Acetone is a significant pollutant in contaminated
groundwaters and industrial effluents. It can be
treated
by the UV/H2O2 process but only slowly.
This study
aims to understand the degradation mechanism and
hence the reasons for slow treatment. The degradation of acetone was carried out in a UV reactor
in the presence of ∼16 mM H2O2 such that
most
of the UV was absorbed by H2O2. The decay
of acetone
was followed by gas chromatography, and the
generation of intermediates (identified as acetic, formic,
and oxalic acids) was followed by ion chromatography.
Measurement of the total organic carbon indicated a
complete carbon balance throughout the reaction
ending in mineralization. A kinetic model, based on
an
assumed mechanism, was developed that generated
a profile of reactants and intermediates in
agreement with the experimental data, including the
pH profile. The initial concentrations of acetone
and hydrogen peroxide strongly affect the initial rate
of acetone degradation, but no pH effect was
observed in the range of 2−7. It is concluded that
acetone treats slowly because intermediates build
up to such a concentration that they compete
significantly for hydroxyl radicals and also because
the mechanism appears to involve some degree of
acetone recycling.