EGU24-14030, updated on 09 Mar 2024
https://doi.org/10.5194/egusphere-egu24-14030
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Secondary Flow and Turbulent Kinetic Energy in a Dredged Channel with Riverbank

Sukhjeet Arora, Harish Kumar Patel, Abhijit Dilip Lade, and Bimlesh Kumar
Sukhjeet Arora et al.
  • IIT Guwahati, IIT Guwahati, Civil Engineering, Guwahati, India (sukhjeet@iitg.ac.in)

Sand dredging from the rivers has become an uncontrolled practice that harms the river's ecology. It affects the flow structure of the river, leading to further deterioration of the river's morphology. Several field investigations and experimental studies have conformed to the erosive effects of sand mining pits upstream and downstream of mining locations. We conducted laboratory-scale flume experiments to study the impact of a mining pit on the secondary flow structure across a riverbank cross-section. Three bank slopes were tested, namely, 25°,31°, and 40°, and gravity flow experiments were conducted with and without a mining pit. Turbulent velocity data across the cross-section was analyzed to study the transverse and velocity distribution across the riverbank for both with-pit and without-mining-pit cases. Results show that dredging an upstream mining pit significantly affects the transverse and vertical velocities, especially on the bank slopes and near the bed in the main channel portion. The turbulent kinetic energy in the flow region on the bank slope and near the bed in the main channel portion significantly increases because of the pit excavation. These alterations in the secondary flow within the riverbank can lead to morphological changes and may affect the bank stability of rivers.

Keywords: Sand Mining, Turbulent kinetic energy, turbulence

How to cite: Arora, S., Kumar Patel, H., Dilip Lade, A., and Kumar, B.: Secondary Flow and Turbulent Kinetic Energy in a Dredged Channel with Riverbank, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-14030, https://doi.org/10.5194/egusphere-egu24-14030, 2024.