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法库沸石对氨氮的吸附特性和阳离子交互过程
引用本文:李圣品, 刘菲, 陈鸿汉, 李梦姣. 法库沸石对氨氮的吸附特性和阳离子交互过程[J]. 环境工程学报, 2015, 9(1): 157-163. doi: 10.12030/j.cjee.20150126
作者姓名:李圣品  刘菲  陈鸿汉  李梦姣
作者单位:1.中国地质大学(北京) 水资源与环境工程北京市重点实验室, 北京 100083
基金项目:国家"水体污染控制与治理"科技重大专项(2009ZX07-424002-002)
摘    要:以0.9~2 mm和3.3~4 mm粒径沸石的天然法库沸石作为实验材料,开展了等温吸附实验、动力学实验和阳离子影响实验,探讨了天然沸石对氨氮(NH4+-N)的吸附特性及阳离子交互过程。结果表明,法库沸石对NH4+-N等温吸附线符合Langmuir和Freundlich吸附方程,最大吸附量为10.41 mg/g。吸附动力学过程符合准二级和颗粒内经扩散动力学方程,其吸附NH4+过程为物理吸附和化学吸附过程,并以化学吸附为主。对反应过程中各离子浓度监测发现,沸石中与NH4+发生离子交换的主要是Na+、Ca2+和K+,三者占离子交换总量的99%。共存阳离子在沸石吸附NH4+过程中,Ca2+和Mg2+对吸附过程影响最大,Na+影响最小。

关 键 词:法库沸石   吸附等温线   吸附动力学   离子交换
收稿时间:2014-02-16

Adsorption characters of ammonium by Faku zeolite and cation exchanges in ammonium removal process
Li Shengpin, Liu Fei, Chen Honghan, Li Mengjiao. Adsorption characters of ammonium by Faku zeolite and cation exchanges in ammonium removal process[J]. Chinese Journal of Environmental Engineering, 2015, 9(1): 157-163. doi: 10.12030/j.cjee.20150126
Authors:Li Shengpin  Liu Fei  Chen Honghan  Li Mengjiao
Affiliation:1.Beijing Key Laboratory of Water Resources and Environmental Engineering, China University of Geosciences (Beijing), Beijing 100083, China
Abstract:To study the characters and cation exchange processes of the adsorbed NH4+ into zeolite, Faku natural zeolite (0.9~2 mm and 3.3~4 mm) was selected as experiment material. According to the designed purpose, an isotherm adsorption experiment, an adsorption kinetics experiment and a cation influencing experiment were conducted, respectively. The results showed that in the isotherm adsorption experiment, the NH4+ into Faku zeolite demonstrated a good fit of Langmuir and Freundlich models, and the maximun adsorption capacity of NH4+ was 10.41mg/g. In the adsorption kinetics experiment, the NH4+ adsorption data were successfully described by the pseudo second-order kinetic model and the intraparticle diffusion equation, suggesting that the process of NH4+ into the Faku zeolite was both a physical and a chemical adsorption processes, and the latter played a dominant role. Based on the data obtained from the cation influencing experiment, the main exchange cations by NH4+ were Na+ , Ca2+ and K+, accounting for about 99% of the total exchange amount. Among the coexistent cations (K+, Na+, Ca2+, Mg2+), Ca2+ and Mg2+ showed a significant effect on NH4+ removal by zeolite, while Na+ exhibited a minimum effect on NH4+ removal.
Keywords:Faku zeolite  isotherm  kinetic model  ion exchange
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