Equilibrium shapes of coastline in plan

AuthorNarongsak Vichetpan
Call NumberAIT Thesis no. 280
Subject(s)Coast changes
NoteA thesis submitted in partial fulfillment of the requirements for the degree of Master of Engineering of the Asian Institute of Technology, Bangkok, Thailand.
PublisherAsian Institute of Technology
AbstractA straight sedimentary coastline containing headlands, if it suffers persistent waves from an oblique direction and no replenishment is provided for material removed down coast, will assume a crenulate shape which becomes progressively more indented. Finally a shape is reached which is in equilibrium with the waves. This occurs when the incoming waves break simultaneously around the periphery and there is no further longshore drift. The development of such equilibrium shaped bays was studied by means of a model in which wave direction and wave periods were the sole variables. Thus the wave height, water depth, beach height and sedimentary material were the same throughout. The shape of the bay at various stages from straight line to fully stable was measured after various wave durations. It was found that the major curved portion of the water line was a logarithmic spiral, the constant of which varied throughout. A consistent pattern was observed for this constant for the three wave approach angles of 30°, 45° and 60° and the three wave periods of 0.6, 1.0 and 1.4 seconds.
Year1969
TypeThesis
SchoolStudent Research Before 1980
DepartmentOther Field of Studies (No Department)
Academic Program/FoSThesis (Year <=1979)
Chairperson(s)Silvester, Richard
Examination Committee(s)Pichai Boonyakanjana ;Ackermann, Norbert L
Scholarship Donor(s)Asian Institute of Technology
DegreeThesis (M. Eng) - Asian Institute of Technology, 1969


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