering >Evaluation of residence time distribution and mineralogical characterization of the biooxidation of sulfide minerals in a continuous stirred tank reactor
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Evaluation of residence time distribution and mineralogical characterization of the biooxidation of sulfide minerals in a continuous stirred tank reactor

机译:连续搅拌釜反应器中硫化物矿物的生物氧化停留时间分布和矿物学表征的评估

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摘要

The residence time distribution (RTD) of the liquid phase and the mineralogical characterization of the biooxidation of refractory gold mineral was studied in a continuous stirred tank reactor. The latter was achieved using a native mixed culture of acidophilic mesophiles. The RTD was assessed using a mathematical model of stirred tanks in parallel. The oxidation of sulfide and the phases generated through the biooxidation process were evaluated via X-ray diffraction (XRD).The results indicated that the experimental RTD fit to the model. The reactor has a high tendency to behave as a completely mixed reactor. However, the mixed flow inside the reactor has disturbances such as by-pass and dead zones. The estimated mean residence time for the model was approximately 36% greater than the theoretical residence time. It was probably caused by the delay in the outflow of the tracer due to gas hold-up, foaming at the top and the design of the reactor outlet structure. The XRD outcomes showed that the oxidation of arse-nopyrite was greater than that of pyrite. Similarly, the formation of jarosite and brushite was observed. It was concluded that the dead zones could increase the probability of jarosite precipitations.
机译:在连续搅拌釜反应器中研究了液相的停留时间分布(RTD)和难熔金矿物的生物氧化的矿物学特征。后者是通过使用嗜酸性中温细菌的天然混合培养物实现的。使用并行搅拌釜的数学模型评估RTD。通过X射线衍射(XRD)对硫化物的氧化和生物氧化过程中产生的相进行了评估,结果表明实验RTD符合模型。该反应器倾向于表现为完全混合的反应器。但是,反应器内部的混合流会产生干扰,例如旁路和死区。该模型的估计平均停留时间比理论停留时间大约大36%。这可能是由于气体滞留,顶部起泡以及反应器出口结构设计问题导致示踪剂流出延迟所致。 X射线衍射结果表明,砷铁矿的氧化作用大于黄铁矿的氧化作用。类似地,观察到黄钾铁矾和透钙磷石的形成。结论是,死区可以增加黄铁矿降水的可能性。

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