天然磁铁矿处理含Hg(Ⅱ)废水实验研究
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P578. 4+ 6;X703. 1

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国家自然科学基金资助项目(49972017)


The Disposal of Hg(II)-bearing Wastewater by Natural Mangnetite
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    摘要:

    利用重金属离子可在水合金属氧化物和氢氧化物矿物表面产生吸陵作用的原理,进行了天然磁铁矿处理含Hg(Ⅱ)废水的实验研究,结果表明:当温度为25℃,吸附平衡时间为60分钟、试样用量为20g/L,试样粒径为200目以下、pH值为6.40,离子强度为零时,Hg(Ⅱ)初始浓度为1.12mg/L的溶液的吸附率可达98%,使废水中Hg(Ⅱ)的浓度达到国家排放标准。pH值、离子强度、粒径、试样用量、废水浓度、温度、时间均对Hg(Ⅱ)的吸附率有一定的影响,其中pH值的影响最大,Hg(Ⅱ)在天然磁铁矿上的吸附等温曲线不同于Langmuir和Freundlich等温曲线,而是表现为台阶段,符合分级离子/配位子交换等温曲线。

    Abstract:

    The main influencing factors and isotherm adsorption in the treatment of Hg(Ⅱ)-bearing wastewater by using natural magnetite were studied on the basis of the theory of adsorbing heavy metal ions on the surface of water-metal oxides and hydroxides. The results show that the disposal can attain 98% when temperature is 25℃, time is 60min, quantity is 20 g/L, pH is 6.40, grain size is smaller than 200 mesh, ionic strength is zero and Hg(Ⅱ) concentration is 1.12 mg/L and that such factors as pH, ionic strength, quantity, Hg(Ⅱ) concentration, grain size, temperature and time exert different degrees of influence on the disposal, of which the influence of pH is the strongest. The research indicates for the first time that the adsorption isotherm of Hg(Ⅱ) on natural magnetite does not show Langmuir and Freundlich isotherm, but assumes plateau isotherm, which is consistent with the isotherm stepwise ion/coordination particle exchange.

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赵 谨,鲁安怀,姜 浩,等, 2001. 天然磁铁矿处理含Hg(Ⅱ)废水实验研究[J]. 岩石矿物学杂志, 20(4):549~554.
ZHAO Jin, LU An-huai, JIANG Hao, et al, 2001. The Disposal of Hg(II)-bearing Wastewater by Natural Mangnetite[J]. Acta Petrologica et Mineralogica, 20(4): 549~554.

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  • 最后修改日期:2001-06-07
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