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The effect of sodium sulphate on the hydrogen reduction process of nickel laterite ore

机译:硫酸钠对红土镍矿氢还原过程的影响

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A series of nickel laterite ores with different calculated amounts of anhydrous sodium sulphate were prepared by physical blending or sodium sulphate solution impregnation. The reduction of the prepared nickel laterite ore by H_2 was carried out in a fluidised-bed reactor with provisions for temperature and agitation control, and the magnetic separation of the reduced ore was performed using a Davis tube magnetic separator. The mineralogical properties of the raw laterite ore, reduced ore and magnetic concentrate were characterised using ICP, TG-DSC, N_2 adsorption, X-ray diffraction and optical microscopy. The catalytic activity of sodium sulphate was also studied by using Hydrogen temperature-programed reduction. The experimental results indicate that Na_2SO_4 could overcome the kinetic problems faced by the laterite ore and that it exhibited noticeable catalytic activity only if the temperature reached at least 750 °C This high temperature accelerated the crystal phase transition of the silicate minerals and increased the utilisation of H_2. In comparing the results from the two different methods for adding Na_2. SO_4, the nickel content and recovery of the magnetic concentrate were increased by using the impregnation method rather than the physical blending method and the increasing amount of sodium sulphate assisted in the further beneficiation of nickel. The partial pressure of H_2 and the reducing time also affected the reduction process of the iron oxides. The results of the microscopic study indicated that the formation of a Fe-S solid solution, which was derived from the SO_2 sulphide reduction of FeO, was conducive to mass transfer and accelerated the coalescence of metallic ferronickel particles. For the nickel laterite ore, under the synergistic effect of sodium sulphate and hydrogen, a nickel content and nickel recovery of 6.38% and 91.07% were obtained, respectively, with high product selectivity.
机译:通过物理混合或硫酸钠溶液浸渍制备了一系列具有不同计算量的无水硫酸钠的红土镍矿。在具有温度和搅拌控制的条件下,在流化床反应器中通过H_2将制备的镍红土矿石还原,并且使用戴维斯管磁分离器进行还原矿石的磁分离。利用ICP,TG-DSC,N_2吸附,X射线衍射和光学显微镜对未加工的红土矿石,还原矿石和磁性精矿的矿物学特性进行了表征。还使用氢气程序升温还原技术研究了硫酸钠的催化活性。实验结果表明,Na_2SO_4可以克服红土矿石所面临的动力学问题,并且只有在温度达到至少750°C时,Na_2SO_4才表现出明显的催化活性。高温加速了硅酸盐矿物的晶相转变,并提高了硅酸盐矿物的利用率。 H_2。比较两种添加Na_2的方法的结果。通过使用浸渍法而不是物理掺混法,SO_4,镍含量和磁性精矿的回收率增加,并且硫酸钠的增加有助于镍的进一步选矿。 H_2的分压和还原时间也影响了铁氧化物的还原过程。微观研究结果表明,Fe-S固溶体的形成是由于Fe_2O_2硫化物还原生成的Fe-S固溶体有助于传质并加速了金属镍铁颗粒的聚结。对于红土镍矿,在硫酸钠和氢的协同作用下,镍含量和镍回收率分别达到6.38%和91.07%,具有较高的产品选择性。

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