Abstract

Square wave voltammetry automated by sequential injection analysis was applied to determine the Freundlich adsorption coefficients for the adsorption of atrazine onto a clay rich soil. The detection limit in soil extracts was between 0.18 and 0.48 μmol L −1, depending on the medium used to prepare the extracts (0.010 mol L −1 KCl, CaCl 2 or HNO 3 and 0.0050 mol L −1 H 2SO 4), all of them conditioned in 40 mmol L −1 Britton–Robinson buffer at pH 2.0 in presence of 0.25 mol L −1 NaNO 3. Also in soil extracts the linear dynamic range was between 1.16 and 18.5 μmol L −1 (0.25–4.0 μg mL −1), with a sampling frequency of 190 h −1. The K f Freundlich adsorption coefficient was 3.8 ± 0.2 μmol 1−1/ n L n kg −1 in medium of 0.010 mol L −1 KCl or CaCl 2, but increased to 7.7 ± 0.1 and 9.0 ± 0.3 μmol 1−1/ n L n kg −1 in 0.010 mol L −1 HNO 3 and 0.0050 mol L −1 H 2SO 4, respectively. The increase of K f was related to the decrease of pH from 6.4–6.7 in KCl and CaCl 2 to 3.7–4.0 in presence of HNO 3 or H 2SO 4, which favors protonation of atrazine, facilitating electrostatic attractions with negative charges of the clay components of the soil. The 1/ n parameters were between 0.76 and 0.86, indicating that the isotherms are not linear, suggesting the occurrence of chemisorption at specific adsorption sites. No statistically significant differences were observed in comparison to the adsorption coefficients obtained by HPLC. The advantage of the proposed SI–SWV method is the great saving of reagent because it does not use organic solvent as in the case of HPLC (50% (v/v) acetonitrile in the mobile phase). Additionally the start up of SI–SWV is immediate (no column conditioning necessary) and the analysis time is only 19 s.

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