小球藻的絮凝沉降及溶气气浮采收研究

研究了氢氧化钠对不同生长时期小球藻液的絮凝效果,比较了絮凝沉降法和溶气气浮法的采收效果,并初步优化了气浮操作参数。结果表明,在小球藻液中添加氢氧化钠能够取得很好的絮凝效果,添加700 mg/L氢氧化钠,沉降30 min即能达到90%的沉降采收率;同等氢氧化钠添加量下,溶气气浮法的采收效果要优于絮凝沉降法;确定的气浮采收最佳操作参数:指数生长期和稳定期藻液的最佳氢氧化钠添加量分别为350 mg/L和600 mg/L,溶气水进水流速为60 L/h,溶气水/藻液体积比为25%。絮凝沉降法中指数生长期和稳定期的小球藻液采收效果相差不大,而溶气气浮法中同等采收条件下指数生长期的采收率高于稳定期,其采收浓缩倍数也略高于稳定期。     

粉石英与红柱石的浮选分离机理研究

本文以油酸钠作为捕收剂,研究了磷酸氢二钠、柠檬酸和硅酸钠等抑制剂对粉石英与红柱石浮选分离效果的影响.结果表明,磷酸氢二钠是红柱石与粉石英浮选分离的一种优良的抑制剂;在其最佳浓度0.47×10-2 mol /L,浮选液pH值为8.5时,粉石英与红柱石浮选回收率差高达47.86％.红外光谱及Zeta电位分析结果表明,油酸钠对红柱石兼有物理和化学吸附作用,对粉石英仅有物理吸附作用,因而对红柱石有更强的捕收能力;磷酸氢二钠对粉石英表面起解吸作用,能有效抑制粉石英起浮,从而实现粉石英与红柱石的分离.     

山东省日照石英岩矿除铁试验方法简介

山东省日照石英岩矿中的铁矿物主要以黄铁矿和褐铁矿为主，根据该矿石的性质，采用浮选、浮选一磁选、磁选3种选别方法进行对比试验，最终确定单一磁选方法较为适宜。     

A捕收剂在磷矿石浮选中优缺点性能研究和改进措施探索

通过对一些难选磷矿石系统的浮选试验研究发现:A捕收剂作为一种不饱和脂肪酸,可以取代或者部分取代AW、阜新皂等其它浮选捕收剂;另外,当A捕收剂与表面活性剂组成脂肪酸类混合型捕收剂时,可改善A捕收剂的浮选性能,并取得了较好的试验结果。     

贵港含金银多金属硫化矿床矿物特征及选矿试验

广西贵港含金银多金属硫化矿区属中温热液型矿床。根据其工艺矿物学研究特征 ,采用“优先浮选”的工艺流程 ,试验获得了满意的指标 ,金、银分别富集于砷硫精矿、铅精矿中。金、银总回收率均大于 85 %。     

反浮选-冷结晶法生产氯化钾相图分析

察尔汗盐湖是我国最大的可溶性钾镁盐矿床,以相图理论为依据,介绍了反浮选—冷结晶法从含钠光卤石制取氯化钾的相图分析。     

Simultaneous optimization of the performance of flotation circuits and their simplification using the jumping gene adaptations of genetic algorithm-II: More complex problems

The binary-coded elitist non-dominated sorting genetic algorithm with the modified jumping gene operator (NSGA-II-mJG) is used to obtain global optimal solutions of flotation circuits. Several single-objective and multi-objective optimization problems are solved using the interconnecting cell linkage parameters (fraction flow rates) and the mean cell residence times as the decision variables. In the single-objective problem, the overall recovery of the concentrate stream is maximized for a desired grade of the concentrate. Two two-objective optimization problems are then solved. In one, the number of non-linking streams and the overall recovery of the concentrate are maximized simultaneously. This gives several simple circuits in a systematic manner with only marginally lower recoveries. In the other two-objective optimization problem, the overall recovery of the concentrate is maximized while the total cell volume is minimized. A three-objective problem (maximization of the overall recovery of the concentrate, maximization of the number of non-linking streams and minimization of the total cell volume) is then solved. All the problems constrain the grade of the product to lie at a fixed value. Finally, a complex and computationally intensive four-objective optimization problem is solved. The solution of several practical optimization problems in this study helps develop useful insights into the optimal solutions.     

Mechanism of Crystal Redistribution in a Sheet-like Magma Body: Constraints from the Nosappumisaki and Other Shoshonite Intrusions in the Nemuro Peninsula, Northern Japan

Processes of crystal separation in a magma heavily laden withcrystals without phase change are investigated from observationson frozen magma systems: Nosappumisaki and other shoshoniteintrusions in the Nemuro peninsula, Japan, for which the originof the crystals and the initial conditions are well constrained.The Nosappumisaki intrusion is 120 m in thickness and extendsfor more than 1·5 km. It exhibits a wide range of lithologicalvariation, principally as a result of crystal redistributionafter intrusion. Crystals in each lithology can be clearly dividedinto two kinds according to their composition and texture: thosepresent before the intrusion of the magma (‘phenocrysts’)and those that crystallized in situ after intrusion. From thevertical change in mode and size of ‘phenocrysts’,it is shown that (1) augite ‘phenocrysts’ were rapidlydeposited, with little overgrowth after intrusion, by significantcoagulation or clustering on a time-scale of more than a fewyears, and (2) plagioclase ‘phenocrysts’, definitelydenser than the melt but concentrated in the upper level, floatedby counter flow of massive deposition of augite ‘phenocrysts’.These results indicate that in a magma heavily laden with crystalsof a few millimeters in size (>20 vol. %), crystal–crystaland crystal–melt interaction play an important role inthe separation of crystals from the host melt. KEY WORDS: magma chamber; sill; crystal settling; plagioclase flotation; Nosappumisaki