Effect of Organic and Mineral Soil Fractions on Sorption Behaviour of Chlorophenol and Triazine Micropollutants
| Autor: | Sanja Fingler, Vlasta Drevenkar, Sanja Stipičević |
|---|---|
| Rok vydání: | 2009 |
| Předmět: |
Sorbent
010501 environmental sciences Toxicology 01 natural sciences Soil chemistry.chemical_compound Soil Pollutants Humic acid Freundlich equation Organic matter Atrazine Pesticides 0105 earth and related environmental sciences Triazine Chlorophenol chemistry.chemical_classification Minerals Herbicides Triazines 010401 analytical chemistry Public Health Environmental and Occupational Health Sorption 0104 chemical sciences chemistry Environmental chemistry Adsorption ametryn atratone atrazine chlorophenolate anions didealkylated atrazine Freundlich isotherm humic acid hydroxyatrazine mineral surface organic matter Hydrophobic and Hydrophilic Interactions Chlorophenols |
| Zdroj: | Archives of Industrial Hygiene and Toxicology. 60:43-52 |
| ISSN: | 0004-1254 |
| DOI: | 10.2478/10004-1254-60-2009-1898 |
| Popis: | Effect of Organic and Mineral Soil Fractions on Sorption Behaviour of Chlorophenol and Triazine Micropollutants This article compares the sorption behaviour of 2,4,6-trichlorophenol, 2,3,4,6-tetrachlorophenol, pentachlorophenol, chlorotriazine atrazine, methylthiotriazine ametryn, methoxytriazine atratone, hydroxyatrazine, and didelakylated atrazine in a topsoil and an aquifer sediment before and after removal of sorbent organic matter and in humic acid. Freundlich isotherm coefficients K f and 1/n and free energy change (δG°) were calculated for all compounds in all sorbents. According to sorbent pH values, chlorophenolate anions and uncharged triazine species dominated in all sorption experiments with topsoil and aquifer sediment. In experiments with humic acid, chlorophenols, atrazine, and didealkylated atrazine existed almost completely as neutral species, whereas protonated species dominated for hydroxyatrazine, atratone, and ametryn. In addition to a hydrophobic partition, sorption of all compounds in native soil and sediment sorbents includes specific, more polar interactions, which greatly depend on sorbate acidity/basicity, specific properties of the sorbent organic matter and of mineral surface, as well as on the system pH. A significantly greater sorption intensity of all compounds in "organic-free" than in the native aquifer sediment confirmed the importance and possible dominance of mineral surface in the sorption process. Sorption intensity of chlorophenol and triazine compounds in humic acid was closely related to compound hydrophobicity. Greater sorption of almost completely protonated hydroxyatrazine than of the more hydropohobic but uncharged atrazine indicated different humic acid reaction sites for two compounds and consequently different sorption mechanisms. |
| Databáze: | OpenAIRE |
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