Monday, 7 November 2005
11

Fate of Ammonium in Aerated and Conventional Septic System Leachfield Soil Using Stable Nitrogen Isotope Tracer Techniques.

John T. Richard1, David A. Potts2, Josef Gorres1, Jose Amador1, and Barb Nowicki1. (1) University of Rhode Island, 024 Coastal Institute - Kingston, Kingston, RI 02881, (2) Geomatrix, LLC, Killingworth, CT 06419

 

 

Approximately ¼ of the population of the U.S. relies on onsite wastewater treatment systems (OWTS) for disposal of domestic wastewater. Failing or improperly functioning OWTS are public health and environmental hazards because of their potential to degrade ground, surface, and coastal water quality. It has been estimated that up to 50% of the N inputs into Greenwich Bay, Rhode Island comes from septic system effluent. Comparison of an innovative OWTS using a patented leachfield aeration process (AIR) compared to a traditional leachfield (LEACH) has shown that aeration improves effluent quality, with a greater percent removal of N. Although N removal has been documented, the processes responsible have not been characterized. The main goal of this project was to characterize the fate of nitrogen (as NH4+) from septic tank effluent in AIR and LEACH soil by amending it with 15NH4Cl, and Br-, to trace transformations of N over a 24 h period in the gas, drainage water, and soil pools. Our hypothesis was that the bulk of the 15N label would show up in the water pool as 15NO3-, and in the gas pool as 15N2 and 15N2O in the AIR treatment as a result of nitrification and subsequent denitrification. Preliminary analysis of the drainage water showed that the bulk of the inorganic N pool was composed of 15NO3- in the AIR treatment.  Gas isotope data indicates at least a 1000-fold 15N enrichment in the AIR treatment relative to the LEACH treatment, indicating the occurrence of denitrification in the AIR treatment.

 

 


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