1989/11/01 by Juan A. Zazo, José A. Casas, A.F. Mohedano +4 · 2 citations
Chemistry · Earth and Planetary Sciences · Environmental Science · #Acetic acid #Advanced oxidation water treatment #Aerosol #Air pollution #Aqueous solution #Arctic #Atmospheric and Environmental Gas Dynamics #Atmospheric chemistry and aerosols #Atmospheric sciences #Benzene #Benzoquinone #Catechol #Chemistry #Climatology #Electrochemical Analysis and Applications #Environmental science #Formic acid #Geography #Geology #Hydroquinone #Maleic acid #Malonic acid #Meteorology #Muconic acid #Neutron activation analysis #Oceanography #Organic chemistry #Oxalic acid #Phenol #Phenols #Precipitation #Reagent #Water Quality Monitoring and Analysis
paper · doi:10.1021/es050452h
openalex publication_date 1989/11/01 · openalex created_date 2016/06/24 · openalex updated_date 2026/06/11
Phenol oxidation by Fenton's reagent (H2O2 + Fe2+) in aqueous solution has been studied in depth for the purpose of learning more about the reactions involved and the extent of the oxidation process, under various operating conditions. An initial phenol concentration of 100 mg/L was used as representative of a phenolic industrial wastewater. Working temperatures of 25 and 50 degrees C were tested, and the initial pH was set at 3. The H2O2 and the Fe2+ doses were varied in the range of 500-5000 and 1-100 mg/L, respectively, corresponding to 1-10 times the stoichiometric ratio. A series of intermediates were identified, corresponding mainly to ring compounds and short-chain organic acids. Most significant among the former were catechol, hydroquinone, and p-benzoquinone; the main organic acids were maleic, acetic, oxalic, and formic, with substantially lower amounts of muconic, fumaric, and malonic acids. Under milder operating conditions (H2O2 and Fe2+ at lower concentrations), a great difference was found between the measured total organic carbon (TOC) and the amount of carbon in all analyzed species in the reaction medium. This difference decreased as the doses of H2O2 and Fe2+ increased, indicating that the unidentified compounds must correspond to oxidation intermediates between phenol and the organic acids. To establish a complete oxidation pathway, experiments were carried out using each of the identified intermediates as starting compounds. Dihydroxybenzenes were identified in the earlier oxidation stages. Muconic acid was detected in catechol but not in the hydroquinone and p-benzoquinone oxidation runs; the last two compounds were oxidized to maleic acid. Oxalic and acetic acid appeared to be fairly refractory to this oxidation treatment. A detailed knowledge of the time evolution of the oxidation intermediates is of environmental interest particularly in the case of hydroquinone and p-benzoquinone because their toxicities are several orders of magnitudes higher than that of phenol itself. The time evolution of the intermediates and TOC was fitted to a simple second-order kinetic equation, and the values of the kinetic constants were determined. This provides a simplified approach useful for design purposes.