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作 者:赵瑞超[1,2] 韩跃新 何明照[3] 李艳军 ZHAO Rui-chao;HAN Yue-xin;HE Ming-zhao;LI Yan-jun(School of Resources & Civil Engineering, Northeastern University, Shenyang 110819, China;School of Coal & Mining Engineering, Inner Mongolia University of Science & Technology, Baotou 014010, China;CITIC Pacific Mining Management Pty Ltd., 45 St. Georges Terrace, Perth, WA6000, Australia)
机构地区:[1]东北大学资源与土木工程学院,沈阳110819 [2]内蒙古科技大学矿业与煤炭学院,包头014010 [3]CITIC Pacific Mining Management Pty Ltd.,45 St.Georges Terrace,Perth,WA6000,Australia
出 处:《中国有色金属学报》2018年第5期1076-1082,共7页The Chinese Journal of Nonferrous Metals
基 金:“十二五”国家科技支撑计划项目(2012BAB14B05); 中央高校基本科研业务费重大科技创新项目(N140108001); 内蒙古科技大学创新基金项目(2011NCL042)
摘 要:在相同的球磨条件下,对4种窄粒级的绿泥石进行实验室分批湿式球磨试验。结果表明:4种粒级绿泥石的磨矿动力学都遵循一阶磨矿动力学,球磨0.25~0.5 mm的绿泥石时获得最大的破碎速率函数Si=0.35 min^(-1),正常的破碎粒级范围应该小于0.5 mm;在较短的磨矿时间内,0.25~0.5 mm绿泥石的细粒级产出具有明显的零阶产出特征;采用G-H算法获得0.25~0.5 mm粒级绿泥石的累积破碎分布函数Bij,利用磨矿总体平衡动力学模型,对粒级为0.25~0.5 mm的绿泥石进行球磨模拟仿真计算,试验结果与模拟仿真结果高度一致。Under an invariant mill environment, batch wet ball grinding studies were carried out by grinding four mono-sized fractions of single mineral of chlorite. The results show that all mono-sized fractions of chlorite follow the first-order breakage mechanism. The maximum breakage rate for chlorite, obtained in the feed size fraction of 0.25-0.5 mm, is 0.35 min^-1. The normal breakage behavior is obtained when the feed size is less than 0.5 mm. The fine fraction output for 0.25-0.5 mm size fractions of chlorite has a clear the zero-order output characteristics at a relatively short grinding time. The cumulative breakage distribution functions for 0.25-0.5 mm size fractions of chlorite are obtained using G-H algorithm. The simulated product size distribution data obtained,using the discrete-size, continuous-time Population Balance Model(PBM), are consistent with experimental data for 0.25-0.5 mm size fractions of chlorite.
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