Abstract

The objectives of this study are: 1) to capture the existing condition of the river channel in Sangatta River estuary, including the bathymetry of the river bed, and the cross-sectional dimensions of the river, 2) to design a stable navigation channel in Sangatta River estuary that allows less maintenance dredging and improves navigability of the channel during a critical condition when the water level is at the lowest, and 3) to test the effectiveness of the stable cross section in term of the availability of navigable depth. This research is divided into five stages, namely: 1) preparatory stage and preliminary survey, 2) main surveys, 3) hydrological and hydraulic analysis, 4) waterway design, and 5) dredging plan. The hydraulic analysis also includes determining the water level and depth profiles before and after dredging. HEC-RAS software is used to simulate, for each month, the water level and depth profiles in the channel at a critical condition when the sea water level is at low water spring (LWS) coincides with the river flow of 50% probability of occurrence, Q50. A stable channel for Sangatta River estuary is characterized with a bed slope, S = 0.00015, a flow depth, D = 3.6 m, a bed width, b = 76.3 m and a sidewall slope, m = 1.5. The simulation results show that the stable cross sections of the river provide sufficient water depth for navigation, even during the critical condition.

Highlights

  • The depth of navigation channel is generally designed only based on vessel size without considering river morphodynamic processes, such as bank erosion [1, 2, 3], scouring, and siltation, which dictate the crosssectional dimensions of the river

  • The stable slope and stable cross-sectional dimensions are acceptable and they can be referred for developing navigation channel in Sangatta River estuary

  • The stable channel geometry for Sangatta River estuary is characterized with the following dimensions: bed slope, S = 0.00015, water depth, D = 3.6 m, bed width, b = 76.3 m and side wall slope, m = 1.5

Read more

Summary

Introduction

The depth of navigation channel is generally designed only based on vessel size without considering river morphodynamic processes, such as bank erosion [1, 2, 3], scouring, and siltation, which dictate the crosssectional dimensions of the river. Stable slope and cross-sectional dimensions can be predicted using various methods, based on dominant discharge and bed sediment size [6, 9, 10]. Most of the time, those type of data are not available or lacking [11] This is one of the reasons why the stable cross-sectional dimensions are rarely taken into consideration in determining the depth of navigation channels

Objectives
Methods
Findings
Conclusion
Full Text
Published version (Free)

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 call