Quantifying sediment storage on the floodplains outside levees along the lower Yellow River during the years 1580–1849. Issue 2 (22nd October 2018)

• Record Type: Journal Article
• Authors: Chen, Yunzhen; Overeem, Irina; Kettner, Albert J.; Gao, Shu; Syvitski, James P. M.; Wang, Yuanjian
• Is Part Of: Earth surface processes and landforms. Volume 44:Issue 2(2019)
• Page Start: 581
• Page End: 594
• Publication Date: 2018-10-22
• Subjects: Sediment budget -- Yellow River -- Levee breaches -- Floodplain sedimentation -- Bankfull discharge; Geomorphology -- Periodicals; 551.4
• DOI: 10.1002/esp.4519
• Languages: English
• ISSNs: 0197-9337

Abstract

Abstract: The lower Yellow River channel was maintained by artificial levees between 1580 and 1849. During this period, 280 levee breaches occurred. To estimate sediment storage on the floodplains outside the levees, a regression model with a decadal time step was developed to calculate the outflow ratio for the years when levee breaching occurred. Uncertainty analysis was used to identify the likely outflow ratio. Key variables of the model include annual water discharge, a proxy for levee conditions, and potential bankfull discharge of the channel before flood season. Uncertainty analysis reveals an outflow ratio of 0.35–0.56. We estimate that during this period, 18.8–30.1% of the total ~312 Gt of sediment load was deposited on the floodplains outside the levees. Human‐accelerated erosion in the Loess Plateau caused a 4‐fold increase in sediment delivery to the lower Yellow River, which could not be accommodated by channel morphodynamic changes. As a result, 21.2–27.5% of the total sediment load was deposited within the levees, creating a super‐elevated channel bed that facilitated an uncommonly high breach outflow ratio. Hence, the factor of a large super‐elevation relative to the mean main channel depth should be considered when designing diversions to restore floodplains. © 2018 John Wiley & Sons, Ltd. Abstract : Around 24% of the sediment was deposited in the channel belt and floodplains within levees, 19–30% was trapped in the floodplains outside the levees, and the rest was delivered to the delta area. Human‐accelerated erosion in the Loess Plateau caused a super‐elevated channel bed on the lower river, which favors sediment trapping in the floodplains outside the levees.