4.7 Article

Effect of pH and the role of organic matter in the adsorption of isoproturon on soils

Journal

CHEMOSPHERE
Volume 57, Issue 8, Pages 771-779

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.chemosphere.2004.07.009

Keywords

herbicide; hydrogen bonding; hydrophobic interaction; multiple-step isotherm; TOC; UV absorbance

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Equilibrium measurements were carried out with the herbicide isoproturon on natural adsorbents (brown forest-, chemozem-, sandy soils and quartz) in different buffered media (pH 5, 7, 8 phosphate buffer). Adsorption isotherms were fitted by a multi-step adsorption equation providing numerical information used in the environmental propagation models and risk assessment works. In the adsorption of the slightly polar isoproturon the dissolved organic matter of the soil and the pH play an important role. At molecular level, results are interpreted by taking into consideration the hydrophobic interaction and the formation of hydrogen bonds between the surface and the solute. The observed adsorption behavior indicates that the organic matter content of the soils and its soluble fulvic acid, alkaline soluble humic acid and insoluble humin fractions were considerable different. The chernozem soil containing the highest amount of insoluble organic fraction proved to be a very efficient adsorbent. The brown forest and the sandy soils exhibit rather similar adsorbent properties but at pH 7 the latter containing more fulvic acid adsorbs less isoproturon due to the enhanced solubility of the soil organic matter. In alkaline conditions the negatively charged solute and the surface repel each other and the hydrophobic interactions are also weaker than in neutral media. (C) 2004 Elsevier Ltd. All rights reserved.

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