Mineralogy and carbothermal reduction behaviour of vanadium-bearing titaniferous magnetite ore in Eastern India

Vanadium-beaxing titaniferous magnetite bands hosted by Precambrian gabbro-norite-anorthositic rocks or their metamorphic equivalents were discovered in some parts of Eastern Indian Shield, containing 48%-49% Fe （total）, 10%-25% TiO2, and 0.3%-2.20% V2O5 by mass. Mineralogical and petrological study, composition, and characterization of the vanadium-bearing titaniferous magnetite ore were carried out by scanning electron microscopy-energy dispersive X-ray （SEM-EDX）, wave length X-ray florescence （WDXRF）, inductively coupled plasma-atomic emission spectroscopy （ICP-AES）, X-ray diffraction （XRD）, etc. Chemical beneficiation for valuable metals, such as Fe, Ti, andV, was performed by reduction roasting. The direct and indirect reduction were investigated by mixing the lump ore with solid activated charcoal in a closed reactor and purging the reducing gas mixture in standard reducibility index apparatus at different temperatures and time intervals. The reduction roasting parameters were optimized. Finally, the reduced samples were crushed and upgraded by magnetic separation. The results show that, the maximum mass fractions of magnetic and nonmagnetic parts achieved axe 69.36% and 30.64%, respectively, which contain 10.6% TiO2 and 0.84% V205 in the magnetic part and 36.5% TiO2 and 0.22% V205 in the nonmagnetic part.     

一种风化低品位铁矿石的可选性试验

随着铁矿资源的日益贫乏,对低品位矿石的开发利用成为选矿的发展趋势。山东省某矿业公司矿石属于风化程度较高的低品位铁矿石,样品粒度为10～0mm,含水量1％～2％。根据试样的性质和风化矿分选的经验,采用干式磁选抛尾、干选粗精矿再磨再选的试验流程,获得品位为66％的精矿产品,对低品位铁矿石的开发利用具有一定的借鉴意义。     

红格矿深还原一熔分过程及钒、铬走向的研究

深还原一熔分固相还原后的金属化球团生产钒铬生铁是利用红格矿的途径之一．由于V2O5与CrO3,的赋存、分布以及冶炼过程中的走向基本一致,综合回收利用二者可一起考虑．为了提高钒、铬回收率,实现钛和铁的有效分离,通过单因素试验考察了在氩气保护下,配料的碱度、深还原一熔分温度和配碳量对熔分过程和钒、铬走向的影响．结果表明,当熔渣碱度为1.2,配碳量为0.5％,熔分时间为15min,熔分温度为1610℃时,渣铁的分离效果较好,且有利于钒、铬熔于铁相．     

东秦岭铅锌银金钼多金属成矿带成矿规律及找矿标志

东秦岭位于华北板块与扬子板块之间的拼合带———秦岭造山带东段。该区是一典型的地球化 学急变带与地球物理梯度交叉区,壳幔富含Pb,Zn,Au,Ag,W,Mo元素,为一元古宙—古生代裂陷槽, 熊耳群、宽坪群、二郎坪群、耀岭河组火山岩系中的火山喷发Cu,Pb,Zn,Ag,Au矿(化)层;秦岭群、官道 口群、栾川群、陶湾群滨海、浅海陆缘碎屑碳酸盐建造中强烈的火山喷(气)发活动形成的硅质条带(团 块)硅质岩以及含Ag,Pb,Zn,Au矿化层状矽卡岩带,多期次的构造岩浆活动,使区内Pb,Zn,Ag,Au, W,Mo叠加富集体成矿,从而使东秦岭地区Pb,Zn,Ag,Au,W,Mo多金属矿床在区域分布、成矿空间、 时间上呈现出一定的规律性和明显的找矿标志。     

铬渣中铬的赋存形态表征和酸浸出特性

为研究铬渣在湿法解毒技术无害化处理过程中重金属污染物铬的浸出特性,对铬渣进行了酸中和能力实验,分析了不同p H条件下铬渣中总铬和6价铬及其他主要金属元素的溶出特性,并采用X射线荧光仪、X射线衍射仪、扫描电子显微镜以及热重分析对铬渣中的元素组成和矿物物相组成进行表征.得出硫酸硝酸法和TCLP法毒性浸出实验中浸出液中Cr主要以Cr6+形式存在.铬渣的强碱性且在碱性范围内有较大的缓冲能力以及复杂的物相组成是制约湿法还原铬渣处理效果的两个主要因素,因此,优选工艺p H条件来提高铬渣中铬的溶出率是提高湿法还原处理效率的关键,浸出p H在8.0左右时,能够获得较高的6价铬浸出率且处理成本相对较低.