TECHNICAL PAPERS
Jun 25, 2009

Sediment Oxygen Demand and Nutrient Fluxes for a Tropical Reservoir in Singapore

Publication: Journal of Environmental Engineering
Volume 136, Issue 1

Abstract

Sediment oxygen demand (SOD) and nutrient flux studies were conducted for a tropical reservoir in Singapore in order to determine the approximate SOD and nutrient release rates from the sediments. SOD values obtained from laboratory experiments ranged from 1.4 to 3.3gO2/m2-day . Similar results were also obtained by calculating SOD values from in situ DO measurements taken in the field. The nutrient flux study was performed in the laboratory at a constant temperature of 25°C in oxic and anoxic columns. Except for nitrate+nitrite , higher nutrient release rates were generally observed under anoxic conditions. The ammonium release rate was 0.06gO2/m2-day under oxic conditions and 0.117gO2/m2-day under anoxic conditions. The nitrate flux rate was 0.17gO2/m2-day under oxic conditions but was negligible under anoxic conditions. Orthophosphate flux results were negative throughout the oxic incubation implying that sediments acted as a sink. The release rate of orthophosphate was 0.0076gO2/m2-day under anoxic conditions.

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Acknowledgments

We acknowledge the funding support from the UNSPECIFIEDPublic Utilities Board, Singapore.

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Information

Published In

Go to Journal of Environmental Engineering
Journal of Environmental Engineering
Volume 136Issue 1January 2010
Pages: 78 - 85

History

Received: Jul 22, 2008
Accepted: Jun 23, 2009
Published online: Jun 25, 2009
Published in print: Jan 2010

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Authors

Affiliations

Karina Yew-Hoong Gin E-mail: [email protected]
Associate Professor, School of Civil and Environmental Engineering, Nanyang Technological Univ., Block N1, 50, Nanyang Ave., Singapore 639798, Singapore (corresponding author). E-mail: [email protected]
Anuja Padma Gopalakrishnan
Project Officer, School of Civil and Environmental Engineering, Nanyang Technological Univ., Block N1, 50, Nanyang Ave., Singapore 639798, Singapore.

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