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Inter-particle water infiltration dynamics of iron ore fines during granulation process

机译:造粒过程中铁矿石粒子的颗粒渗透动力学

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Inter-particle water infiltration dynamics of iron ore fines and concentrates was investigated using Washburn Capillary Rising method to evaluate the effect of various raw material conditions presented in the iron ore sintering process. The final water content and initial infiltration rate of the ores were determined from the measured infiltration curves and found to be heavily affected by the ore type and the blending, pre-wetting and packing conditions. The final water content of the ores was found to increase with the voidage of the packed ore bed. Ores forming a more permeable bed with a larger voidage is expected to achieve a higher final water content. The final water content of the blended ores showed an intermediate value between the component ores and can be readily predicted from the final water content of the component ores. Like the dry ore, the pre-wetted ore showed a similar infiltration curve. However, compared with the dry ore, the pre-wetted ore picked a considerably less amount of water at the end of infiltration test because some voidages were occupied by initial water. The initial infiltration rate of the ores was found to be greatly governed by the specific surface area, then bed voidage and contact angle. The Canadian magnetite concentrate showed the fastest initial infiltration rate of 3.0 x 10(-9) kg(2)/s likely due to its smallest specific surface area On the other hand, the Brazilian ores consisting of micro-porous hematite measured the smallest infiltration rate of 3.2 x 10(-10) kg(2)/s due to their largest specific surface area Unlike the final water content, the initial infiltration rate of the blended ores cannot be readily calculated from the component ores due to the nonlinear relationship between the initial infiltration rate and specific surface area. Pre-wetting was believed to improve the wettability and connection of ores with infiltrated water, leading to a faster completion of infiltration. (C) 2018 The Authors. Published by Elsevier B.V.
机译:使用keyburn毛细管上升法研究了铁矿石渗透性和浓缩物的颗粒渗透动力学,评价铁矿石烧结过程中各种原料条件的效果。从测量的渗透曲线确定最终水含量和初始渗透速率,发现受矿石类型和共混,预润湿和包装条件的严重影响。发现矿石的最终水含量随着包装矿床的空隙而增加。预期形成具有较大空隙的更渗透性床的矿石预期达到更高的最终含水量。混合矿体的最终水含量显示在组分矿石之间的中间值,并且可以从组分矿石的最终含水量方便预测。与干燥矿石一样,预染色的矿石显示出类似的渗透曲线。然而,与干燥矿石相比,预染色的矿石在渗透试验结束时挑选了相当少量的水,因为一些空隙由初始水占据。发现矿石的初始渗透率由特定表面积大大管辖,然后大大管辖,然后是床床停留和接触角。加拿大磁铁矿浓缩物显示出最快的3.0×10(--9)千克(2)/ s的最快渗透率,另一方面是其最小的比表面积,由微多孔赤铁矿组成的巴西矿石测量了最小的渗透由于其最大的比表面积与最终含水量不同,3.2×10( - 10)kg(2)/ s的速率,由于非线性关系之间的非线性关系,不能容易地计算混合矿石的初始渗透速率初始渗透率和特定表面积。认为预润湿可改善渗透水的润湿性和连接,导致渗透的更快完成。 (c)2018作者。 elsevier b.v出版。

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