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Atmospheric acid leaching mechanisms and kinetics and rheological studies of a low grade saprolitic nickel laterite ore

机译:低品位腐泥镍红土矿石的大气酸浸机理及动力学和流变学研究

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Improved atmospheric acid leaching (AL) of complex, low grade nickel (Ni) laterite ores warrants greater knowledge of the exact processes underpinning Ni and pay metal cobalt (Co) extraction rates, acid consumption and pulp handleability. In this study, the influence of agitation rate (600-1000 rpm) and temperature (70 and 95 degrees C) on the isothermal, batch acid leaching and rheological behaviour of saprolitic Ni laterite slurry (40 wt% solid) was investigated over 4 h at pH 1. The leaching behaviour was distinctly incongruent and reflected strong temperature-dependent Ni/Co extraction, acid consumption and the proliferation of gangue minerals' constituent elements (e.g., Na, Mg, Al, Fe). Whilst the total mass of acid consumed per ton of dry ore processed was greater at higher temperature, the total kg acid consumed per kg Ni and Co extracted was markedly lower. In all cases, the slurries displayed time-dependent, non-Newtonian, shear thinning rheological behaviour. The pulp viscosities and shear yield stresses were generally greater at lower than at higher temperature, with both increasing dramatically in the course of 4 h leaching. Agitation rate in the range 600-1000 rpm had no noticeable impact on Ni and Co leaching rates, confirming the insignificance of volume diffusion limitation. Although high pulp shear viscosities in the range 37-120 mPa s were observed in the course of leaching, they did not have an impact on Ni and Co leaching mechanisms and kinetics from the saprolitic laterite ore. The mechanism of saprolitic laterite ore leaching appears to follow a chemical reaction controlled, shrinking core model with apparent activation energies of 75.5 +/- 3.8 and 81.2 +/- 4.1 kJ/mol, respectively, for the release of Ni and Co. (C) 2015 Elsevier B.V. All rights reserved.
机译:复杂的低品位镍(Ni)红土矿石的改善的大气酸浸(AL)保证了对支撑Ni的确切工艺有更多的了解,并支付了金属钴(Co)的萃取率,酸消耗和纸浆可处理性。在这项研究中,研究了搅拌速率(600-1000 rpm)和温度(70和95摄氏度)对腐殖质镍红土浆料(固体含量40 wt%)的等温,分批酸浸和流变行为的影响,历时4小时。在pH为1时,浸出行为明显不一致,反映出强烈的温度依赖性Ni / Co萃取,酸消耗和脉石矿物成分元素(例如,Na,Mg,Al,Fe)的扩散。在较高温度下,每吨干矿石所消耗的酸总质量较高,而每千克提取的Ni和Co所消耗的总酸总千克显着较低。在所有情况下,浆液都显示出时间相关的,非牛顿的,剪切稀化的流变行为。在较低的温度下,纸浆的粘度和剪切屈服应力通常要比在较高的温度下大,在4 h的浸出过程中两者都急剧增加。搅拌速度在600-1000 rpm范围内对Ni和Co的浸出速度没有明显影响,证实了体积扩散限制的重要性。尽管在浸出过程中观察到了高的纸浆剪切粘度,范围为37-120 mPa s,但它们对腐泥红土矿石的Ni和Co浸出机理和动力学没有影响。腐泥红土矿石浸出的机理似乎遵循化学反应控制的,收缩的岩心模型,对于镍和钴的释放,表观活化能分别为75.5 +/- 3.8和81.2 +/- 4.1 kJ / mol。 )2015 Elsevier BV保留所有权利。

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