| 粘土矿吸附过程中四环素基团变化研究 |
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| 引用本文： | 张志旭,吴根义,许振成.粘土矿吸附过程中四环素基团变化研究[J].农业环境科学学报,2017,34(2):115-120. |
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| 作者姓名： | 张志旭 吴根义 许振成 |
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| 作者单位： | 湖南农业大学资源环境学院, 湖南 长沙, 410128;湖南植物功能成分利用协同创新中心, 湖南 长沙, 410128;国家中医药管理局亚健康干预技术实验室, 湖南 长沙, 410128,湖南农业大学资源环境学院, 湖南 长沙, 410128,湖南农业大学资源环境学院, 湖南 长沙, 410128;环保部华南环境科学研究所, 广东 广州, 510655 |
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| 基金项目： | 环境保护部公益性科研专项“畜禽养殖污染负荷模拟估算技术与实证研究”（201509038） |
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| 摘 要： | 湖南红壤主要由富含硅铝的高岭土和蒙脱石组成，选取这两种粘土矿作为吸附介质在实验室环境下模拟了四环素的吸附过程，通过高效液相色谱和红外光谱检测分析了四环素的主要基团在不同吸附阶段的变化，结果表明-OH是影响吸附速率和吸附量的主要基团，发生的吸附在解吸过程中也难于解吸；C=O主要在吸附后期起作用，吸附能力不强，易解吸，可能与其吸电子能力较弱有关。
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| 关 键 词： | 四环素，粘土矿，红外光谱，吸附 |
| 收稿时间： | 2016/9/6 0:00:00 |
Functional Groups' Variation of Tetracycline in the Process of Adsorption in Clay Minerals |
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| ZHANG Zhi-xu,WU Gen-yi and XU Zhen-cheng.Functional Groups'' Variation of Tetracycline in the Process of Adsorption in Clay Minerals[J].Journal of Agro-Environment Science( J. Agro-Environ. Sci.),2017,34(2):115-120. |
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| Authors: | ZHANG Zhi-xu WU Gen-yi and XU Zhen-cheng |
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| Institution: | College of Resources & Environment, Hunan Agricultural University, Changsha 410128, China;Hunan Co-Innovation Center for Utilization of Botanical Functional Ingredients, Changsha 410128, China;State Key Laboratory of Sub-health Intervention Technology, Changsha 410128, China,College of Resources & Environment, Hunan Agricultural University, Changsha 410128, China and College of Resources & Environment, Hunan Agricultural University, Changsha 410128, China;South China Institute of Environmental Sciences, MEP, Guangzhou 510655, China |
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| Abstract: | Red soil in Hunan Province is consist of Kaolin & Montmorillonite, 2 kinds of typical clay minerals rich in Si&Al. We conducted experiments on the tetracycline (TC) adsorption in the laboratory by selecting the clay minerals above as adsorptive medium, monitored and meseasured by HPLC and FTIR. The variation of main groups of TC were exhibted in different adsorption phases. Results showed that-OH was the main group which affected adsorption rate and adsorption capacity, the adsorption with-OH was hard to be desorbed once it was formed. C=O had its'' effect in the later adsorption phase, but the adsorption ability was weak and the adsorption was easily desorbed. It was likely related to the weaker electrophilic ability. |
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| Keywords: | tetracycline clay mineral fourier transform infrared spectroscopy adsorption |
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