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Abstract

A two-dimensional flow model was constructed to assess the impact of levee axis adjustment on flow variation at Xinsha Island. The results indicate that the longer the return periods, the higher the water level in the southern waterway, with a maximum increase of 0.183 m. Conversely, the northern waterway exhibits a water level decrease, with a maximum reduction of 0.128 m. The flow velocity in the southern waterway diminished by roughly 0.3 m/s, but the flow velocity in the northern waterway rose by a maximum of 0.45 m/s. After the levee axis is adjusted, the flow diversion capacity of the north waterway is effectively enhanced, thereby benefiting flood regulation. Relationships between variations in upstream boundary discharge and flow variations surrounding Xinsha Island are presented to facilitate swift and dependable forecasts. These findings clearly illustrate the influence of levee axis changes on the hydrodynamic properties of the river.
Original languageEnglish
Number of pages22
JournalWater
Volume18
Issue number9
Early online date22 Apr 2026
DOIs
Publication statusE-pub ahead of print - 22 Apr 2026

Data Availability Statement

The raw data supporting the conclusions of this article will be made available by the authors on request.

Funding

This research was funded by the National Natural Science Foundation of China, grant number 52401330.

Keywords

  • Fuchun River
  • numerical river flow modelling
  • levee adjustment
  • hydrological impacts

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