山西省繁峙县香坪钼矿地质特征及找矿标志

分析了香坪钼矿矿床的区域地质背景和地质特征,提出了矿床的成因及找矿标志,对今后找矿具有重要的指导意义。     

低品位难选钼中矿的选别试验

在研究福建省某钼矿厂难选低品位钼中矿性质基础之上,通过高效捕收剂、组合抑制剂的优化配伍,结合浮选与重选技术,实现了该钼矿物的高效综合利用,得出合理的浮选流程结构与药剂制度和最佳的重选工艺参数.浮选钼精矿产品品位为45.14%,回收率达到64.7%,钼浮选尾矿由重选可分别获得硫精矿和重选钼精矿,其中重选钼精矿产品品位为3.17%,回收率达到17.2%,整个流程中钼总回收率达到81.9%.     

微米级二硫化钼作为添加剂的润滑油性能研究

将表面改性后的微米级二硫化钼添加至基础油中,利用MRS-10W型和M-2000型试验机,对所制备润滑油的摩擦学性能进行测定.结果表明,基础油中添加含量为1.5%的微米级二硫化钼后,润滑油的最大无卡咬载荷提高了15.5%,摩擦副之间的摩擦系数降低了33.1%,磨损量减少了43.5%.     

皖南大坞尖钨(钼)矿床地质特征及成因分析

大坞尖钨(钼)矿床是皖南地区新发现的小型钨(钼)矿床.该矿床的矿体主要呈似层状,主要赋存于蓝田组下段白云质灰岩和钙质泥岩中.赋矿围岩以强烈的绢云母化、硅化和碳酸盐化为特征,矿石矿物为白钨矿和辉钼矿,脉石矿物主要有石英和绢云母.矿床的形成可划分4个成矿阶段,即无水矽卡岩阶段、含水矽卡岩阶段、石英硫化物阶段和碳酸盐阶段.通过对矿床地质特征和控矿因素的综合分析研究,认为大坞尖钨(钼)矿床属矽卡岩-云英岩复合型热液矿床,研究区具有重要的找矿潜力.     

pH值对浸矿细菌的活化以及金精矿脱砷的影响

通过在摇瓶中设定6个不同初始pH值梯度1.3,1.5,1.7,1.8,1.9,2.1,对细菌的活化以及高砷金精矿的脱砷浸出进行了研究.细菌活化阶段,HQ-0211菌在pH值1.3~1.9范围更加适应,活化速度快,氧化效果好.高砷金精矿细菌脱砷阶段,初始pH值在1.7~1.9范围最利于细菌浸矿,停滞期短,氧化速度快.初始pH值较高,为2.1时,细菌会较快进入衰亡期,不适于细菌浸矿.初始pH值较低,为1.3~1.5时,细菌适应停滞期长,氧化脱砷速度缓慢.     

低品位钼精矿的钼提取研究

采用焙烧—氨浸—渣碱浸工艺对某低品位钼精矿进行钼提取的研究.结果表明,碳酸钠的加入能有效分解钼酸钙,提高钼的提取率.焙烧—氨浸阶段最优工艺条件为焙烧温度600℃,焙烧时间2 h,氨浸温度80℃,氨水过量系数1.4,碳酸钠用量467 kg/t,液固比4.浸出渣中的钼分别采用酸法(HCl)和碱法(Na2CO3+NaOH)进行提取.结果表明:酸法仅可回收渣中34.92%的钼,而且操作过程不易控制,不适合实际应用;碱法(Na2CO3+NaOH)处理工艺中碳酸钠用量533 kg/t,氢氧化钠用量433 kg/t.放大实验结果显示整个流程钼的回收率达到96.8%.     

Solid FeS lubricant: a possible alternative to MoS2 for Cu-Fe-based friction materials

Molybdenum disulfide (MoS2) is one of the most commonly used solid lubricants for Cu-Fe-based friction materials.Nevertheless,MoS2 reacts with metal matrices to produce metal sulfides (e.g.,FeS) and Mo during sintering,and the lubricity of the composite may be related to the generation of FeS.Herein,the use of FeS as an alternative to MoS2 for producing Cu-Fe-based friction materials was investigated.According to the reaction principle of thermodynamics,two composites—one with MoS2 (Fe-Cu-MoS2 sample) and the other with FeS (FeS-Cu2S-Cu-Fe-Mo sample),were prepared and their friction behaviors and mechanical properties were compared.The results showed that MoS2 reacted with the Cu-Fe matrix to produce FeS,metallic ternary sulfides,and Mo when sintered at 1050℃.The MoS2-Cu-Fe and FeS-Cu2S-Cu-Fe-Mo samples thereby exhibited similar characteristics with respect to phase composition,density,hardness,and tribological behaviors.Micrographs of the worn surfaces revealed that the stable friction regime for both composites stemmed from the iron sulfides friction layers rather than from the molybdenum sulfides layers.     

He-Ar isotopic system of fluid inclusions in pyrite from the molybdenum deposits in south margin of North China Block and its trace to metallogenetic and geodynamic background

The helium and argon isotopic compositions of the ore-forming fluids from the molybdenum deposits such as Jinduicheng, Donggou, Shijiawan, and Sandaozhuang, which are located in the East Qinling molybdenum belt in south margin of North China Block （SMCNB）, are reported in this paper. The origin and the evolution of the ore-forming fluids and their coupled-relationships with the intra-continental collision and orogenic process of Qinling Orogen in Mesozoic-Cenozoic have been discussed. The 3He/4He and 40Ar/36Ar values （3He/4He=1.38-3.64 Ra, and 40Ar/36Ar=295.68-346.39, respectively） of the fluid inclusions in pyrite from the molybdenum deposits in East Qinling suggest that, the ore-forming fluid system is mixed by two end members. One is the high temperature deep-derived fluid congenetic with the porphyries generated by crust-mantle mixing, and the other is the low-temperature meteoric water which is rich in crustal radiogenic He with the component of atmospheric Ar. From the Pb isotopic composition, and ore-bearing potential of the porphyry and the regional stratum, we can conclude that the ore-forming materials of the deposits in the East Qinling molybdenum belt are derived from the deep source by the mixing of lower crust and upper mantle. Therefore, the formation of the molybdenum deposits in SMNCB can be related to the crust-mantle interaction, which is accompanied by the intra-continental orogenic and extension process in the post-collision period of Qinling Orogen. The granitic porphyries which are related to Mo mineralization are not simple crust-remelting type granites or S type granites, but belong to syntexis-type or mantle-derived granites, hence their formation has a profound and regional geodynamic background.     

低品位硼铁矿中硼的富集

采用还原焙烧、磁选工艺流程和粉矿直接入炉焙烧技术,对难选低品位硼铁矿中硼的富集进行了研究.按化学当量比C/O=1(原子比)进行配碳,使用马弗炉进行焙烧实验,在500～1 450℃研究了不同焙烧温度下硼品位和硼回收率的变化.研究结果表明:随着焙烧温度的提高,铁晶颗粒增大,在1 200℃时硼精粉品位达到14.29%,满足硼化工工业对硼品位的要求(ω(B2O3)≥12%);硼回收率在1 200℃以上时能达到90%以上.当焙烧温度在1 350℃以上时,硼的回收率和品位没有太大的变化.焙烧温度选择在1 200～1 350℃为宜,既能实现高的硼回收率,硼品位又能满足硼化工工业的要求.     

高压密封消解石墨炉原子吸收测定土壤中的全钼

对密封消解石墨炉原子吸收光谱法测定土壤中全钼的各参数条件进行研究。建立密封消解石墨炉原子吸收光谱法测定土壤中全钼的方法。在最佳测试条件下,钼方法检出限为0．32μg／L,测定相对标准偏差为1．1％,样品加标回收率为92．7％-102．2％．用于土壤中全钼的测定,结果满意。