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Environmental problems - Chemical approaches
RESEARCH ARTICLE

Monitoring advanced oxidation of Suwannee River fulvic acid

Janey V. Camp A B E , Dennis B. George A B , Martha J. M. Wells A C F and Pedro E. Arce D
+ Author Affiliations
- Author Affiliations

A Center for the Management, Utilisation, and Protection of Water Resources, Tennessee Technological University, Box 5033, Cookeville, TN 38505, USA.

B Department of Civil and Environmental Engineering, Tennessee Technological University, Cookeville, TN 38505, USA. Email: dgeorge@tntech.edu

C Department of Chemistry, Tennessee Technological University, Cookeville, TN 38505, USA.

D Department of Chemical Engineering, Tennessee Technological University, Cookeville, TN 38505, USA. Email: parce@tntech.edu

E Present address: Department of Civil and Environmental Engineering, Vanderbilt University, Nashville, TN 37203, USA. Email: janey.v.smith@vanderbilt.edu

F Corresponding author. Email: mjmwells@tntech.edu

Environmental Chemistry 7(3) 225-231 https://doi.org/10.1071/EN09146
Submitted: 18 November 2009  Accepted: 18 March 2010   Published: 22 June 2010

Environmental context. Potentially toxic disinfection by-products form when water containing humic and fulvic acids is chlorinated to destroy pathogenic microorganisms. A pulsed electrical discharge was examined for its ability to destroy an aquatic fulvic acid by oxidation. Spectroscopically, changes in the organic structures were observed, but carbon content and disinfection by-products were not reduced.

Abstract. A pilot-scale pulsed electrical discharge (PED) system was used to treat Suwannee River fulvic acid (SRFA) as a representative precursor material for the formation of disinfection by-products (DBPs), specifically trihalomethane compounds. Ultraviolet-visible and fluorescence spectroscopy, dissolved organic carbon (DOC), and the trihalomethane formation potential (THMFP) were used as analytical parameters to monitor the effects of treatment on the substrate. The potential for SRFA degradation (5 mg L–1 DOC) was examined over 60 min at each of four operational configurations, varying pulse energy and frequency (0.15 J and 60 Hz, 0.15 J and 120 Hz, 0.4 J and 60 Hz, and 0.4 J and 120 Hz) in a factorial design. Statistically significant changes occurred for UV254, EX254EM460, and EX328EM460 under selected conditions; however, concomitant changes in DOC and THMFP were not observed. The composition of SRFA changed, but organic carbon was not mineralised to carbon dioxide. In addition to showing degradation by PED, the significance of the preliminary findings of this research was to demonstrate that spectroscopic monitoring of precursor degradation alone can be misleading, and that whereas ultraviolet-visible and fluorescence spectroscopy indicated degradation of precursor compounds, DOC and THMFP measurements were unchanged and did not support the occurrence of mineralisation in this system.

Additional keywords: disinfection by-products, dissolved organic matter, pulsed electrical discharge, trihalomethane formation potential.


Acknowledgements

Assistance from Prit Chowdhuri, Jerry Fishback, Jeff Holmes, Perry Melton, Mary Nubbe, Mike Renfro, and the Environmental Quality Laboratory staff is gratefully acknowledged.


References


[1]   J. J. Rook , Formation of haloforms during chlorination of natural waters. Water Treat. Exam. 1974 , 23,  234.
         [Verified 16 November 2009]