黄书鑫, 冯健, 刘杰泉, 余军霞, 池汝安. 黏土矿物对风化壳淋积型稀土矿浸矿剂中NH4+的吸附和脱附特性研究[J]. 中国矿业, 2021, 30(6): 152-158. DOI: 10.12075/j.issn.1004-4051.2021.06.009
    引用本文: 黄书鑫, 冯健, 刘杰泉, 余军霞, 池汝安. 黏土矿物对风化壳淋积型稀土矿浸矿剂中NH4+的吸附和脱附特性研究[J]. 中国矿业, 2021, 30(6): 152-158. DOI: 10.12075/j.issn.1004-4051.2021.06.009
    HUANG Shuxin, FENG Jian, LIU Jiequan, YU Junxia, CHI Ru'an. Adsorption and desorption characteristics of clay minerals on NH4+ in the leaching agent of weathered crust elution-deposited rare earth ore[J]. CHINA MINING MAGAZINE, 2021, 30(6): 152-158. DOI: 10.12075/j.issn.1004-4051.2021.06.009
    Citation: HUANG Shuxin, FENG Jian, LIU Jiequan, YU Junxia, CHI Ru'an. Adsorption and desorption characteristics of clay minerals on NH4+ in the leaching agent of weathered crust elution-deposited rare earth ore[J]. CHINA MINING MAGAZINE, 2021, 30(6): 152-158. DOI: 10.12075/j.issn.1004-4051.2021.06.009

    黏土矿物对风化壳淋积型稀土矿浸矿剂中NH4+的吸附和脱附特性研究

    Adsorption and desorption characteristics of clay minerals on NH4+ in the leaching agent of weathered crust elution-deposited rare earth ore

    • 摘要: 为了消除风化壳淋积型稀土矿中残留浸矿剂所导致的环境污染问题,本文研究了风化壳淋积型稀土矿中主要黏土矿物蒙脱土、高岭土和伊利石对稀土浸矿剂中NH4+的吸附和脱附行为和机理,并采用纳氏比色-分光光度法对NH4+进行测定。结果表明,蒙脱土、高岭土和伊利石对NH4+的吸附为单分子层吸附,符合Langmuir模型,且NH4+的最大吸附量分别为5.99 mg/g、0.12 mg/g、1.10 mg/g,风化壳淋积型稀土矿中NH4+的释放源主要来自于蒙脱土和伊利石。解吸附实验结果表明金属离子和去离子水对NH4+的解吸附能力遵循Fe3+≈Al3+≥Mg2+>Ca2+>K+>Na+>H2O。镁盐解吸附实验结果表明其对黏土矿物上NH4+的解吸附速度快,解吸附率高,同等条件下其对风化壳淋积型稀土矿中残留NH4+的洗脱率大于95%。

       

      Abstract: In order to eliminate the environmental pollution caused by the residual leaching agent in the weathered crust elution-deposited rare earth ore, the adsorption and desorption characteristics of montmorillonite, kaolinite and illite on NH4+ in the leaching agent of weathered crust elution-deposited rare earth ore are investigated, and concentration of ammonium ion is determined by Nessler colorimetric-spectrophotometry in this paper.The results show that adsorption isotherms of ammonium on the three clay minerals are a mono-layer sorption and fitted well to Langmuir model.Maximum adsorption capacity of montmorillonite, kaolinite and illite on NH4+ is 5.99 mg/g, 0.12 mg/g and 1.10 mg/g, and release source of NH4+ is mainly from montmorillonite and illite.Desorption results show that efficiency of the eluate followed the order, Fe3+≈Al3+ ≥ Mg2+>Ca2+>K+>Na+>H2O.Experimental results show that the NH4+ desorption by magnesium salt is the fast process with high efficiency.Under the same conditions, the elution rate of residual NH4+ in weathering crust eluvial rare earth ore is more than 95%.

       

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