Metallographic Analysis of Cu-Zr-Al Bulk Amorphous Alloys with Yttrium Addition

Minor yttrium addition can improve the glass-forming ability of Cu-Zr-Al ternary alloys via suppression of the growth of eutectic clusters. Yttrium addition also makes the room temperature ductility of the alloys decrease, and both the compressive strength and elastic strain limits increase slightly.

LnMsbO_6和Ln_2M_2O_7 (M = Zr, Ti)复合氧化物的合成、组成、结构及发光等性质的研究

在综合文献报导的基础上，我们选择了LnMsbO_6和Ln_2M_2O_7 (M = Zr, Ti)做为研究体系，对其合成、组成、结构以及稀土离子在其中的发光性质进行了较为系统的研究。用氢氧化物共沉淀的方法，在等摩尔阳离子原料配比条件下，我们制备了LnMsbO_6和Ln_2M_2O_7(M = Zr, Ti, Ln = La - Yb, Y除Ce和Pm)。根据对组成的分析结果并与文献对比，我们认为得到的化合物组成与给出的分子式是一致的。由热分析并结合x-ray衍射分析对LnZrsbO_6的形成反应进行了研究，其结果表明化合物的形成过程是一个较慢的固相反应过程。通过x-ray粉沫衍射物相分析并结合掺杂Eu~(3+)的发光光谱，我们确定了在不同条件下合成的LnMsbO_6和Ln_2M_2O_7化合物的结构类型，并计算了所有化合物的晶胞参数。在对上述结构特性及其变化规律进行研究后，我们认为Ln_2M_2O_7结构变化规律与ΔZ/(d~2) (Z为阳离子电荷，d为阳离子与阴离距离)有关，随ΔZ/(d~2)值由小到大，Ln_2M_2O_7(M = Zr, Ti)先是形成具有荧石结构的阳离子无序固溶体，然后逐渐过渡到荧石结构的变型——有序的立方烧绿石结构，最后变型到单斜晶系结构。LnMsbO_6(M = Zr, Ti)低温相结构与Ln_2M_2O_7(M = Zr, Ti)是有联系的，即基本保持了其立方晶系结构。然后锑的加入使这种结构变得很不稳定，因此在高温灼烧下上述立方相将不可逆地变为更稳定的高温结构相。利用磁天平对LnMsbO_6和Ln_2M_2O_7进行了室温条件下的磁学性质测量，其玻尔磁子数的实验值与Van Vleck理论值符合较好。由此也可说以说明化合物的组成与给出的分子式是一致的。用荧光光谱仪对Eu~(3+)在不同基质中做发光光谱，其结果表明Eu~(3+)在烧绿石结构的Ln_2M_2O_7中，Ln~(3+)是处于具有反演中心的D_(3d)格位，这时~5D_0 → ~7F_2的电体极跃迁（～610nm）是被禁阻的，因此Eu~(3+)主要的发光为~5D_0 → ~7F_1磁体极跃迁（～590nm），并劈裂为两条谱线。在其它不具有反演中心的格位中Eu~(3+)的~5D_0 → ~7F_2跃迁则是较强的。在La~(3+)有着多个较低对称性格位的La_2Ti_2O_7:Eu中，无论是Eu~(3+)的激发光谱，还是发射光谱，其~5D_0与~7F_0之间的跃迁谱线都不只一条，这与La~(3+)多对称性格位特性是一致的。在立方荧石结构的LnZrsbO_6:Eu中，用Eu~(3+)电荷迁移带激发的发光光谱与用其它激发带激发的很不相同，其~5D_1能级的跃迁谱线非常强，我们认为这可能是由于电荷迁移激发态，将大部分能量传递给3~5D_1能级的结果。另外，我们比较了在Ln_2Zr_2O_7和LnZrsbO_6中Eu~(3+)的发光强度，发现前者要比后者强许多。在研究Bi~(3+)对Eu~(3+)的敏化作用时，我们发现在Y_2M_2O_7:Bi, Bu中Bi~(3+)对Eu~(3+)有较好的敏化作用，而在YMsbO_6:Bi, Eu中则没有。同时我们注意到对于Eu~(3+)取代六配位La~(3+)格位时，其电荷还移带位置和符合Hoefdraad认为是不变的规律，而是随着基质晶格的不同发生变化的。对Dy~(3+)在LnMsbO_6和Ln_2M_2O_7基质中发光性质研究中，我们看到Dy~(3+)的发光主要为兰色的~4F_(9/2) → ~6H_(15/2)跃迁(～480nm)和黄色的~4F_(9/2) → ~6H_(13/2)跃迁(～580nm)。其黄光与兰光的强度比值（R）随基质晶格的不同可以有很大的变化。一般情况下R值总是要大小1，且不随湿度和Dy~(3+)掺杂浓度变化。同时我们比较了在Ln_2Zr_2O_7和LnZrsbO_6 (Ln = Y, Gd, La)基质体系中Dy~(3+)的发光强度，发现同Eu~(3+)类似前者较后者强许多。在论文中我们给出了在Y_2M_2O_7和YMsbO_6 (M = Zr, Ti)中Sm~(3+)的激发光谱与发射光谱，从中可以看到当Sm~(3+)在Y_2Ti_2O_7中取代占据D_(3d)格位的Y~(3+)时，其~4G_(5/2) → ~6H_(9/2) (～650nm)电体极跃迁是被禁阻的。同时还给出了在YZrsbO_6中H_0~(3+)和Er~(3+)的激发光谱与发射光谱。此外，我们研究了Eu~(3+)和Dy~(3+)在一些基质体系中发光强度随温度的变化规律。发现Y_2Zr_2O_7:Eu的临界猝来温度要比La_2Zr_2O_7:Eu的高，Ln_2Zr_2O_7:Dy (Ln = La, Y)的温度猝来曲线则大致相同，且随温度和猝来要比Ln_2Zr_2O_7:Eu缓慢，对于上述现象我们利用位形坐标给出了一定的解释。然而所有的样品发光强度从室温开始，随温度的升高都是单调下降的。

Electrocatalytic properties of Cu-Zr amorphous alloy towards the electrochemical hydrogenation of nitrobenzene

The Cu-Zr amorphous alloy was studied as an electrocatalyst towards the electrochemical hydrogenation of nitrobenzene. The electrocatalyst was activated by chemical etching in HF solution. Resulted changes in the morphology, chemical composition and crystalline structure of the electrocatalyst surface were characterised by scanning electron microscopy, X-ray diffraction and Auger electron spectroscopy. The electrocatalytic properties of the Cu-Zr amorphous alloy were assessed by voltammetric measurements. Due to the formation and aggregation of Zr residue modified Cu nanocrystals on the surface caused by the selective dissolution of Zr components in the chemical etching, the activated amorphous alloy is an effective electrocatalyst for the electrochemical reduction reaction of nitrobenzene with aniline as the main product. The positive shift of the peak potential and accompanying increase in the value of peak current in voltammograms with increasing Cu content and decreasing Zr content of the alloy surface in the chemical etching are indicative of improved electrocatalytic activity. (C) 2002 Elsevier Science B.V. All rights reserved.

稀土Sm对于Cu/Zr基合成醇催化剂的改性作用

中国科学院山西煤炭化学研究所

Energy Dissipation In Fracture Of Bulk Metallic Glasses Via Inherent Competition Between Local Softening And Quasi-Cleavage

Compression, tension and high-velocity plate impact experiments were performed on a typical tough Zr41.2Ti13.8Cu10Ni12.5Be22.5 (Vit 1) bulk metallic glass (BMG) over a wide range of strain rates from similar to 10(-4) to 10(6) s(-1). Surprisingly, fine dimples and periodic corrugations on a nanoscale were also observed on dynamic mode I fracture surfaces of this tough Vit 1. Taking a broad overview of the fracture patterning of specimens, we proposed a criterion to assess whether the fracture of BMGs is essentially brittle or plastic. If the curvature radius of the crack tip is greater than the critical wavelength of meniscus instability [F. Spaepen, Acta Metall. 23 615 (1975); A.S. Argon and M. Salama, Mater. Sci. Eng. 23 219 (1976)], microscale vein patterns and nanoscale dimples appear on crack surfaces. However, in the opposite case, the local quasi-cleavage/separation through local atomic clusters with local softening in the background ahead of the crack tip dominates, producing nanoscale periodic corrugations. At the atomic cluster level, energy dissipation in fracture of BMGs is, therefore, determined by two competing elementary processes, viz. conventional shear transformation zones (STZs) and envisioned tension transformation zones (TTZs) ahead of the crack tip. Finally, the mechanism for the formation of nanoscale periodic corrugation is quantitatively discussed by applying the present energy dissipation mechanism.

Ti-V-Cr固溶体储氢合金的结构及电化学性能研究

本论文首先研究了Ni、Zr分别对Ti-V－Cr固溶体储氢合金中Cr和Ti部分取代的影响，得到了性能良好的Ti0．17Zr0．08V0．35Cr0．10Ni030基质合金。在此基础上进一步研究了入甄、B、Fe、Co、Al元素的添加或取代对基质合金的结构及电化学性能的影响。采用XRD、ICP、SEM一EDX、XPS、EIS、线性极化和阳极极化等表征手段对Ti一V－Cr固溶体储氢合金的结构及电化学性能进行分析和表征，主要结果如下：①Ti一V－Cr合金自身在碱性电解液中几乎无电化学活性。当用Ni部分取代Cr后，合金中出现具有电化学活性的第二相，其电化学性能得到有效地改善和提高。②Ti0.25-xZr_xV0.35Cr0.1Ni0.3（x＝0．05-0．15）合金主要是由bcc相和c14Laves相组成。随Zr含量从0．05增加到0．08，合金电极的放电容量和倍率放电能力增加；当x继续从0．08增加到0．15时，其变化较小。合金电极的电荷转移电阻随x增加而降低，当x在0．08到0．15之间变化时，电荷转移电阻变化也比较小。表明电荷转移电阻的大小与合金的电化学性能密切相关。③经过50次充、放电循环后，Tio．17zr"sV时scrol0Ni03。合金电极在303K和313K的放电容量能保持在90％以上；在70℃时的放电容量仍能达到275mA扮g。根据不同温度时的交换电流密度，计算了Ti。，17Zr008V时SCr川0Ni030合金电极表面电化学反应的表观活化能，其值约为50kJ／mol。④通过Nln、B、Fe、C。、AI对Tio．17zroosvo35Crol0Nio3。合金基质的添加与取代的研究，得到了具有高容量的储氢合金。其中Tio．17Zr008Vo35Cro．10Ni020Mnol。合金室温最高放电容量达到390n1A扮g；在253一343K的温度范围内，Tiol7Zr08V035Cr0JONioz5Mnoos合金具有高的放电容量，其容量在167一298mA树g之间变化，但是这些合金的稳定性有待进一步的提高。⑤合金充、放电过程中，晶格的扭曲和膨胀、Zr和V的溶解使得合金结构发生变化；合金的严重粉化及表面致密氧化膜的形成，是导致Ti一V－Cr合金电化学性能的衰减的主要原因。

广西贺县龙水金矿床的同位素地球化学研究及成因探讨

广西贺县龙水金矿位于湘桂稳定区，桂粤交界山脉的北段，博白-茶陵深断裂的西侧，区内广泛发育加里东期到燕山期的花岗岩，出露的基底地层主要为震旦系到寒武系。本文主要研究龙水金矿II号矿化带。该带位于寒武系水口群清溪亚群和大宁花岗闪长岩体的接触带附近，围岩为寒武系的碳质板岩，矿脉为硫化物石英脉，主要有黄铁矿、方铅矿、闪锌矿和石英等矿物。金矿化与硫化物密切相关。主要的金矿物为银金矿，少许自然金。确定金矿床的成矿年龄一直是个比较刺手的问题。本文选择矿脉中信为是成矿期的石英作为Rb-Sr等时年龄测定的对象，是基于其纯净和其中的原生气液包体基本可代表成矿热液的特征。结果表明其Rb-Sr等时年龄为120.5Ma，并认为此年龄代表了成矿年龄。有石英Rb-Sr等时线的~(87)Sr/~(86)Sr初始比为0.732089, 与矿脉中碳酸相加矿物的Sr同位素比值（约为0.7337-0.7402）一起，表明Sr应是来自地壳的富Rb盐矿物的Sr源区。另外，为了与围岩的蚀变年龄对比，测定了近矿围岩的Rb、Sr同位素组成，结果形成两条等时线，年龄分别为245.9 Ma和173.6 Ma，表明成矿以前至少发生了两次地质事件，导致了Sr同位素的均一化。这两次地质事件分别与华南的东吴运动及燕山运动第一幕相对应。矿石Pb同位素的~(206)Pb/~(204)Pb、 ~(207)Pb/~(204)Pb 和~(208)Pb/~(204)Pb 分别在18.4-18.9、15.6-16.1和38.4-39.6的范围内，并在~(207)Pb/~(204)Pb vs ~(206)Pb/~(204)Pb坐标图上呈现出斜率为1左右的线性排布。只有个别数据点要以得出依据Doe模式的模式年龄，约为200 Ma。在Zart,am Pb构造模式中，矿石Pb同位素数据大部分位于上地壳Pb线以上，呈现出富放射性成因Pb的特征。为了解释异常Pb的成因，本文进行了定量计算。结果表明矿石Pb为古老的存留地壳Pb与少地幔源Pb的混合，即矿石Pb同位素经历了这样的演化过程：在39-29.8亿年间由地幔分异出的地壳 Pb，未参与壳幔循环作用，一直到燕山期，与少量幔源Pb混合，并加入成矿。混合μ值为9.85-10.22。矿石的地质情况及矿石Pb同位素的Δα-Δβ-Δγ示踪结果均支持这一结论。本文初次研究了脉石英中的U、Pb同位素组成。脉石英中Ｕ含量很低。Pb同位素组成基本可以划分为两组，一组为与方铅矿数据近似的普通Pb组成，另一组则较富放射性成因Pb，并向围岩的Pb同位素组成漂移，可能是随着热液的演化和大气降水的加入，受围岩Pb的影响所致。矿脉中硫化物样品的S同位素比值（加权平均为0.16‰）和碳酸盐矿物样品的C同位素比值（在-0.1～-4.1‰的范围内），表明其应为内生来源。根据脉石英的气液包体均一温度（180-250 ），计算与脉石英存在0同位素平衡的热液的同位素的同位素组成，结果为1.2～-4.8‰，表明有大气降水的参与。石英气液包体水溶液为弱碱性，其成分分析表明其中K_2O/Na_2和CaO/MgO（分别根据K~+/Na~+和Ca~(2+)/Mg~(2+)的换算）与围岩相差很大。另外，矿石中微量元素主要为Au、A2g、Cu、Pb、Zn、Co、Ni、Mo、Bi、Ga、As、Sb、和Hg，而围岩中微量元素则主要为Cu、Ni、Mn、V、Zr、Ti、Cr和Ba。因此，热液中成矿元素主要不是来自围岩。黄铁矿的Co/Ni、S/Se/的比值可以指示热液化的来源。龙水金矿矿脉中黄铁矿的Co/Ni > 1，S/Se < 15000，均在与岩浆作用有关的热液范围内。因此，热液活动应主要与岩浆岩有关。矿石、围岩和花岗闪长岩的稀土配分模式相似，均呈现向右倾斜的V字型，并且类似于太古代后沉积岩。结合Pb、Sr同位素的研究，推测花岗闪长岩的源岩主要为古老的地壳物质。概括起来，龙水金矿床为约120.5 Ma形成的中低温热液矿床；热液中成矿物质主要来自花岗闪长岩。由于围岩与矿床紧密的空间联系及围岩中的高Au含量，围岩可能提供了一部分Au及其他成矿物质。

HfO2的纯度对紫外多层膜反射率的影响

用辉光放电质谱法和二次离子质谱仪测定了两种HfO2材料及它们相应的单层膜中的杂质含量，结果发现，无论是在体材料中还是在用电子束蒸发技术沉积的材料单层薄膜中，ZrO2都是这两种HfO2材料中最主要的杂质。而且，这两种HfO2材料中Zr含量的差别远远大于Ti、Fe含量的差别，这说明Zr含量的差别正是引起两种HfO2膜层光学性能差别的原因。用这两种不同纯度的HfO2材料与同一纯度的SiO2材料组合，沉积形成266nm的紫外反射镜，实验结果表明这两种反射镜的反射率分别在99.85% 和 99.15%左右。这个结果与依据单层膜得出的光学常数所设计的结果符合的很好。

Structure and electrochemical characteristics of melted composite Ti0.10Zr0.15V0.35Cr0.10Ni0.30-LaNi5 hydrogen storage alloys

The structure and electrochemical characteristics of melted composite Ti0.10Zr0.15V0.35Cr0.10Ni0.30+x% LaNi5 (x=0, 1, 5 and 10) hydrogen storage alloys have been investigated systematically. XRD shows that the matrix phase structure of V-based solid solution phase with a BCC structure and C14 Laves phase with hexagonal structure is not changed after adding LaNi5 alloy. However, the amount of the secondary phase increases with increasing LaNi5 content. Field emission scanning electron microscopy-energy dispersive spectroscopy (FESEM-EDS) shows that the C14 Laves phase contains more Zr and the white lard phase has a composition close to (Zr, Ti)(V, Cr, Ni, La)(2).

Hydrogen absorption in Ti45Zr35Ni17Cu3 amorphous and quasicrystalline alloy powders

Ti45Zr35Ni17Cu3 amorphous and icosahedral quasicrystal line (I-phase) powders were synthesized by mechanical alloying (MA) and subsequent annealing, the phase structure and hydrogen absorption properties of two powders were investigated. XRD analysis indicated that the MAed powder was an amorphous phase and annealed powder was an I-phase. Two alloy exhibited excellent hydrogen adsorption property and started to absorb hydrogen without induction time. PCT measurement showed that the plateau pressure of the amorphous powders was obviously higher than that of the I-phase powders. After the first hydrogen cycling, the partial amorphous phase changed to (Zr, Ti)H-2 phases, and the I-phase was steady. Similar hydride phases Ti2ZrH4 and (Zr, Ti)H-2 were also formed after the second hydrogen cycling for the amorphous and I-phase alloy powders.

东天山镁铁-超镁铁岩铜镍硫化物矿床通道式成矿机制与岩体含矿性评价研究

A mafic-ultramafic complex belt well developed in Eastern Tianshan, Xinjiang, NW China, which contains a series of Cu-Ni sulfide deposits. This area is the important production basis for Cu-Ni deposits, including Tulargen deposit, Hulu deposit, Huangshan-Huangshandong deposit, Hulu deposit, Xiangshan deposit, Tianyu deposit, Chuanzhu deposit. In China, especially Eastern Tianshan, it is prevalent that large Cu-Ni deposits occurred in small intrusions, typically including Jinchuan, Kalatongke, et al., so the ore-forming mechanism and evaluation rule for those small intrusions are very meaningful and of universal significance. On the basis of the research to typical Cu-Ni deposits, ore-forming conditions and processes are summarized through which to evaluate the ore-bearing potential for barren intrusions and unexplored mafic-ultramafic intrusions. By the contrast, metallogenic rule and mechanism of ore genesis are concluded, and evaluation system is preliminarily set up on the basis of these conclusions. Quantitatively simulation for the composition of olivine is introduced for the first time in China to discuss the interaction between magma and sulfide, and a new method to calculate the Mg-Fe composition of primitive magma is developed. Interaction between magma and sulfide liquid is used to get the Ni content in sulfide liquid. Sulfur isotopic characteristics in sulfide minerals in country rocks and ores are used to judge crustal sulfur introduction, which is applied for the first time in China. Re-Os isotopic characteristics are related to the ore-forming process, to interpret the process of enrichment of chalcophile elements. On the basis of the evaluation system, Mati, Chuanzhu, Luodong, Xiadong, those intrusions are evaluated to their ore-bearing potential. According to the studies to typical Cu-Ni deposits, conduit-type ore-forming model is set up, and the characteristics of the model are concluded systematically. The evaluation system and conduit-type ore-forming model can be helpful to the evaluation of mafic-ultramafic intrusions in this and similar mafic-ultramafic intrusion belts. The studied typical deposits and mafic-ultramafic intrusion include Tulargen deposit, Hulu deposit, Huangshandong deposit, Chuanzhu deposit, Mati intrusion，Luodong intrusion, Xiadong intrusion, and others. Through studies, there are similar characteristics for Tulargen and Hulu deposits in magma origin, composition of primitive magma（MgO=12.5%, FeO=12% and MgO=11%, FeO=10.5% respectively）, magma evolution, mechanism of sulfide segregation and conduit-type ore-forming process. By Re-Os isotopic system, the ore forming date of Tulargen deposit is 265.6±9.2Ma, which is consistent to regional metallogenic event, but little younger. The Mg-Fe composition of primitive magma of Baishiquan, Huangshandong area, Kalatongke is lower than that of Tulargen and Hulu deposit, showing common basalt composition. The Mg# value（Mg#=(Mg/Mg+Fe）increases gradually from Kalatongke to Baishiquan to Huangshan-Huangshandong East. Baishiquan intrusions show relatively higher crustal contamination by evidence of trace element, which indicates the lower magma original source, from depleted mantle to crust. One break is the discovery of komatiitic intrusion, Xiadong intrusion, which shows characteristics of highly magnesium (Max Fo=96). The primitive magma is calculated of MgO=28%，FeO=9%, belonging to komatiitic magma. Tectonic evolution of Eastern Tianshan is discussed. By the statistics of ore-forming data of porphyry copper deposits, magmatic sulfide Cu-Ni deposits, orogenic hydrothermal gold deposits, we believe that those deposits are the successive products of oceanic subduction, are and back-arc basin collision and post-orogenic extention. And Cu-Ni sulfide deposits and orogenic gold deposits occurred in the stage of post-orogenic extention. According to the conclusions, the conduit-type ore-forming mechanism of magmatic sulfide deposit is set up, and its characteristics and conditions are concluded as well. The conduit-type ore-forming system includes magma generation, sulfide segregation, enrichment of chalcophile elements, interaction of sulfide and magma, sulfide collection in limited space in magma conduit and bottom of the chamber, which make a whole ore-forming system.The ore-forming process of Cu-Ni sulfide deposits is concluded as three steps: 1. mantle derived magma rises upward to the middle-upper crust; 2. magma suffers crustal contamination of different degrees and assimilates crustal sulfur, which leads to sulfur saturation and sulfide segregation. Sulfide liquid interacts with magma and concentrates chalcophile elements; 3. enriched sulfide located in the conduit(Tulargen) or bottom of the chamber (Hulu). Depleted magma rises upward continuously to form barren complexes. For the practical cases, Tulargen deposit represents the feeding conduit, and Hulu deposit represents the bottom of the staging magma chamber. So the deeper of west of Tulargen and southwest of Hulu are the favorite locate for ore location. The evaluation for ore potential can be summarized as follows: (1) Olivine can be served as indicator for magma evolution and events of sulfide segregation; (2) Sulfur isotopic characteristics is an efficient method to judge sulfur origin for magmatic sulfide deposit; (3) Re-Os content of the ores can indicate interaction between sulfide and silicate magma and crustal contamination; (4) PGE mineralization is effected by degree of partial melting of mantle; (5) Cu/Zr is efficient parameter to judge sulfide segregation; (6) The effects of multiple magma fractionation and emplacement are important, for inverse order shows the destruction to previous solid lithofacies and orebodies. Mati, Chuanzhu, Xiadong, Luodong, mafic-ultramafic intrusions are evaluated using evaluation system above. Remarkable Ni depletion is found in olivine of Mati, and southwest of the intrusion can be hopeful location for ore location. Chuanzhu intrusion has remarkable evidence of sulfide segregation, but the intrusion represents the narrow feeder conduit, so the wide part of the conduit maybe the favorite location for sulfide to deposit. The ore potential of Luodong and Xiadong is not good. Both the intrusions show no Ni depletion in olivine, and there is no sulfide in country rocks, so no crustal sulfur is added into the magmatic system. For Sidingheishan, a very large intrusion, the phenomenon of sulfide segregation is found, but there are no favorite places for sulfide to deposit. So the Cu-Ni ore potential maybe not good, but PGE mineralization should be evaluated further.