Abstract
In this paper, we investigate the behavior of total sediment transport in the Barudbug weir, Situdam, Karawang, West Java, Indonesia, which is a crucial aspect of water management in the Citarum river basin. We utilize SESAME instrument observation data, encompassing rainfall, TSS, and depth parameters, gathered over a period of approximately three years. Additionally, we employ a two-dimensional Advection-Diffusion analytic model that takes into account settling velocity. The observation results reveal a positive correlation between TSS and depth, with TSS levels increasing following heavy rainfall. Furthermore, there exists a time delay between rainfall events and the subsequent rise in TSS concentration, suggesting an upstream source of sediment. The model outcomes demonstrate an inverse relationship between TSS concentration and the velocity of river flow, as the river flow acts as a leaching mechanism.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callMore From: IOP Conference Series: Earth and Environmental Science
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.
