Sediment budget as affected by construction of a sequence of dams in the lower Red River, Viet Nam

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• 作者：Xi Xi Lu^a ; ^b ; ^{geoluxx@nus.edu.sg" class="auth_mail" title="E-mail the corresponding author} ; Chantha Oeurng^c ; Thi Phuong Quynh Le^d ; Duong Thi Thuy^e
• 关键词：Dam impacts ; Sediment budget ; Sediment deposition ; Red River ; Vietnam
• 刊名：Geomorphology
• 出版年：2015
• 出版时间：1 November 2015
• 年：2015
• 卷：248
• 期：Complete
• 页码：125-133
• 全文大小：1836 K

文摘

Dam construction is one of the main factors resulting in riverine sediment changes, which in turn cause river degradation or aggradation downstream. The main objective of this work is to examine the sediment budget affected by a sequence of dams constructed upstream in the lower reach of the Red River. The study is based on the longer-term annual data (1960–2010) with a complementary daily water and sediment data set (2008–2010). The results showed that the stretch of the river changed from sediment surplus (suggesting possible deposition processes) into sediment deficit (possible erosion processes) after the first dam (Thac Ba Dam) was constructed in 1972 and changed back to deposition after the second dam (Hoa Binh Dam) was constructed in 1985. The annual sediment deposition varied between 1.9 Mt/y and 46.7 Mt/y with an annual mean value of 22.9 Mt/y (1985–2010). The sediment deposition at the lower reach of the Red River would accelerate river aggradation which would change river channel capacity in the downstream of the Red River. The depositional processes could be sustained or changed back to erosional processes after more dams (the amount of sediment deposit was much less after the latest two dams Tuyen Quang Dam in 2009 and Sonla Dam in 2010) are constructed, depending on the water and sediment dynamics. This study revealed that the erosional and depositional processes could be shifted for the same stretch of river as affected by a sequence of dams and provides useful insights in river management in order to reduce flood frequency along the lower reach of the Red River.