Abstract

Continuous channel degradation has occurred recently in the Lower Yellow River (LYR) due to water impoundment of the Xiaolangdi Reservoir. In this paper, observed hydrological data from 1999 to 2005 were used to analyze the processes and characteristics of recent channel adjustment in the LYR. Main research results can be described as follows. The scour amount in the braided reach made up 77% of the total one in the LYR, and the scour magnitude per unit channel length in the braided reach upstream of Gaocun was relatively large, while the value in the reach between Gaocun and Sunkou was lowest among all the lower reaches. Cross-sectional profiles adjustment in the lower reaches was characterized by channel narrowing. The longitudinal main-channel profiles in the LYR during different periods were concave-shape curves, and concavity values of these profiles increased slightly with the recent channel degradation. Bankfull discharges in the lower reaches increased due to the scouring in the main channel. Migration amplitude of the thalweg in the braided reach was greater than that in the meandering reach.

 

Keywords: The Xiaolangdi Reservoir, the Lower Yellow River, Channel adjustment, cross-sectional profiles, Longitudinal profiles, Concave-shape curves, bankfull discharge, channel migration