黔西北某地伴生多金属低品位铁矿工艺矿物学研究

以化学分析、化学物相分析、透反射显微镜及EPMA为主要研究手段,对黔西北某地伴生多金属低品位铁矿的工艺矿物学特征进行了详细研究。该区含矿岩石为一套以火山成因为主的火山碎屑岩,矿石中有价元素除铁外,伴生有钛、铜、镓、铌等。载铁矿物工艺矿物学研究结果表明,矿石中铁主要以褐铁矿形式存在,与粘土矿物常常混杂出现,分布不均,团块大小差异也大,矿物间的嵌布关系复杂,提示依靠传统物理选矿难达到有用矿物的富集。除褐铁矿外,矿石中存在少量硅铁钛金属互化物。     

破碎矿体分段凿岩阶段嗣后充填采矿法实践

为解决黄沙坪矿79#1-1矿体由于矿体含硫高、矿岩破碎不稳固、允许暴露面积小、矿山无胶结充填系统,因而开采困难的问题,进行中深孔成孔试验和孔底温度监测试验,在此基础上提出长锚索预护顶下分段凿岩阶段嗣后充填采矿法。文中介绍了该方法的特点、结构尺寸、采准切割与回采工艺。现场工业试验表明,该方法实现了矿体安全、高效的回采。     

酸碱淋溶对尾矿砂含水率和重金属含量的影响

为研究酸碱溶液对尾矿砂含水率和重金属含量的影响,采用室内土柱动态淋溶的方法,对采自阜新同乃矿尾矿坝的尾矿进行实验,测得不同pH溶液动态淋溶后的尾矿砂含水率,并应用火焰原子吸收光谱法,测出尾矿砂中6种重金属元素在淋溶后的含量,结果表明:①经酸碱溶液淋溶后尾矿砂土体的含水率出现增加的现象;②淋溶液pH从4增加到7时,Cu和Cr的含量逐渐减少,淋溶液pH从7增加到10时,Cu和Cr的含量逐渐增加;相反Mn和Ni的含量先随pH的增加而增加,在pH大于8和8.5左右开始降低;Fe含量出现略微减少的趋势;Cd含量在淋溶液pH 4～6.5范围内逐渐增加,而后含量降低。文中淋溶液选择的是酸碱溶液而不是纯净水,所以用此结果描述尾矿库的环境和安全情况更具有实际意义。     

临江羚羊铁矿石深度还原试验研究

针对原矿品位为34.79%的吉林临江羚羊铁矿石,进行了深度还原单因素条件试验;考察了还原温度、还原时间、料层厚度等因素对深度还原及磁选分离结果的影响.试验结果表明,还原温度、还原时间对深度还原过程的影响较大.在配煤过剩倍数2.0,还原煤粒度-1.5 mm和矿石粒度-2.0 mm的条件下,适宜的深度还原条件为还原温度1 275℃,还原时间50 min,料层厚度30 mm.在该试验条件下,获得了最终产品含铁质量分数93.05%,回收率85%,金属化率91.29%,达到我国炼钢用直接还原铁H92产品标准要求.     

菱铁矿对假象赤铁矿与石英混合矿浮选的影响

碳酸铁对铁矿石的浮选影响极大,严重恶化浮选指标.在三种浮选体系下,研究菱铁矿含量对假象赤铁矿与石英混合矿浮选的影响.结果表明,在十二胺和油酸钠反浮选体系下,菱铁矿加入到两种混合矿中时,浮选指标下降.十二烷基硫酸钠体系下,假象赤铁矿和石英混合矿中加入少量菱铁矿时,精矿品位有所增加.因此,若要实现含碳酸盐铁矿石的有效分选,必须首先消除细粒级菱铁矿的影响.     

山西省临县刘家庄矿区铝土矿矿石特征

山西省临县刘家庄矿区铝土矿详查,采用深部钻探、浅井工程,并结合采样化验等工作方法和手段,基本查明山西省临县刘家庄矿区铝土矿矿体(层)的数量、产状、厚度、规模、形态特征;基本查明矿石的矿物种类、含量、共生组合及矿石结构构造特征,矿石的化学成分、有益有害组分的种类,划分矿石的自然类型和工业类型;通过初步可溶性试验基本查明矿石中Al2O3可溶性及赤泥沉降性能;为进一步勘探提供了充分可靠的依据。     

山西繁峙县金鸡沟矿区多金属矿地质特征及成矿规律

繁峙县金鸡沟多金属矿区位于华北地台北缘,山西断隆—五台隆起北东部,矿区经多次构造变动,在区内形成了一系列断裂破碎带,后经热液多次充填、叠加,金、多金属元素得到进一步的富集,在部分有利地段形成了金、多金属矿体。通过对地质、矿床特征、控矿因素的分析研究,总结出了区内构造发育,岩浆活动频繁,矿产资源丰富,周边已知金属矿产有金、银、铜、铅、锌、钼、铁矿床多处,成矿地质条件良好,找矿潜力巨大。     

浅谈代县西曲网沟铁矿矿体地质特征

从矿层厚度、矿石品位、矿体规模、开采工程地质条件等方面分析了代县西曲网沟铁矿的矿床地质特征．提出了该矿的工业意义。     

VSM and Mössbauer study of nanostructured hematite

In the present work, we have synthesized nanostructured hematite samples using chemical precipitation method. The crystal structure and the grain size of the samples were studied using XRD. The zero field cooled and field cooled magnetization curves of the samples were recorded in the temperature range from 300 to 10 K. The variations of Morin transition temperature and blocking temperature with the grain size of the samples were investigated. The hysterics curves of the samples were recorded and the samples showed a superparamagnetic nature at room temperature whereas, at 10 K the samples showed open hysteresis curves. The sample with smaller grain size showed higher value of coercivity compared to samples with larger grain size. Mössbauer spectra of the samples were recorded and the grain size dependence on Mössbauer parameters was investigated.     

Al‐for‐Fe substitution in hematite: the effect of low Al concentrations in the Raman spectrum of Fe2O3

Five different mixed Al‐hematites with an aluminium molar content varying from 0 to 10% were investigated by micro‐Raman spectroscopy to study the effect of Al‐for‐Fe substitution on the hematite lattice. A red shift of hematite vibrational wavenumbers and a line broadening were observed; also a shoulder located near 430 cm⁻¹ and a broad band at 670 cm⁻¹ developed. The variation of the spectral features is discussed in terms of a local disorder correlated to the insertion of Al³⁺ ions into the Fe(O)₆ octahedra constituting hematite structure. A multivariate analysis was also carried out on the spectral data to distinguish between the doped samples analysed. Copyright © 2007 John Wiley & Sons, Ltd.