内蒙古白云鄂博超大型REE-Nb-Fe矿床脉状矿化时代与成矿流体特征

Bayan Obo REE-Nb-Fe ore deposit is the largest REE deposit in the world. Owing to its unique type and tremendous economic value, this deposit has widely attracted interests from geological researchers and vast amount of scientific data have been accumulated. However, its genesis, especially ore-forming age and REE sources, have been under dispute for a long time. On the basis of previous research works, this paper mainly conducts studies on the Early Paleozoic ore-forming event in the Bayan Obo deposit. The following results and conclusions can be suggested: Sm-Nd isotopic analytical results of bastnaesite, beloeilite, albite and fluorite samples from a coarse-crystalline ore lode present an isochron age of 436±35Ma. Besides, Rb-Sr isotope dating of the coarse-crystalline biotite lode that intruded into banded ores gives an isochron age of 459±39Ma. The two ages verify the exist of Early Paleozoic ore-forming event at Bayan Obo, which characterized by extensive netted mineralization of REE fluorocarbonates, aeschynite and monazite, accompanied by widely fluorite-riebeckite-aegirine-apatite alteration. Sr-Nd isotope composition of vein minerals is located between EMI and ancient lower crust component in the ISr(t)-εNd(t) correlation diagram, indicating that there is a crustal contamination during veined mineralization. A large area late Paleozoic granitoids are distributed in the southeast region of east open pit of the mine. The granitoids intruded directly into the ore-bearing dolomite, and produced intense skarnization. Moreover, at 650-660m of the drill core on 22 line and 1598m level flat in the south of East Open Pit, we firstly found skarnization rocks. Single grain and low background Rb-Sr isochrone dating on phlogopite in skarn gives 309±12Ma. Considering the intruded contacting relationship, the late Paleozoic granitoids, already extended to the under part of REE ore bodies, must be posterior to the latest intense REE mineralization, and is only a destructive tectonic and magmatic activity. Fluid inclusion types of fluorite in the Bayan Obo deposit consist of multiphase daughter mineral-bearing inclusion, two or three phase CO2-bearing inclusion and two phase aqueous inclusion. Petrography, laser Raman analysis and microthermometry study indicate that the fluids involving in REE-Nb-Fe mineralization at Bayan Obo might be mainly of H2O-CO2-NaCl-(F-REE) system. The presence of REE-carbonate as a daughter mineral in fluid inclusions shows that the original ore-forming fluids are rich in REE elements.

可见光响应光催化剂K4Ce2M10O30（M=Ta, Nb）及其光解水特性的研究

氢能已被广泛认为是最具有潜力解决能源危机和环境问题的理想替代能源之一，其开发备受各个领域科学家的重视，更是从根本上解决环境地球化学工作者的主要目标：对已被破坏的环境和生态进行修复以及对可能破坏环境与生态的人类活动进行干预和指导。在众多的氢能开发手段中，利用太阳能光催化分解水制取氢气是一种兼顾能耗、资源和环境的最为理想和最有前途的氢能开发手段之一。在光催化分解水过程中，最为首要的研究内容就是开发具有适宜能带结构能响应可见光，稳定地、高量子效率地光解水的固相半导体光催化剂。 本论文中，通过高温固相反应合成了呈四方晶系钨青铜结构的半导体光催化剂K4Ce2M10O30(M=Ta, Nb)，吸收边分别达到580 nm (M＝Ta) 和690 nm (M＝Nb)，对应带隙为2.2 eV和1.8 eV。可见光下（λ> 420 nm）光催化分解H2O产生H2和O2的活性表明它们不仅有适宜的带隙响应可见光，并且其价带和导带位置能满足完全分解水的电化学电位需要。在担载Pt、RuO2以及NiO（NiOx）等助催化剂对产氢性能有显著的提高。同时以乙醇钽和草酸铌可溶性前驱体，分别通过溶胶凝胶法（Sol-gel）和聚合物络合法(Polymerizable Complex)制备了K4Ce2Ta10O30和K4Ce2Nb10O30。通过湿法化学合成的光催化剂显示了更高的光催化活性，并且通过PC法制备的K4Ce2Nb10O30更是实现了在大于300 nm 的光辐射下完全分解纯水产生摩尔比为约2:1 的H2和O2。 通过高温固相反应得到Nb取代K4Ce2Ta10O30中部分晶格Ta形成的单相无限固溶体系列K4Ce2Ta10-xNbxO30（x=0~10）是结构一致的同系物，吸收边介于540 nm～710 nm 之间，并且随着x的增加，吸收边依次红移，光催化产氢活性依次降低，但是x=2，5，8时的产氧活性比x=0和10的高，光催化活性的差异主要源于它们光吸收特性和能带结构的差异。基于密度范函理论DFT的第一性原理计算结果表明，光催化剂K4Ce2M10O30(M=Ta, Nb)的能带结构为：导带主要由Ta 5d (Nb 4d)组成，处于高能级的电子未占据态的Ce 4f 与其有很明显的重迭，但由于其高度局域特性，不能很好地参与光生电子在导带的传导，从而其对光催化活性的贡献很小，而价带则由O 2p与Ta 5d (Nb 4d)以及电子占据态的Ce 4f杂化轨道组成。同时通过高温固相反应合成了系列含稀土元素的光催化剂K4Re2M10O30(Re=La, Ce, Nd, Sm, Y; M=Ta, Nb)，通过对它们及其前驱体氧化物的光吸收特性以及电子结构的第一性原理计算研究，合理的解释了只有当Ln＝Ce时才具有可见光响应特性的微观机理。

白云鄂博超大型Fe-Nb-REE矿床碳酸盐脉状体的包裹体研究

白云鄂博矿床是世界上最大的Fe-Nb-REE矿床,其矿床成因一直是中外地质学家争论的焦点.而矿床附近的碳酸盐脉状体则成为赋矿白云岩岩浆成因的直接因素,该文拟从包裹体的角度对矿区碳酸盐脉状体进行研究,对其成因进行探讨,并对其与赋矿白云岩的关系作初步的讨论.通过对碳酸盐脉状体包裹体在包裹体类型,组合,均一温度,盐度,成分等方面的研究,发现不同区域,不同产状的碳酸盐脉状体包裹体特征存在较大的差异,这反映了其在岩石成因方面的差异:(1)都拉哈拉和尖山附近:为典型的岩浆成因;(2)宽沟背斜核部:可能是富碳酸盐盐熔体侵入构造裂隙形成的;(3)白云镇东北部(CV31,CV32)可能为侵入到混合岩中的热液脉;(4)东介勒格勒以南:具有明显的沉积特征.

Enhanced Plasticity of Zr-Based Bulk Metallic Glass Matrix Composite with Ductile Reinforcement

A composite material containing uniformly distributed micrometer-sized Nb particles in a Zr-based amorphous matrix was prepared by suction cast. The resulting material exhibits high fractured strength over 1550 MPa and enhanced plastic strain of about 29.7% before failure in uniaxial compression test at room temperature. Studies of the serrations on the stress-strain curves and the shear bands on the fractured samples reveal that the amplitude of the stress drop of each serration step corresponds to the extent of the propagation of a single shear band through the materials. The composite exhibits more serration steps and smaller amplitude of stress drop due to the pinning of shear band propagation by ductile Nb particles.

Microstructure Study Of Laser Welding Cast Nickel-Based Superalloy K418

Experiments of laser welding cast nickel-based superalloy K418 were conducted. Microstructure of the welded seam was characterized by optical microscopy (OM), scanning electron microscopy (SEM), X-ray diffraction (XRD), and energy dispersive spectrometer (EDS). Mechanical properties of the welded seam were evaluated by microhardness. The corresponding mechanisms were discussed in detail. Results show that the laser welded seam have non-equilibrium solidified microstructures consisting of Cr-Ni-Fe-C austenite solid solution dendrites as the dominant and some fine and dispersed Ni-3(Al,Ti) gamma' phase as well as little amount of MC needle carbides and particles enriched in Nb, Ti and Mo distributed in the interdendritic regions, cracks originated from the liquation of the low melting points eutectics in the HAZ grain boundary are observed, the average microhardness of the welded seam and HAZ is higher than that of the base metal due to alloy elements' redistribution of the strengthening phase gamma'. (C) 2008 Elsevier B.V. All rights reserved.