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Spectroscopic Study of Carbaryl Sorption on Smectite from Aqueous Suspension

机译:悬浮液中蒙脱石对十八碳烯的吸附光谱研究

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摘要

Sorption of carbaryl(1-naphthyl-N-methyl-carbamate)from aqueous suspension to smectite was studied using Fourier transform infrared(FTIR),high-performance liquid chromatography(HPLC)(for batch sorption),and quantum chemical methods.The amount of carbaryl sorbed was strongly dependent on the surface-charge density of the smectite with more sorption occurring on the two"low"surface-charge density smectites(SHCa-1 and SWy-2)compared to that of the high surface-charge SAz-1 smectite.In addition,the amount of carbaryl sorbed was strongly dependent on the nature of the exchangeable cation and followed the order of Ba approx Cs approx Ca > Mg approx K > Na approx Li for SWy-2.A similar trend was found for hectorite(SHCa-1)of Cs > Ba > Ca > K approx Mg > Na approx Li.Using the shift of the carbonyl stretching band as an indicator of the strength of interaction between carbaryl and the exchangeable cation,the observed order was Mg > Ca > Ba approx K > Na > Cs.The position of the carbonyl stretching band shifted to lower wavenumbers with increasing ionic potential of the exchangeable cation.Density functional theory predicted a cation-induced lengthening of the C=0 bond,resulting from the carbonyl group interacting directly with the exchangeable cation in support of the spectroscopic observations.Further evidence was provided by a concomitant shift in the opposite direction by several vibrational bands in the 1355-1375 cm~(-1)region assigned to stretching bands of the carbamate N-C_(carbonyl)and O_(ether)-C_(Carbonyl)bonds.These data indicate that carbaryl sorption is due,in part,to site-specific interactions between the carbamate functional group and exchangeable cations,as evidenced by the FTIR data.However,these data suggest that hydrophobic interactions also contribute to the overall amount of carbaryl sorbed.For example,the FTIR data indicated that the weakest interaction occurred when Cs~+ was the exchangeable cation.In contrast,the highest amount of carbaryl sorption was observed on Cs-exchanged smectite.Of all the cations studied,Cs has the lowest enthalpy of hydration.It is suggested that this low hydration energy provides the carbaryl with greater access to the hydrophobic regions of the siloxane surface.
机译:采用傅里叶变换红外光谱(FTIR),高效液相色谱(HPLC)(用于批吸附)和量子化学方法研究了水悬浮液中甲萘威(1-萘基-N-甲基氨基甲酸酯)从蒙脱石中的吸附量。吸附的甲萘威的吸附量强烈依赖于蒙脱石的表面电荷密度,与高表面电荷的SAz-相比,两种“低”表面电荷密度的蒙脱石(SHCa-1和SWy-2)上的吸附更多。 1蒙脱石。此外,西维因的吸附量很大程度上取决于可交换阳离子的性质,并且SWy-2的Ba约Cs约Ca> Mg约K> Na约Li的顺序。 Cs> Ba> Ca> K> K约Mg> Na约Li的锂蒙脱石(SHCa-1)。利用羰基伸缩带的位移作为西维因与可交换阳离子之间相互作用强度的指标,观察到的顺序为Mg> Ca> Ba约K> Na> Cs。羰基链的位置兴能带随着可交换阳离子的离子电势增加而移动到较低的波数。密度泛函理论预测了阳离子诱导的C = 0键加长,这是由于羰基直接与可交换阳离子相互作用而引起的,这有助于光谱学观察。 1355-1375 cm〜(-1)区域的几个振动带在相反方向上的伴随移动提供了证据,这些振动带被分配给氨基甲酸酯N-C_(羰基)和O_(醚)-C_(羰基)的伸展带这些数据表明西维因的吸附部分是由于氨基甲酸酯官能团与可交换阳离子之间的位点特异性相互作用所致,正如FTIR数据所证明的那样。然而,这些数据表明疏水性相互作用也有助于碳氢化合物的总量。例如,FTIR数据表明,当Cs〜+为可交换阳离子时,相互作用最弱。相反,最大吸附量为在所有被研究的阳离子中,Cs的水合焓最低。这表明低水合能为碳芳基提供了更大的进入硅氧烷表面疏水区域的通道。

著录项

  • 来源
    《Environmental Science & Technology》 |2005年第23期|p.9123-9129|共7页
  • 作者单位

    Crop,Soil and Environmental Sciences,Purdue University,915 West State Street,West Lafayette,Indiana 47907-2054,Department of Crop and Soil Sciences,Michigan State University,East Lansing,Michigan 48824-1325,and USDA-ARS National Soil Tilth Laboratory;

    Crop,Soil and Environmental Sciences,Purdue University,915 West State Street,West Lafayette,Indiana 47907-2054,Department of Crop and Soil Sciences,Michigan State University,East Lansing,Michigan 48824-1325,and USDA-ARS National Soil Tilth Laboratory;

    Crop,Soil and Environmental Sciences,Purdue University,915 West State Street,West Lafayette,Indiana 47907-2054,Department of Crop and Soil Sciences,Michigan State University,East Lansing,Michigan 48824-1325,and USDA-ARS National Soil Tilth Laboratory;

    Crop,Soil and Environmental Sciences,Purdue University,915 West State Street,West Lafayette,Indiana 47907-2054,Department of Crop and Soil Sciences,Michigan State University,East Lansing,Michigan 48824-1325,and USDA-ARS National Soil Tilth Laboratory;

    Crop,Soil and Environmental Sciences,Purdue University,915 West State Street,West Lafayette,Indiana 47907-2054,Department of Crop and Soil Sciences,Michigan State University,East Lansing,Michigan 48824-1325,and USDA-ARS National Soil Tilth Laboratory;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 环境化学;
  • 关键词

  • 入库时间 2022-08-17 14:07:58

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