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Adsorption of Divalent Metal Ions on a Herbaceous Peat

机译:草本泥炭对二价金属离子的吸附

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摘要

This study was performed to determine divalent metal ion [Cu(II),Zn(II),Mn(II)and Ni(II)] adsorption characteristics of the herbaceous peat of the Gavur Lake,Turkey.The adsorption data of the metal ions were fitted to both the Langmuir and the Freundlich isotherms.The adsorption capacity of the peat was much higher for Cu(38.5 mg g~(-1))compared with Zn(28.0 mg g~(-1)),Mn(26.4 mg g~(-1))and Ni(24.1 mg g~(-1)).A steady increase in equilibrium Ca and Mg ion concentrations were measured as initial metal ion concentrations increased from 1 X 10"3 M to 5 X 10~(-3)M in Cu and Zn adsorption experiments indicating that ion exchange was an important mechanism in the adsorption.The kinetic study revealed that the adsorption followed the pseudo-second-order model and the interaction between the metal ions and the peat was very fast,especially for Cu.The pH study revealed that Cu adsorption was not affected in the pH range between 3 and 5,but the adsorption of Zn,Mn and Ni was lower at pH 3 compared with pH 4 and 5.
机译:进行了这项研究,以确定土耳其加夫湖的草炭泥炭的二价金属离子[Cu(II),Zn(II),Mn(II)和Ni(II)]的吸附特性。金属离子的吸附数据泥炭对Cu(38.5 mg g〜(-1)),Zn(28.0 mg g〜(-1)),Mn(26.4 mg)的吸附能力要高得多。 g〜(-1))和Ni(24.1 mg g〜(-1))。随着初始金属离子浓度从1 X 10“ 3 M增加到5 X 10〜 (-3)M在铜和锌的吸附实验中表明离子交换是吸附的重要机理。动力学研究表明,吸附遵循伪二级模型,金属离子与泥炭之间的相互作用非常强。 pH研究表明,在3至5的pH范围内,Cu的吸附不受影响,但在pH 3时,Zn,Mn和Ni的吸附较低用pH 4和5。

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