Equilibrium partitioning of super(14)C-benzo(a)pyrene and super(14)C-benazolin between fractionated phases from an arable topsoil

Equilibrium partitioning of hydrophobic super(14)C-benzo(a)pyrene and hydrophilic super(14)C-benazolin between fractionated phases from an arable topsoil of Merzenhausen (Germany) was investigated. Topsoil samples were collected from lysimeters which were incubated with different residual crops. A p...

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Published in:Environmental pollution (1987) 2005-06, Vol.135 (3), p.491-500
Main Authors: Sequaris, J-M, Lavorenti, A, Burauel, P
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Burauel, P
description Equilibrium partitioning of hydrophobic super(14)C-benzo(a)pyrene and hydrophilic super(14)C-benazolin between fractionated phases from an arable topsoil of Merzenhausen (Germany) was investigated. Topsoil samples were collected from lysimeters which were incubated with different residual crops. A physical soil fractionation based on sedimentation and centrifugation steps was performed after water extraction. Four soil phases were obtained designated sediment (SED) phase (>20 mu m), microaggregate (MA) phase (2 mu m-20 mu m), colloid (COL) phase (
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Topsoil samples were collected from lysimeters which were incubated with different residual crops. A physical soil fractionation based on sedimentation and centrifugation steps was performed after water extraction. Four soil phases were obtained designated sediment (SED) phase (&gt;20 mu m), microaggregate (MA) phase (2 mu m-20 mu m), colloid (COL) phase (&lt;2 mu m) and electrolyte (EL) phase. The distribution of super(14)C- benzo(a)pyrene, super(14)C-benazolin and organic carbon between the soil phases was established. Enrichment factors for the two chemicals and organic carbon are higher in the COL and MA phases than in the SED phase. The distribution constant K sub(d) of chemicals for Merzenhausen topsoil was calculated according to two-phase or three-phase partitioning models. The three-phase partitioning model presumes the contribution of the organic carbon for the binding of chemicals. A log K sub(oc) of 5.55 can be calculated in the case of super(14)C- benzo(a)pyrene, which is typical of the hydrophobic association with the soil organic carbon. In the case of super(14)C-benazolin, much higher K sub(d) and K sub(oc) values were calculated than found with parent molecules after short-time experiments. Long-term aging processes must be considered. Specific effects on the chemical distribution due to the different crop residues were not detected. 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Topsoil samples were collected from lysimeters which were incubated with different residual crops. A physical soil fractionation based on sedimentation and centrifugation steps was performed after water extraction. Four soil phases were obtained designated sediment (SED) phase (&gt;20 mu m), microaggregate (MA) phase (2 mu m-20 mu m), colloid (COL) phase (&lt;2 mu m) and electrolyte (EL) phase. The distribution of super(14)C- benzo(a)pyrene, super(14)C-benazolin and organic carbon between the soil phases was established. Enrichment factors for the two chemicals and organic carbon are higher in the COL and MA phases than in the SED phase. The distribution constant K sub(d) of chemicals for Merzenhausen topsoil was calculated according to two-phase or three-phase partitioning models. The three-phase partitioning model presumes the contribution of the organic carbon for the binding of chemicals. A log K sub(oc) of 5.55 can be calculated in the case of super(14)C- benzo(a)pyrene, which is typical of the hydrophobic association with the soil organic carbon. In the case of super(14)C-benazolin, much higher K sub(d) and K sub(oc) values were calculated than found with parent molecules after short-time experiments. Long-term aging processes must be considered. Specific effects on the chemical distribution due to the different crop residues were not detected. 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Topsoil samples were collected from lysimeters which were incubated with different residual crops. A physical soil fractionation based on sedimentation and centrifugation steps was performed after water extraction. Four soil phases were obtained designated sediment (SED) phase (&gt;20 mu m), microaggregate (MA) phase (2 mu m-20 mu m), colloid (COL) phase (&lt;2 mu m) and electrolyte (EL) phase. The distribution of super(14)C- benzo(a)pyrene, super(14)C-benazolin and organic carbon between the soil phases was established. Enrichment factors for the two chemicals and organic carbon are higher in the COL and MA phases than in the SED phase. The distribution constant K sub(d) of chemicals for Merzenhausen topsoil was calculated according to two-phase or three-phase partitioning models. The three-phase partitioning model presumes the contribution of the organic carbon for the binding of chemicals. A log K sub(oc) of 5.55 can be calculated in the case of super(14)C- benzo(a)pyrene, which is typical of the hydrophobic association with the soil organic carbon. In the case of super(14)C-benazolin, much higher K sub(d) and K sub(oc) values were calculated than found with parent molecules after short-time experiments. Long-term aging processes must be considered. Specific effects on the chemical distribution due to the different crop residues were not detected. The partition coefficient (K sub(d)) of chemicals was calculated according to two-phase or three-phase partitioning models.</abstract><doi>10.1016/j.envpol.2004.10.018</doi></addata></record>
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title Equilibrium partitioning of super(14)C-benzo(a)pyrene and super(14)C-benazolin between fractionated phases from an arable topsoil
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