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首页> 外文期刊>International Journal of Mineral Processing >2+, Mg 2+ and Zn 2+ on the flotation and surface charge of smithsonite and dolomite with sodium oleate and sodium silicate]]>
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2+, Mg 2+ and Zn 2+ on the flotation and surface charge of smithsonite and dolomite with sodium oleate and sodium silicate]]>

机译:<![cdata [cdata ca 2 + ,mg 2 + 和zn < CE:Sup =“POST”> 2 + 在炉山铁矿石和白云岩的浮选和表面电荷上用钠酸钠和硅酸钠]]]>

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AbstractThis study aimed to determine the conditions required for selective flotation between smithsonite and dolomite using sodium oleate and sodium silicate. Microflotation test results demonstrated recoveries of 95% and 5% for smithsonite and dolomite, respectively, from 2.5×10?5M sodium oleate and 50mg/L sodium silicate at pH9.5. The smithsonite was depressed by the cations Ca2+and Mg2+and, the dolomite was depressed by Zn2+cations, which was probably caused by the reaction of these cations with the oleate anions in the solution, decreasing the concentration of collector available for adsorption onto the minerals. The powerful depression of smithsonite caused by Ca2+cations compared with that caused by Mg2+cations can be considered to have occurred because of the higher concentration of Ca2+in the solution. From the zeta potential measurements at pH9.5, we concluded that the predominant species of oleate and of sodium silicate were adsorbed onto both minerals, and the silicate species prevented the adsorption of oleate anions onto dolomite. The decrease in the negative zeta potential of both minerals after cation conditioning can be related to the electrostatic attraction between the cations and the negative sites on their surfaces. The negative zeta potential of smithsonite increased at a concentration of 1×10?6M Ca2+and Mg2+, whereas the potential decreases at a concentration of 1×10?3M, which can be related to a lower concentration of oleate anions being available for adsorption.Highlights?Sodium oleate had a higher affinity for smithsonite than dolomite at pH9.5.?Sodium silicate is stronger depressant for dolomite compared with smithsonite.?The ion Ca2+at pH9.5 was more effective in smithsonite depression than Mg2+and MgOH+.?There is competition of Ca2+in solution with oleate and surfaces of smithsonite and dolomite.?Selective separation between smithsonite and dolomite is possible up 1.0×10?6M of ions Ca2+and Mg2+.]]>
机译:<![cdata [ 抽象 本研究旨在确定使用钠和硅酸钠和硅酸钠之间的透石质和白云石之间的选择性浮选所需的条件。微型透明试验结果分别显示出炉霉铁和白云岩的95%和5%的回收率,从2.5×10 α5 m钠olate和50mg / l硅酸钠PH9.5。阳离子CA 2 + 和mg 2 + 和白云石由Zn 2 + 阳离子,这可能是由这些阳离子与溶液中的果糕阴离子的反应引起的,降低可用于吸附的收集器的浓度到矿物质上。由CA 2 + 阳离子的强大凹陷与MG 2 + 可以考虑阳离子发生,因为CA 2 + 中的浓度较高。从PH9.5的Zeta电位测量中,我们得出结论,将乳酸钠和硅酸钠的主要物种吸附在两种矿物上,硅酸盐物质预防果酸盐阴离子在白云岩上吸附。阳离子调理后两种矿物质的阴性ζ电位的降低可以与它们表面上的阳离子和阴性位点之间的静电吸引有关。史密森矿的负Zeta电位以1×10 α6 m ca 2 + 和mg 2 + ,而浓度为1×10 3 m,其可以与可用于吸附的较低浓度的含油阴离子有关。 亮点 < CE:简单段ID =“SP0070”View =“全部”> 钠油钠对pH9.5的白云岩具有比白云石更高的亲和力。 与史森矿石相比,硅酸钠较强抑制抑制剂。 < ce:para id =“p0015”查看=“全部”> ion ca 2 + 在pH9.5中在史密森矿凹陷比mg 2 + 和mgoh + < CE:列表项ID =“li0020”> 有CA 2 + 史密森矿和白云石之间的选择性分离是可能的1.0×10 ?6 < / ce:sup> m oon离子ca 2 + 和mg 2 + ]]>

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