精喹禾灵在高岭土和蒙脱石中的吸附行为

丁春霞, 龚道新, 肖浩, 任颖俊, 杨丽华. 精喹禾灵在高岭土和蒙脱石中的吸附行为[J]. 环境化学, 2013, 32(6): 1067-1072. doi: 10.7524/j.issn.0254-6108.2013.06.023
引用本文: 丁春霞, 龚道新, 肖浩, 任颖俊, 杨丽华. 精喹禾灵在高岭土和蒙脱石中的吸附行为[J]. 环境化学, 2013, 32(6): 1067-1072. doi: 10.7524/j.issn.0254-6108.2013.06.023
DING Chunxia, GONG Daoxin, XIAO Hao, REN Yingjun, YANG Lihua. Adsorption of quizalop-p-ethyl on montmorillonite and kaolinite[J]. Environmental Chemistry, 2013, 32(6): 1067-1072. doi: 10.7524/j.issn.0254-6108.2013.06.023
Citation: DING Chunxia, GONG Daoxin, XIAO Hao, REN Yingjun, YANG Lihua. Adsorption of quizalop-p-ethyl on montmorillonite and kaolinite[J]. Environmental Chemistry, 2013, 32(6): 1067-1072. doi: 10.7524/j.issn.0254-6108.2013.06.023

精喹禾灵在高岭土和蒙脱石中的吸附行为

  • 基金项目:

    农业部农药残留试验基金项目(2010H216)资助.

Adsorption of quizalop-p-ethyl on montmorillonite and kaolinite

  • Fund Project:
  • 摘要: 采用批量平衡实验,研究了精喹禾灵在蒙脱石和高岭土中的吸附行为及作用机理.结果表明,精喹禾灵在这两种供试黏土矿物中的吸附过程分为快速吸附、慢速吸附和吸附平衡3个阶段,吸附平衡时间都约为12 h;Langmuir模型能较好地描述其在两种供试黏土矿物中的吸附行为;蒙脱石和高岭土对精喹禾灵的最大吸附容量的关系为蒙脱石>高岭土;傅立叶变换红外光谱以及X-射线衍射分析显示,在吸附过程中精喹禾灵分子进入了蒙脱石层间,而未进入到高岭土层间;蒙脱石主要是通过其层间结构对精喹禾灵进行吸附,而高岭土则主要是通过硅氧外表面发生吸附,其吸附作用力主要是氢键.
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  • 收稿日期:  2012-09-06
丁春霞, 龚道新, 肖浩, 任颖俊, 杨丽华. 精喹禾灵在高岭土和蒙脱石中的吸附行为[J]. 环境化学, 2013, 32(6): 1067-1072. doi: 10.7524/j.issn.0254-6108.2013.06.023
引用本文: 丁春霞, 龚道新, 肖浩, 任颖俊, 杨丽华. 精喹禾灵在高岭土和蒙脱石中的吸附行为[J]. 环境化学, 2013, 32(6): 1067-1072. doi: 10.7524/j.issn.0254-6108.2013.06.023
DING Chunxia, GONG Daoxin, XIAO Hao, REN Yingjun, YANG Lihua. Adsorption of quizalop-p-ethyl on montmorillonite and kaolinite[J]. Environmental Chemistry, 2013, 32(6): 1067-1072. doi: 10.7524/j.issn.0254-6108.2013.06.023
Citation: DING Chunxia, GONG Daoxin, XIAO Hao, REN Yingjun, YANG Lihua. Adsorption of quizalop-p-ethyl on montmorillonite and kaolinite[J]. Environmental Chemistry, 2013, 32(6): 1067-1072. doi: 10.7524/j.issn.0254-6108.2013.06.023

精喹禾灵在高岭土和蒙脱石中的吸附行为

  • 1.  湖南农业大学理学院, 长沙, 410128;
  • 2.  湖南农业大学资源环境学院, 长沙, 410128;
  • 3.  湖南农业大学农业环境保护研究所, 长沙, 410128
基金项目:

农业部农药残留试验基金项目(2010H216)资助.

摘要: 采用批量平衡实验,研究了精喹禾灵在蒙脱石和高岭土中的吸附行为及作用机理.结果表明,精喹禾灵在这两种供试黏土矿物中的吸附过程分为快速吸附、慢速吸附和吸附平衡3个阶段,吸附平衡时间都约为12 h;Langmuir模型能较好地描述其在两种供试黏土矿物中的吸附行为;蒙脱石和高岭土对精喹禾灵的最大吸附容量的关系为蒙脱石>高岭土;傅立叶变换红外光谱以及X-射线衍射分析显示,在吸附过程中精喹禾灵分子进入了蒙脱石层间,而未进入到高岭土层间;蒙脱石主要是通过其层间结构对精喹禾灵进行吸附,而高岭土则主要是通过硅氧外表面发生吸附,其吸附作用力主要是氢键.

English Abstract

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