Abstract
This paper presents the measurement results of turbulent velocity fields for flows in a deep open experiment channel with dense vegetation. The flows showed the strong 3-dimensional properties that the maximum flow directional velocity appears near the 1/3 water depth from the bottom and Reynolds stress become negative over the 2/3 water depth area. For the cause of the phenomena, transport of low velocity fluid by strong boils to go upward from the bottom near vegetation boundary was suggested from the distribution of turbulent flow energy.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.