#TITLE_ALTERNATIVE#

• Main Author: WIDIASTUTY (NIM 22404002), MARIA
• Format: Theses
• Language: Indonesia
• Online Access: https://digilib.itb.ac.id/gdl/view/8529
• Institution: Institut Teknologi Bandung

Processing of erotion and sedimentasion occur by means sediment transport although bed load sediment as well as suspended sediment. Afterwards by sediment transport can be able to monitoring change of morfologion/bathymetri sea level. Sediment transport will be engaged water current and particle sediment. As a general sedimen transport rated at about 3 category that is: bed load, suspended load and wash load. Bed load sediment is sediment transport that experience contact roll over and over during sliding, jumping dan rolling. Where as Suspended load that no experience with base and size particle (Murphy dan Aguirre, 1985;Fredsoe and Rolf, 1993 in Mubarak, 2004). and Wash load composed with small particle, and commonly wash load that is not basic composition. Calculation disribution sediment and change of morfologion/bathymetri used model numeric what is expexted of condition in value. Result analysis refers change of morfologion/bathymetri when experience area work out erotion, will about scraped and basic topography which to use ease up, where as area which sedimentation, will be deposition and base topografhy with purpose more or depth of water increase shallow.