EFFECT OF CHLORINE CONTENT OF CHLORINATED PHENOLS ON THEIR OXIDATION-KINETICS BY FENTONS REAGENT

Authors
Citation
Wz. Tang et Cp. Huang, EFFECT OF CHLORINE CONTENT OF CHLORINATED PHENOLS ON THEIR OXIDATION-KINETICS BY FENTONS REAGENT, Chemosphere, 33(8), 1996, pp. 1621-1635
Citations number
12
Categorie Soggetti
Environmental Sciences
Journal title
ISSN journal
00456535
Volume
33
Issue
8
Year of publication
1996
Pages
1621 - 1635
Database
ISI
SICI code
0045-6535(1996)33:8<1621:EOCCOC>2.0.ZU;2-C
Abstract
The effect of chlorine content of chlorinated phenols on their oxidati on kinetics by Fenton's reagent was evaluated through different kineti c studies. First, elementary oxidation rate constants between hydroxyl radicals and 2,4-DCP,2,4,6-TCP as determined in this study are 7.210 (9) M(-1)s(-1) and 6.310(9) M(-1)s(-1), respectively. The relative ra tios between the rate constants of 2-CP and 2,4,6-TCP referred to the rate constant of 2,4-DCP indicates that the reactivity of chorophenols decreases with increasing substitution of chlorine on the aromatic ri ng. Second, the pseudo-first order oxidation kinetic constants at over dosed H2O2 and Fe2+ were proportional to the number of unsubstituted p ositions, while no correlation between dechlorination constants and th e number of unoccupied sites on the aromatic ring was found. Third, de chlorination kinetic model as a function of H2O2, Fe2+, and chlorophen ol concentration was developed. At constant H2O2 concentration of 510 (-3) M, the observed dechlorination rate constants for 2-MCP, 2,4-DCP, and 2,4,6-TCP are 1.1610(7) M(-1)s(-1), 2.28*10(7) M(-1)s(-1), and 4 .3610(8) M(-1)s(-1), respectively. All of these results demonstrated that the oxidation rate constants decrease with increasing content of chlorine. In addition, the initial dechlorination rates do not change significantly for all the chlorinated phenols studied at constant H2O2 and Fe2+ concentration, which suggests that the limiting step in Fent on chemistry is the generation of hydroxyl radicals through H2O2 and F e2+. Copyright (C) 1996 Elsevier Science Ltd.