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沸石和膨润土对三价铁的吸附特性研究。

Characterization of Fe(III) Adsorption onto Zeolite and Bentonite.

机构信息

Faculty of Mining, Ecology, Process Control and Geotechnologies, Technical University of Košice, 04200 Košice, Slovakia.

Institute of Hygiene of Animals and Environment, University of Veterinary Medicine and Pharmacy in Košice, 041 81 Košice, Slovakia.

出版信息

Int J Environ Res Public Health. 2020 Aug 7;17(16):5718. doi: 10.3390/ijerph17165718.

Abstract

In this study, the adsorption of Fe(III) from aqueous solution on zeolite and bentonite was investigated by combining batch adsorption technique, Atomic adsorption spectroscopy, X-ray diffraction, and X-ray photoelectron spectroscopy analyses. Although iron is commonly found in water and is an essential bioelement, many industrial processes require efficient removal of iron from water. Two types of zeolite and two types of bentonite were used. The results showed that the maximum adsorption capacities for removal of Fe (III) by Zeolite Micro 20, Zeolite Micro 50, blue bentonite, and brown bentonite were 10.19, 9.73, 11.64, and 16.65 mg.g, respectively. Based on the X-ray photoelectron spectroscopy (XPS) and X-ray fluorescence (XRF) analyses of the raw samples and the solid residues after sorption at low and high initial Fe concentrations, the Fe content is different in the surface layer and in the bulk of the material. In the case of lower initial Fe concentration (200 mg.dm), more than 95% of Fe is adsorbed in the surface layer. In the case of higher initial Fe concentration (4000 mg.dm), only about 45% and 61% of Fe is adsorbent in the surface layer of zeolite and bentonite, respectively; the rest is adsorbed in deeper layers.

摘要

在这项研究中,通过结合批量吸附技术、原子吸收光谱分析、X 射线衍射和 X 射线光电子能谱分析,研究了沸石和膨润土从水溶液中吸附 Fe(III)的情况。尽管铁在水中普遍存在,是一种必需的生物元素,但许多工业过程都需要有效地从水中去除铁。使用了两种类型的沸石和两种类型的膨润土。结果表明,沸石 Micro 20、沸石 Micro 50、蓝膨润土和棕膨润土对 Fe(III)的最大吸附容量分别为 10.19、9.73、11.64 和 16.65mg.g。基于对原始样品和在低初始 Fe 浓度和高初始 Fe 浓度下吸附后的固体残留物的 X 射线光电子能谱 (XPS) 和 X 射线荧光 (XRF) 分析,Fe 在材料的表面层和体相中的含量不同。在较低的初始 Fe 浓度 (200mg.dm) 下,超过 95%的 Fe 被吸附在表面层。在较高的初始 Fe 浓度 (4000mg.dm) 下,沸石和膨润土的表面层分别只有约 45%和 61%的 Fe 被吸附,其余的则被吸附在更深的层中。

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