伊利石和高岭石对U(Ⅵ)的吸附

    Adsorption of Illite and Kaolinite for U(Ⅵ)

    • 摘要: 以伊利石和高岭石为吸附剂,通过静态吸附法研究了其对U(Ⅵ)的吸附特性。考察了接触时间、初始浓度、吸附剂质量、pH、温度、离子种类、腐殖酸等对其吸附效果的影响;采用红外光谱(FTIR) 对伊利石和高岭石的结构进行了表征。研究结果表明:伊利石和高岭石对U(Ⅵ)具有很强的吸附能力,在10 h、铀初始质量浓度为30 mg/L、吸附剂质量为0.04 g、pH=5的条件下,伊利石对U(Ⅵ)的吸附效果最好;在12 h、铀初始质量浓度为30 mg/L、吸附剂质量为0.01 g、pH=5的条件下,高岭石对U(Ⅵ)的吸附效果最好;随着温度的升高,伊利石和高岭石对U(Ⅵ)的吸附能力不断增强,尤其是伊利石;溶液中Mg2+、CO2-3、HCO-3显著降低了伊利石和高岭石对U(Ⅵ)的吸附效果;随着腐殖酸浓度的增加,伊利石对U(Ⅵ)的吸附能力提高,高岭石对U(Ⅵ)的吸附能力降低。

       

      Abstract: The adsorption behavior of U(Ⅵ) on illite and kaolinite was studied as a function of adsorption time, initial concentration of U(Ⅵ), adsorbent mass, pH, temperature, the type of ionic species and humic acid by the static experimental method; the structure of the illite- and kaolinite were characterized by FTIR. The experimental results display that the illite have the best adsorption effect on U(Ⅵ) at the initial mass concentration of 30 mg/L, adsorbent mass of 0.04 g, 10 h and pH=5; the kaolinite have the best adsorption effect on U(Ⅵ) at the initial mass concentration of 30 mg/L, adsorbent mass of 0.01 g, 12 h and pH=5; the adsorption capacity of illite and kaolinite is enlarged with the increasing of temperature, especially illite. Mg2+, CO2-3 and HCO-3 in solution significantly reduce the adsorption of U(Ⅵ) by illite and kaolinite; with the increase of humic acid, the adsorption capacity of illite improves, but the adsorption capacity of kaolinite decreases.

       

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