Abstract
Membrane introduction mass spectrometry (MIMS) was used to directly monitor the loss of trace gasoline contaminants (benzene, toluene, 2-methylthiophene and methylcyclohexane) in nanomolar (ppb) aqueous solutions under a variety of UV-induced advanced oxidation processes (AOP). The decay kinetics of these contaminants were followed simultaneously in “real-time” via tandem mass spectrometric techniques by re-circulating the reaction mixture in a closed loop over a semi-permeable membrane interface. The photocatalyzed degradations were observed to follow pseudo–first-order kinetics with rate constants ranging from 0.006 to 0.2 min−1 depending on the reaction conditions. We report rate enhancements for several UV-based advanced oxidative processes using physisorbed titanium dioxide (TiO2/UV, TiO2/UV/O2, TiO2/UV/H2O2) and compare these to the direct photolysis of H2O2 under otherwise identical conditions. The relative degradation rates of 4 trace contaminants are reported for reactions carried out in the same solution. The degradation kinetics were also monitored directly in a natural surface water spiked with the same contaminant suite. The observed decay kinetics in the presence of TiO2 in air-saturated natural water were similar to those carried out in deionized water. However, when the photo-oxidation was enhanced by the addition of H2O2, the degradation was markedly slower in natural water relative to deionized water due to competition for photons by dissolved organic matter. This work further demonstrates the use of MIMS as a sensitive on-line measurement technique for “in-situ” reaction monitoring of organic contaminants at environmentally relevant concentrations in complex solutions and reactive media.
Acknowledgments
The authors acknowledge the Canada Foundation for Innovation, the British Columbia Knowledge Development Fund, the Science Council of British Columbia and Vancouver Island University for infrastructure funding to establish the Applied Environmental Research Laboratories. The authors are grateful for the financial support of this work provided by the Natural Science and Engineering Council of Canada (NSERC) through the Discovery and USRA programs. The authors also wish to thank an anonymous reviewer for their constructive and helpful suggestions.
Notes
1 [H2O2] = 5 mM,
2 [H2O2] = 20 mM,
3 [H2O2] = 2.6 mM,
4 [H2O2] = 8 mM, [Fe2 +] = 0.1 mM.
*Selected ion monitoring (SIM) used in this case.
1 air saturated at 45°C, [O2,aq] = 0.19 mM.
2 oxygen saturated at 45°C, [O2,aq] = 0.90 mM.
3 [H2O2,aq] = 70 mM.
4 % k 1 = A/(A+B) * 100, where A and B are pre-exponential terms in y = A e −k1t + B e −k2t .