Sonophotocatalytic mineralization of antipyrine in aqueous solution

•The UV/H2O2/Fe/US process is an alternative for mineralization of antipyrine.•92% of TOC is removed after 50min.•Antipyirine photodegradation proceeds mainly through a radical mechanism.•Important synergistic effect (45.3%) between sonolysis and photoFenton. The mineralization of aqueous solutions...

Full description

Saved in:
Bibliographic Details
Published inApplied catalysis. B, Environmental Vol. 138-139; pp. 318 - 325
Main Authors Durán, A., Monteagudo, J.M., Sanmartín, I., García-Díaz, A.
Format Journal Article
LanguageEnglish
Published Kidlington Elsevier B.V 17.07.2013
Elsevier
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:•The UV/H2O2/Fe/US process is an alternative for mineralization of antipyrine.•92% of TOC is removed after 50min.•Antipyirine photodegradation proceeds mainly through a radical mechanism.•Important synergistic effect (45.3%) between sonolysis and photoFenton. The mineralization of aqueous solutions of antipyrine, an emerging contaminant, using an innovative homogeneous sono-photocatalytic oxidation process (H2O2/UV/Fe/Ultrasound) was evaluated in an artificial UV lamp. At the selected operation conditions [H2O2]=1500ppm, pH=2.7, amplitude=100%, pulse length (cycles)=0.3 during 15min and then 1, 92% of TOC is removed after 50min treating an aqueous solution containing 50ppm of antipyrine. An important synergistic effect between sonolysis and photoFenton (UV/H2O2/Fe) of 45.4% was quantified using the first order rate constants for TOC. Comparison experiments of scavenger-loaded conditions demonstrate that the antipyirine photodegradation proceeds mainly through a radical mechanism probably beginning by the cleavage of the NN bond of penta heterocycle leading to the formation of aromatic acids (anthranilic and 1,4-benzenedicarboxylic acids) then followed by the opening of phenyl ring to form small molecular organic acids (mainly 2-butenedioic, 4-oxo-pentanoic and butanedioic acids), which may be decomposed further into CO2.
Bibliography:ObjectType-Article-2
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 23
ObjectType-Article-1
ObjectType-Feature-2
ISSN:0926-3373
1873-3883
DOI:10.1016/j.apcatb.2013.03.013