广西某锰银矿工艺矿物学及锰的赋存状态

对广西某锰银矿进行了工艺矿物学的研究,查明了锰银原矿石矿矿物成分.金属矿物主要为硬锰矿、软锰矿、黄铁矿、赤铁矿和少量毒砂、黄铜矿、闪锌矿.矿石的主要结构是隐晶质结构、胶状结构、显微鳞片结构及砂质结构.主要的构造是脉状构造、胶状构造、浸染状构造.精矿中银品位是3 923 g.t-1,锰的赋存状态是独立的锰矿物,锰矿物是硬锰矿和软锰矿.精矿中硬锰矿在0.152~0.088 mm粒级范围内占17%,0.088~0.074 mm粒级范围内占38%;>0.074 mm粒级范围占40%;软锰矿在0.152~0.088 mm粒级范围内占18%,0.088~0.074 mm粒级范围内占35%;>0.074 m...     

黄绿色葡萄石的矿物学特征及谱学研究

葡萄石可以以板状、片状、葡萄状、肾状、放射状或块状集合体的形式产出,因其美丽的外观和特殊的晶体结构,近年来受到了学者的广泛关注。本文通过电子探针、粉晶X射线衍射仪、傅里叶变换红外光谱仪、显微拉曼光谱仪、紫外可见分光光度计等仪器对黄绿色葡萄石的成分、结构及谱学特征进行了分析与探讨。葡萄石的主要致色元素为Fe,且Fe³⁺经常取代Al³⁺占据八面体配位,Fe²⁺经常取代Ca²⁺存在于空隙中。电子探针数据表明:Fe与Al的含量变化整体呈现负相关关系,Fe与Ca的含量变化也整体呈现负相关关系,Fe含量相对较高的样品其黄绿色调加深。XRD图谱和拉曼光谱的结果表明:在葡萄石中绿帘石以包裹体的形式存在。红外光谱和拉曼光谱表明葡萄石中存在硅氧四面体和铝氧八面体两种架构,紫外可见吸收光谱揭示了葡萄石的致色机理。本文对葡萄石的矿物学特征及谱学特征进行系统分析,为后续葡萄石的进一步研究提供思路与实验数据。     

湖南永和海泡石粘土的矿物学研究

作者应用x射线衍射、红外光谱、差热分析、电子自旋共振及透射电镜研究了湖南浏阳永和海泡石粘土的矿物学特征,确定了由于类质同像替换在海泡石和滑石结构中存在着晶格缺陷,为进一步探讨它的工业利用提供了必要的资料。     

河北近北庄磁铁矿的矿物学和地球化学组成及其药用意义

通过采用X射线衍射（XRD）、X射线荧光光谱法（XRF）和电感耦合等离子质谱（ICP-MS）等分析方法对河北近北庄磁铁矿的矿物学和化学组成特征进行了分析,分析表明,河北近北庄磁铁矿为沉积变质型磁铁矿;磁铁矿样品中Zn、Se、Mn、Mo等人体必需的微量元素平均含量较高,富集系数分别为2.22、2.11、1.85、1.8,Zn、Mn等微量元素具有安神作用,表明该区磁铁矿有一定的医用价值.     

Mössbauer Spectroscopy in the Geosciences: Highlights and Perspectives

Single-walled and thin multiwalled carbon nanotubes are prepared by a catalytic-chemical-vapor-deposition method involving the simultaneous formation of Fe or Co nanometric particles from oxide solid solutions based on Al₂O₃, MgAl₂O₄ or MgO. This paper is an overview of the authors' work on the characterization by Mössbauer spectroscopy used in complement to electron microscopy and specific-surface-area measurements. It is notably attempted to correlate the nature of the different iron phases in the carbon nanotube-metal-oxide powders with the formation mechanisms of the nanotubes. Massive composites and hydrogen storage are proposed as possible applications.     

攀西微细粒钛铁矿工艺矿物学特征

以传统工艺矿物学研究方法为基础,结合化学分析、XRD,SEM及MLA等手段,对微细粒钛铁矿物料的化学组成、矿物组成、粒度分布、矿物嵌布特征进行了研究,在此基础上,对物料分选特性进行了讨论分析.研究结果表明:物料中67.04%的有价元素Ti赋存在钛铁矿中,脉石矿物主要为钛辉石、绿泥石和长石;物料中-19μm粒级产率达74.33%,其中各矿物粒度分布差别较大,有用矿物粒度较脉石矿物细;钛铁矿矿物单体解离度为90.43%,与钛辉石紧密连生.该研究结果为攀西微细粒钛铁矿物料的高效回收提供了依据.     

镍钼矿中胶硫钼矿的赋存状态及浮选试验研究

通过多元素分析,物相分析,扫描电子显微镜等检测,发现镍钼矿中的钼主要赋存于胶硫钼矿中,S∶Mo原子个数比介于2.72～2.94之间,且胶硫钼矿与黄铁矿,镍黄铁矿共生关系密切。通过闭路浮选试验,可以获得含Mo质量分数为10.55%,回收率为84.06%的精矿,精矿中钼质量分数95.54%以胶硫钼矿存在。     

RELATION BETWEEN THE OPTICAL ANISO-TROPY INDEX AND THE POLARIZABILITY ELLIPSOID OF ATOM GROUPS

The optical anisotropy index is a new conception which has been proposed by the author of this paper on the basis of the Gladstone refractivity (i.e. specific energy by Larsen). The conception is very useful for studying the structural-optical mineralogy. The polarizability ellipsoid of atom groups in minerals may be obtained from the optical anisotropy index; conversely, when the crystal structure, orientation, and the polarizability ellipsoid of atom groups are known, the optical anisotropy index of the minerals may be calculated, and then three principal refractive indices, and the optical axis angles may be calculated, too. The calculated values of optical properties are in very good agreement with the experimental values. This calculation method is much simpler thanBragg's for the carbonates, and the precision of calculated values is much higher than that of Bragg's. The principle of calculation method is suitable for all the minerals containing some strong anisotropic atom groups, besides carbonat     

KTB iron mineralogy at iridium deficient layers revealed by Mössbauer spectroscopy

Mössbauer spectroscopic studies of two sedimentary layers from Petriccio section in Gubbio formation are presented. It is found that these layers have almost the same iron phases nanophase hematite and phyllosilicate and with the same compositions as those in the Cretaceous-Tertiary Boundary (KTB) in Petriccio. The two layers also show enhancement in the siderophile elements such as Cr, Ni, Fe, Ca etc. to that found in the KTB layer. The two layers are well separated from the KTB layer, 128 and 149 cm below this layer, and show no enhancement of iridium. From the data it is suggested that the two layers also represent some kind of impact by extraterrestrial (ET) bolides.