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Mathematical simulation of flow in the Sedone river | |
Author | Nguyen Huu-Thoi |
Call Number | AIT SSPR no. WA-89-07 |
Subject(s) | Hydraulics--Mathematical models |
Note | A special study submitted in partial fulfilment of the requirements for the degree of Diploma AIT, School of Engineering and Technology |
Publisher | Asian Institute of Technology |
Series Statement | Special studies project report ; no. WA-89-07 |
Abstract | Due to the need to know the backwater effect from the Mekong river at Pakse along the Sedone river, this special study on mathematical simulation of flow in the Sedone river is then made. A one-dimensional finite difference model is developed to simulate the hydraulic conditions of the river consisting of two subsystems, namely Subsystem 1 from Muang Souvannakhili to Ban Dong Gnang and Subsystem 2 right downstream from the weirs to Pakse at the Mekong River. The division of the river into two subsystems is made at the Selabam Fall where unknown energy loss exists. The developed mathematical model is successfully applied to the simulation of flow in Subsystem 1. However, the model would not work well for Subsystem 2 unless some modifications of riverbed would be introduced due to the complexity of the topographical condition in the vicinity of the powerhouse and a significant drop of the riverbed. Calibrations and simulations are carried out for the flows from June to October, using data available in 1987. The results obtained from calibrations show that the roughness coefficients applied to the system are variable, depending on flow conditions (low, medium or high flow) and local topographic conditions of the reaches of the river. The values of Manning's n are highest for low flow. Based on the computed data together with observed data, the rating curves at a number of stations along the considered river system are developed. There is a good agreement between these developed rating curves with those developed by TATA Consulting Engineers for most of the stations. The results show that the looping rating occurs for Gauge No. 9. A study on the effect of highwater levels at Pakse on the water levels at Tailrace is also conducted. It is found from the study that the effect of backwater goes very far upstream from Pakse. However, the backwater effect would not reach Gauge No. 4 (Tailrace) when the water levels at Pakse are less than 102.40 m MSL. |
Year | 1989 |
Corresponding Series Added Entry | Asian Institute of Technology. Special studies project report ; no. WA-89-07 |
Type | Special Study Project Report (SSPR) |
School | School of Engineering and Technology |
Department | Department of Civil and Infrastucture Engineering (DCIE) |
Academic Program/FoS | Water Resources Research Engineering (WA) |
Chairperson(s) | Suphat Vongvisessomjai |
Degree | Special Studies Project Report (M. Sc.) - Asian Institute of Technology, 1989 |