1. Academic Validation
  2. Leaching of terbumeton and terbumeton-desethyl from mini-columns packed with soil aggregates in laboratory conditions

Leaching of terbumeton and terbumeton-desethyl from mini-columns packed with soil aggregates in laboratory conditions

  • Chemosphere. 2006 Nov;65(9):1600-9. doi: 10.1016/j.chemosphere.2006.03.046.
A Conrad 1 O Dedourge R Cherrier M Couderchet S Biagianti
Affiliations

Affiliation

  • 1 Laboratoire d'Eco-Toxicologie, Université de Reims Champagne-Ardenne, Unité de Recherche Vignes et Vins de Champagne, UFR Sciences Exactes et Naturelles, URVVC UPRES-EA 2069, Moulin de la Housse, Reims, France. arnaud.conrad@univ-reims.fr
Abstract

Leaching of terbumeton (TER) and terbumeton-desethyl (TED) from mini-columns packed with natural soil aggregates was investigated. Five soil samples from the Champagne area (France) with different physicochemical parameters were used. The soil samples were hand-packed into a 50 mm column in laboratory conditions. An aqueous solution of TER or TED was percolated through the column and collected effluents were analyzed for TER or TED using HPLC-DAD. The leaching experiments showed that TER and TED were moderately mobile. TED was more mobile than TER, possibly because of its higher polarity. The proportion of organic matter affected the mobility of TER and TED through soil columns (r=0.971) and leaching was lowest for soil having the highest organic matter content (5.9%). TER and TED were not significantly influenced by leaching solution composition (deionized water or CaCl(2) solution), but were strongly affected by soil packing. Packing resulted in less rapid release of compounds suggesting that unpacking may have contributed to preferential pathways through the soil columns. Increasing contact time between TER and soils before leaching decreased the mobility of TER and increased its persistence in soils. Indeed, 76% of TER was released when leaching started after a 15 h contact time whereas it was down to 26% after an aging treatment of 360 h. A proportion of TER (from 8% to 32%) and TED (from 8% to 17%) remained in soil. Associated to its high stability in soils this could in part account for a very slow transfer over the years towards the groundwater.

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