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%.     

The Discussion with Determination of Molybdenum in Geochemical Exploration Samples by Emission Spectrometry

文章采用发射光谱法测试水系、岩石、土壤等化探样品里高、中、低含量的钼元素,讨论了电极、缓冲剂等对样品测试结果的影响.     

4株根瘤菌菌株与热研5号柱花草共生最适钼浓度研究

采用砂培的方法,设7个钼水平,4个菌株,通过对株高增加、地上部产量、植株氮含量、根瘤数和固氮酶活性的测定及综合分析,确定使热研5号柱花草接种不同根瘤菌菌株达到最佳促生性能的钼浓度.结果表明：高浓度钼不利于产量的增加,缺钼不利于氮含量的增加;经主因子分析,热研5号柱花草接种LZ3-2的最适钼浓度为1 500 mg·L－1, 接种菌株RJS9-2及不接种的最适钼浓度为1 000～1 500 mg·L－1,接种菌株YM11-1最适钼浓度为500～1 500 mg·L－1;接种菌株PN13-3最适钼浓度为2 000 mg·L－1.     

钼酸盐复配绿色缓蚀剂的研究

用失重法研究了在自来水介质中,钼酸盐与硬脂酸钠(SS)和十二烷基苯磺酸钠(SDBS)对碳钢的缓蚀作用,讨论了产生协同效应的原因,分析了不同缓蚀配方的缓蚀效果,得到了较佳的复合配方。     

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%.     

精选教学内容提高小学语文课堂教学的有效性

每位教师每节课的时间相同,但为什么优秀教师教出来的学生学习能力强,学习成绩优秀,学习习惯好,同时又学得轻松愉快呢?这就涉及到教学有效性的问题."有效"是教学的本质特性,也是当前课程改革的核心思想,更是教育内涵发展的必然要求.教学的有效性是教学的生命,有效的教学应是教师永恒的追求.从课堂教学中教学内容的选取入手,探讨适合课堂教学的有效性策略问题.这些策略包括深入分析教材的内容,找出最主要、最基本、最本质的内容,参照可能规定给该课堂的教学时间,采用灵活的教学方法来进行课堂教学,以提高课堂教学效率.     

紫外光照射下钴钼杂多酸降解有机染料SRB

制备了不同配比的钴钼杂多酸（CoMox Heteropoly acids,CoMox）,在紫外光（λ≤387 nm）照射下,以有机染料酸性桃红（Sulforhodamine B,SRB）的光催化降解为探针反应,研究了CoMox杂多酸不同配比及用量和体系介质pH值对其降解行为的影响.结果表明,最佳配比的钴钼杂多酸为CoMo12,在pH=3.0,CoMo12用量为1.0 g/L时,对SRB降解效果最好.在紫外光照射下,CoMo12活化O2,3.5 h内SRB脱色率达到96%.通过紫外-可见吸收光谱（UV-vis absorption spectrum）,红外光谱（FTIR）和总有机碳（TOC）测定分析钴钼杂多酸对SRB的降解特性,同时采用苯甲酸荧光光度法跟踪测定降解过程中产生的活性氧化物种,表明CoMo12多酸对SRB的光催化降解过程主要涉及.OH氧化历程.     

Mo isotopes in the Lower Cambrian formation of southern China and its implications on paleo-ocean environment

Over the past decade, as one of nontraditional stable isotopes, Mo isotope has developed rapidly and now become an important geochemical proxy to trace paleo-oceanic and atmospheric evolution through geological history. In this paper, Early Cambrian formations in southern China are investigated. The results indicate that δ 97/95Mo values of Early Cambrian seawater may have been larger than 1.4‰, values that are close to those of the modern ocean. It was also found that the variations in Mo isotope composition in samples from two sections （Huangjiawan and Gezhongwu in Guizhou） were closely related to changes in redox conditions during sedimentary processes. Combining our results with existing data, a preliminary model for the evolution of seawater Mo isotope composition through geological history was provided. It indicated that Mo isotopic variations were generally consistent with the evolution of atmospheric oxygen.     

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.     

磷酸盐分解钼酸钙的热力学

针对磷酸盐分解钼酸钙的过程,根据同时平衡原理和质量守恒定律,绘制了25℃时Ca-Mo-P-H_2O体系溶解组分的lgC-pH图,以及不同总磷浓度条件下溶液中总钙、总钼的lgC-pH图和钼酸钙稳定区. 结果表明,在溶液中总磷浓度一定的条件下,随着pH的增大体系中会依次出现H_2MoO_4(s)、CaMoO_4(s)、Ca5(OH)(PO_4)_3(s)和Ca(OH)_2(s)稳定存在的区域. 总磷浓度直接影响到钼酸钙的分解过程,随着总磷浓度的增加,钼酸钙的稳定区域不断减小甚至消失,使得钼酸钙更加易于分解, 因此溶液中总钼浓度不断增大,而总钙浓度不断降低;但总磷浓度过高会导致溶液中残留游离含磷离子过高. 从热力学角度来看,在钼酸钙分解过程中,添加磷酸盐比碳酸盐更加有利于钼酸钙的分解.