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天然蒙脱石和铝柱撑蒙脱石的胶体性质研究及从水溶液中去除铜离子的研究。

Study of colloidal properties of natural and Al-pillared smectite and removal of copper ions from an aqueous solution.

作者信息

Sartor Lucas Resmini, de Azevedo Antonio Carlos, Andrade Gabriel Ramatis Pugliese

机构信息

a Departamento de Ciência do Solo, Escola Superior de Agricultura "Luiz de Queiroz" , Universidade de São Paulo (ESALQ-USP) , Av. Pádua Dias 11, CP9, CEP 13418-900 , Piracicaba , São Paulo , Brazil.

出版信息

Environ Technol. 2015 Mar-Apr;36(5-8):786-95. doi: 10.1080/09593330.2014.961564. Epub 2014 Oct 9.

Abstract

In this study, an Al-pillared smectite was synthesized and changes in its colloidal properties were investigated. The pillaring solution was prepared by mixing 0.4 mol L(-1) NaOH and 0.2 mol L(-1) AlCl3.6H2O solutions. Intercalated clays were heated to obtain the pillared clay, and X-ray diffractometry (XRD), X-ray fluorescence (XRF), Fourier transform infrared (FTIR) spectroscopy and N2 sorption/desorption isotherms analysis were done to characterize the changes in clay properties. Moreover, adsorption experiments were carried out in order to evaluate the capacity of the pillared clays to remove Cu2+ from an aqueous solution and to characterize the interaction between adsorbent and adsorbate. The results indicate that the natural clay has a basal spacing of 1.26 nm, whereas the pillared clays reached 1.78 nm (500°C) and 1.80 nm (350°C) after calcination. XRF analysis revealed an increase in the Al3+ in the pillared clay as compared to the natural clay. The surface area and pore volume (micro and mesoporous) were higher for the pillared clays. Experimental data from the adsorption experiment were fit to Langmuir and Freundlich and Temkin adsorption models, and the former one was the best fit (highest r2 value) for all the clays and lower standard deviation (Δg%) for the natural clay. On the other hand, the Temkin model exhibited Δg% value lower for the pillared clays. Thermodynamics parameters demonstrate that the Cu2+ adsorption process is spontaneous for all the clays, but with higher values for the pillared materials. In addition, application of the Dubinin-Radushkevich model revealed that the bond between the metal and the clay are weak, characterizing a physisorption.

摘要

在本研究中,合成了一种铝柱撑蒙脱石,并研究了其胶体性质的变化。通过混合0.4 mol L⁻¹的NaOH溶液和0.2 mol L⁻¹的AlCl₃·6H₂O溶液制备柱撑溶液。将插层粘土加热以获得柱撑粘土,并进行X射线衍射(XRD)、X射线荧光(XRF)、傅里叶变换红外(FTIR)光谱和N₂吸附/脱附等温线分析,以表征粘土性质的变化。此外,进行了吸附实验,以评估柱撑粘土从水溶液中去除Cu²⁺的能力,并表征吸附剂与吸附质之间的相互作用。结果表明,天然粘土的层间距为1.26 nm,而柱撑粘土在煅烧后分别达到1.78 nm(500°C)和1.80 nm(350°C)。XRF分析表明,与天然粘土相比,柱撑粘土中的Al³⁺含量增加。柱撑粘土的表面积和孔体积(微孔和介孔)更高。吸附实验的实验数据符合朗缪尔、弗伦德利希和坦金吸附模型,其中前者对所有粘土的拟合效果最佳(r²值最高),天然粘土的标准偏差(Δg%)较低。另一方面,坦金模型对柱撑粘土的Δg%值较低。热力学参数表明,所有粘土对Cu²⁺的吸附过程都是自发的,但柱撑材料的值更高。此外,杜宾宁-拉杜什凯维奇模型的应用表明,金属与粘土之间的键较弱,属于物理吸附。

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