离子交换在膨润土吸附Sr2+中的作用

IF 1.6 3区 化学 Q3 CHEMISTRY, ANALYTICAL
Jingru Ji, Weiyun Liang, Rongtao Yan, Jiaying Ji, Qin Zhang
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引用次数: 0

摘要

本研究考察了GMZ膨润土对Sr2+的吸附行为,考虑了时间和初始浓度的影响,并量化了离子交换的贡献。结果表明,Sr2+吸附在48 h内达到平衡,随着Sr2+初始浓度的增加,吸附量增加,吸附速率下降。同时,离子交换吸附容量增大,在高浓度下达到平稳期,离子交换吸附比从95.7%下降到68.8%。吸附过程受离子交换控制。当离子交换位点饱和时,发生多层吸附,表面或边缘相互作用变得重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Role of ion exchange in the adsorption of Sr2+ by bentonite

Role of ion exchange in the adsorption of Sr2+ by bentonite

Role of ion exchange in the adsorption of Sr2+ by bentonite

This study investigated the adsorption behaviour of Sr2+ by GMZ bentonite, considering the effects of time and initial concentration, and quantified the ion exchange contribution. Results showed that Sr2+ adsorption reached equilibrium within 48 h. As the initial Sr2+ concentration increased, the adsorption capacity increased, whereas the adsorption rate declined. Meanwhile, the ion exchange adsorption capacity increased and reached a plateau at high concentrations, while the ion exchange adsorption ratio decreased from 95.7% to 68.8%. Sorption process is governed by ion exchange. As ion exchange sites saturate, multilayer adsorption occurs and surface or edge interactions become significant.

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来源期刊
CiteScore
2.80
自引率
18.80%
发文量
504
审稿时长
2.2 months
期刊介绍: An international periodical publishing original papers, letters, review papers and short communications on nuclear chemistry. The subjects covered include: Nuclear chemistry, Radiochemistry, Radiation chemistry, Radiobiological chemistry, Environmental radiochemistry, Production and control of radioisotopes and labelled compounds, Nuclear power plant chemistry, Nuclear fuel chemistry, Radioanalytical chemistry, Radiation detection and measurement, Nuclear instrumentation and automation, etc.
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