首页|钙镁离子对白云石浮选矿浆流变性的影响研究

钙镁离子对白云石浮选矿浆流变性的影响研究

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磷矿反浮选脱镁过程中,白云石溶解和回水循环利用导致矿浆中钙镁离子增多,影响白云石的浮选行为,进而影响磷灰石与含钙脉石矿物的分离,因此调控含钙脉石矿物浮选行为的研究是磷矿石分选的研究热点.本研究以常见的含钙脉石矿物——白云石为对象,在不同钙离子和镁离子浓度下进行单矿物浮选试验、矿物颗粒分布和矿浆黏度测试,分析了钙离子和镁离子对白云石浮选流变性的影响,结果表明:弱酸性条件下,钙镁离子在改变矿浆黏度的同时也能影响浮选结果;钙离子对白云石有一定抑制作用,随着钙离子浓度升高,白云石上浮率先降低后有一定程度的上升,矿浆黏度则表现出先上升后下降的趋势;镁离子可以活化白云石上浮,随着镁离子浓度升高,白云石的上浮率先增加后趋于稳定,矿浆黏度表现出先下降后稳定的趋势.
Effect of calcium and magnesium ions on the rheological characteristics of dolo-mite pulp
In the process of removing magnesium from phosphate rock through reverse flotation,the dissolution of dolomite and the recycling of backwater would lead to the increase of calcium and magnesium ions in the pulp.This study took dolomite as the research object,and carried out single mineral flotation test,mineral particle distribution test,and pulp viscosity test under different concentrations of Ca2+and Mg2+.The results were as follows:under weak acidic conditions,Ca2+and Mg2+would affect the flotation results while changing the viscosity of the pulp;Ca2+had a certain inhibitory effect on the dolomite;with the increase of Ca2+concentration,the floating rate of dolomite de-creased first and then increased,while the viscosity of the pulp increased first and then decreased;Mg2+would acti-vate the dolomite;with the increase of Mg2+concentration,the floating rate of dolomite increased first and then re-mained stable,while the viscosity of the pulp decreased first and then remained stable.

dolomitefine particlescalcium and magnesium ionsrheological characteristics of pulp

章铁斌、刘文宝、张覃

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贵州大学 资源与环境工程学院,贵州 贵阳 550025

喀斯特地区优势矿产资源高效利用国家地方联合工程实验室,贵州 贵阳 550025

贵州省非金属矿产资源综合利用重点实验室,贵州 贵阳 550025

贵州科学院,贵州 贵阳 550001

东北大学 资源与土木工程学院,辽宁 沈阳 110819

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白云石 微细粒 钙镁离子 矿浆流变性

国家自然科学基金

52164018

2024

贵州科学
贵州科学院

贵州科学

影响因子:0.395
ISSN:1003-6563
年,卷(期):2024.42(2)
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