Case Studies
Jul 9, 2015

Maintaining Sediment Flows through Hydropower Dams in the Mekong River Basin

Publication: Journal of Water Resources Planning and Management
Volume 142, Issue 1

Abstract

The planning, design, and construction of hydropower dams are occurring at a rapid pace in the Mekong/Lancang River Basin in Southeast Asia. For years the river and its tributaries transported an average of 160 million metric tons of sediment per year to the South China Sea. Reservoirs are expected to trap significant fractions of this sediment, rendering much of it unavailable to transport nutrients and maintain the river’s geomorphic structure and ecological habitats. This paper introduces and applies a method for identifying and evaluating alternative dam siting, design, and operating (SDO) policy options that could help maintain more natural sediment regimes and for evaluating the effect of these sediment-management strategies on hydropower production. This paper focuses on the planned Lower Sesan 2 (LSS2) Dam in Cambodia. This dam would prevent a significant source of sediment from reaching critical Mekong ecosystems, such as Cambodia’s Tonle Sap Lake and the Mekong Delta in Vietnam. The concept of replacing LSS2 as planned with several smaller alternative dams with SDO modifications to enable reservoir sediment flushing is evaluated. These modifications could increase sediment discharge from this site by as much as three to four times compared to current plans but reduce short-term annual energy production by a third or more. Results demonstrate that most of the loss in energy production associated with SDO modifications (at least 94% in the cases considered) results from reduced reservoir size as opposed to modified reservoir operations. It is also found that, from an operational standpoint, sediment flushing is likely best conducted during the transition period between the dry and wet seasons.

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Acknowledgments

This work was funded in part by Cornell University’s David R. Atkinson Center for a Sustainable Future (ACSF). The authors wish to thank the MRC for providing data and advice throughout our studies, including reservoir and dam characteristics data (MRC 2012, 2014) and streamflow data (MRC 2011a). We extend our gratitude to Matt Kondolf and Zan Rubin for helpful discussions and sediment load predictions and to Tom Cochrane, Thanapon Piman, and Mauricio Arias for help in generating 3S basins maps (Fig. 1) and simulating 3S basins flows. We also thank the reviewers for their helpful comments on previous drafts of this manuscript.

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Journal of Water Resources Planning and Management
Volume 142Issue 1January 2016

History

Received: Dec 12, 2014
Accepted: Apr 22, 2015
Published online: Jul 9, 2015
Discussion open until: Dec 9, 2015
Published in print: Jan 1, 2016

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Thomas B. Wild [email protected]
Postdoctoral Fellow, School of Civil and Environmental Engineering, Cornell Univ., Ithaca, NY 14853 (corresponding author). E-mail: [email protected]
Daniel P. Loucks, Dist.M.ASCE [email protected]
Professor Emeritus, School of Civil and Environmental Engineering, Cornell Univ., Ithaca, NY 14853. E-mail: [email protected]
George W. Annandale, F.ASCE [email protected]
Principal, Golder Associates, 44 Union Blvd., Suite 300, Lakewood, CO 80228. E-mail: [email protected]
Prakash Kaini [email protected]
Water Resources Consultant, Hydro Worldwide Inc., Littleton, CO 80123. E-mail: [email protected]

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