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Removal of Cr(VI) from Aqueous Solution by Baritite Clay Adsorption

机译:重晶石粘土吸附去除水溶液中的六价铬

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摘要

Among the investigated clays and minerals (kaolinite, natural zeolite, manual zeolite, bentonite, sepiolite, sepiolite amianthus, tremolite arnianthus, vermiculite and baritite), the baritite clay was selected as the optimal adsorbent for aqueous Cr(VI). The adsorption capacity of Cr(VI) on baritite clay reached as high as 39.01 mg g"' at 20 °C. Then the adsorption kinetics and thermodynamics of Cr(VI) by the baritite clay were studied. Results showed that the pseudo-second-order model was a suitable description for the adsorption kinetics and fitted well with the experimental data. The calculated values of entropy (ΔS°) and enthalpy (AH0) changes of the adsorption process were ΔH° =-9.653 kJ/mol and ΔS° =-22.57 J mol~(-1) K~(-1). This indicated that the adsorption of Cr(VI) on baritite clay was an exothermic process with chemical reactions. Finally, a hypothetical chemical adsorption mechanism of Cr(VT) was proposed.
机译:在所研究的粘土和矿物中(高岭石,天然沸石,手工沸石,膨润土,海泡石,海泡石白石,透闪石蜡菊、,石和重晶石),重晶石粘土被选作Cr(VI)水溶液的最佳吸附剂。在20°C下,Cr(VI)在重晶石粘土上的吸附能力高达39.01 mg g“'。然后研究了重晶石粘土对Cr(VI)的吸附动力学和热力学。序模型是吸附动力学的一个合适描述,并与实验数据吻合良好,吸附过程的熵(ΔS°)和焓(AH0)变化的计算值为ΔH°= -9.653 kJ / mol和ΔS° = -22.57 J mol〜(-1)K〜(-1),这表明Cr(VI)在重晶石粘土上的吸附是一个伴随化学反应的放热过程,最后给出了Cr(VT)的假想化学吸附机理。被提出。

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