Development of the erosion rate model for weak rock river bed (3/3)
Owing to the effects of environmental changes (e.g., earthquake uplift, climate change, etc.) or human activities (e.g., hydraulic engineering, infrastructures construction, gravel mining, etc.), bedrock scouring and stream instability were induced in several major rivers of western Taiwan.Most of the major rivers in western Taiwan flow over the Western Foothills which composed of weak sedimentary rocks.Once the weak rocks lost the protection from overlain armor layer, the channel bedrock erosion progressed rapidly.In order to properly manage the issue of rapid morphological change in river reaches, related works on the subject of weak bedrock erosion carried out in this three-years project, including literature review and data collection, investigation of erosive characteristics of bedrock and rock riverbank, development of erosion rate model for weak rock riverbed and riverbank, and development of guidelines for evaluation of bedrock scour and strategy suggestion for bedrock scour countermeasures.
This is the third executive year of the three-year project.The objectives of this project were all accomplished, including: 1) proposing erosion mechanisms for weak bedrock erosion based on the erosion data of the studied reaches;2) development of erosion rate model for weak rock riverbed; 3) development of erosion rate model for weak rock riverbank; 4) proposing guidelines for evaluation of bedrock scour and strategy suggestion for bedrock scour countermeasures.