ZrO_2 颗粒弥散 MoSi_2 陶瓷力学性能及氧化性能

研究了ＺｒＯ２颗粒弥散ＭｏＳｉ２陶瓷的力学性能及氧化性能．结果表明，ＺｒＯ２颗粒同时实现了室温相变韧化和高温弥散强化双重作用，显著提高了复合材料的室温强韧性及高温强度，同时复合材料仍具有较优良的抗氧化性能．     

关于延长导焦溜槽使用时间的探讨

对焦仓导焦溜槽入焦口频繁破损、更换困难这一生产难题进行研究,采用嵌入式铬钼合金表面焊接处理耐磨夹套对焦仓导焦溜槽进行改造,以解决因焦炭冲击、磨损导致导焦溜槽频繁更换的状况.     

金精矿中银的打萨宗光度分析法研究

本法基于在微酸性（ｐＨ４～５）介质中，银（Ⅰ）与打萨宗生成内络盐显色络合物，被ＣＣｌ４（或氯仿、苯）定量萃取，呈黄色，λｍａｘＣＣｌ４为４６０ｎｍ，ε４６０为３０５×１０４Ｌ·ｍｏｌ－１·ｃｍ－１．方法操作简捷，具有灵敏度和准确度比较高等特点，在０１～２５ｍｇ／Ｌ范围，符合Ｌａｍｂｅｒｔ－Ｂｅｅｒ定律．     

APT结晶母液处理新工艺

根据钨钼化合物性质的差异 ,运用分子设计的理论和方法 ,研究出一种用选择性沉淀法从APT结晶母液中除去钼及砷、锑、锡等杂质 ,并从除钼后的溶液中进一步回收WO3和NH4Cl的新工艺 .回收的WO3以APT形态产出 ,其质量达GB1 0 1 1 6— 88中APT— 0级要求 ,回收率达 90 %～ 95 % ;回收的NH4Cl质量完全符合配制解吸液的要求 ,其实收率达 6 0 %以上 .和工业上处理APT结晶母液的现行工艺相比 ,该工艺能带来明显的经济效益     

含铀硼精矿碳解过程中铀硼分离

含铀硼精矿在ＣＯ中还原焙烧得到熟矿粉，硼的活性为９０．８３％，用通ＣＯ２的碳酸钠水溶液碳解，Ｂ２Ｏ３溶出率在８６％以上，铀溶出率４．８８％，碳酸体系中加适量ＦｅＳ，铀溶出率降至０．６２％以下，较好地实现了铀硼分离。     

MoSi_2基复相材料的研究进展

通过对MoSi2 复相材料近年来研究进展的总结 ,阐述了合金化和复合化对MoSi2 基复相材料性能的改善 .着重叙述了MoSi2 SiC系复相材料的制备方法 ,以及增强相的含量对力学性能的影响 .研究结果表明 ,通过基体的改性和复合化 ,使复相材料的强韧性得到很大程度的提高 ,而不同的制备工艺所得到材料的性能有成倍的差异 .因此 ,协同优化增强剂种类、数量和多种制备工艺的有机结合 ,是制备高性能复相材料的关键 .同时 ,介绍了几种有发展前景的复相材料 ,并提出了MoSi2基复相材料的研究发展趋势 .     

气相色谱法测定金属钼粉中氧含量

采用氢气还原金属钼粉中的氧,以无水甲醇作吸收液,吸收还原产生的水,应用气相色谱法测定吸收液中水的含量以确定金属钼粉中可被氢还原氧的含量。结果表明,本法测定结果与国标方法测定结果基本一致。方法适用于中小型企业实际生产中金属粉末中氧含量的常规测定。     

钼的硫化反应热力学分析

钨钼分离是钨提取冶金中的1道重要工序．目前工业上应用的分离方法大都基于钨和钼对硫亲和力的差异,在一定条件下使MoO2-4硫化为MoS2-4而进一步除去,因而研究有关硫化反应的理论对于寻找最佳工艺条件有重要指导意义．作者通过热力学计算,对钼的硫化行为进行了考察．研究结果表明为使钼完全硫化,溶液的pH值要低于8;实践中所采用的n(S)=4n(Mo)且溶液中游离0.125mol/L,远超过热力学平衡需要,实际上是考虑到动力学原因;在上述条件下钼可完全硫化．     

二硫化钼-硅异质结太阳电池的原位制备及器件模拟

 二维材料与晶体硅形成的异质结太阳电池是当前太阳电池研究热点之一,大多数研究都集中在石墨烯和硅形成的肖特基结太阳电池。为改善器件的能带结构,本研究采用具有一定禁带宽度的n-MoS₂二维半导体材料与p-Si 形成异质结太阳电池。通过实验研究了退火时间对MoS₂材料合成的影响,并对MoS₂-Si异质结的暗电流和光电流曲线进行测量和分析。通过异质结模拟软件wx-AMPS对MoS₂-Si异质结结构进行效率计算和能带分析,探讨了薄膜厚度和载流子浓度对器件开路电压的影响。     

Ore-forming event and geodynamic setting of molybdenum deposit at Wenquan in Gansu Province, Western Qinling

The Wenquan molybdenum deposit is associated with a Triassic granite in this area. The Wenquan granite is enriched in LILE and LREE, poor in HFSE, and has significantly higher contents of alkali （K2O＋Na2O） and Sr, Ba than those of the island arc volcanic rocks. These geochemical characteristics are similar to post-collisional granites in high K calc-alkaline series. Studies of major elements, trace elements, REEs and chronology of the Wenquan pluton show that, in the geodynamic transition stage of continent-continent convergence to extension, the partial melting of the enriched lithospheric mantle generated the basaltic magma and triggered the partial melting of the thickened lower crust which produceded the acidic magma, and the Wenquan pluton was formed by mixing of the two magmas. Molybdenite Re-Os isotopic dating gave Os model ages of 212.7±2.6 Ma to 215.1±2.6 Ma with a weighted mean of 214.1±1.1 Ma, and an Re-Os isochron age of 214.4±7.1 Ma. These ages are close to K-Ar ages （223 to 226 Ma） and a SHRIMP zircon U-Pb age （223±7 Ma） for the Wenquan granite within the error range, but relatively younger. This implies that the Mo mineralization occurred in a late stage of the magmatic intrusion, and the metallogenesis took place in the transition stage from syn-collision to post-collision in the tectonic setting of the Qinling Orogenic Belt （QOB） after continental collision between the North China Block （NCB） and the South China Block （SCB）. This process is also corresponding to the geological events of metamorphism and deformation in South Qinling, closure of the Mian-Lue oceanic basin, and exhumation of the Dabie-Sulu ultrahigh-pressure metamorphic rocks. The large-scale continent-continent collision between NCB and SCB in the middle Triassic triggered significant crustal thickening and exhumation of subducted slab. In the late Triassic, the tectonic setting was transformed to the transition stage from collision to extension. Materials from the asthenospheric mantle would ascend into the root of the lower crust, which could induce partial melting of the lower crust and generate Mo-enriched granitic magma. The ore-forming elements enriched in the fluid derived from the condensation and fraction of the magma resulted in the Mo mineralization. The Mo deposits in the QOB are mainly formed in two episodes, namely 220± Ma and 140± Ma. The two episodes of metallogenesis were developed in the tectonic transition settings from compression to extension, but they were in the different stages of the tectonic evolution. The occurrence of the Wenquan Mo-bearing pluton indicates that the Triassic tectonic-magmatic belt of Western Qinling is another favorable region for Mo mineralization in the QOB. Therefore, it is significant to pay more attention to evaluation of the ore-forming potentiality in the Triassic granites in Western Qinling.