000			naa a22 7ar4500
016			_a000223953100002
022			_a0029-8018
040			_aNEU
041			_aeng
050	0	4	_aGC11.2
100	1		_9577832 _aTurker, U.
245	1	0	_aAverage sediment dislocation analysis for barred profiles. _cU. Turker, M.S.Kabdasli.
260			_c2004. _bPergamon-Elsevier Science Ltd., _aOxford :
520			_aThe difference between 'the equilibrium wave energy dissipation rate' and 'the wave energy dissipation rate' is incorporated in energy per unit of bed area that sediment particles should bear in order to dislocate their position in forming the offshore bar. The result depicted average displacement of sediment particles while the beach profile morphologically changes under storm waves. Theoretical hypothesis is tested using series of experiments such that the volume of offshore bar and the fictive period for the time scale of sediment dislocation, under regular and irregular wave conditions, could be examined. Findings show that fall speed parameter and dimensionless depth parameter govern the average dislocation of sediment particles. (C) 2004 Elsevier Ltd. All rights reserved.
650		0	_9572720 _aNear East University Article
650		0	_9124518 _aOceanography
650		0	_9572723 _aYakın Doğu Üniversitesi Makale
650			_9120132 _aEnergy dissipation
650			_9120253 _aEquilibrium
773			_gOCT 2004, Vol 31 Issue 14-15, p1741-1756 _tOcean Engineering _x00298018
856			_uhttp://library.neu.edu.tr:2048/login?url=http://dx.doi.org/10.1016/j.oceaneng.2004.03.008
942			_x1000007 _kGC00000112A942004 _cOED
005			20161004113739.0
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