Mathematical modelling of arbitrary shaped domain based on dual reciprocity boundary element method with variable bathymetry

被引:0
|
作者
Priya, Prachi [1 ]
Kumar, Prashant [2 ]
Rajni [3 ]
机构
[1] Galgotias Univ, Sch Basic Sci, Dept Math, Greater Noida 201310, Uttar Pradesh, India
[2] Natl Inst Technol, Dept Appl Sci Math, Delhi 110036, India
[3] OP Jindal Global Univ, Jindal Global Business Sch, Sonipat 131001, Haryana, India
关键词
Dual reciprocity boundary element method; Helmholtz equation; Mild slope equation; Slopping bathymetry; Bottom friction; WAVE-INDUCED OSCILLATIONS; HARBOR OSCILLATIONS; THEORETICAL-ANALYSIS; VISAKHAPATNAM PORT; FRINGING REEFS; RESONANCE; BOTTOM; BASIN;
D O I
10.1016/j.oceaneng.2024.118366
中图分类号
U6 [水路运输]; P75 [海洋工程];
学科分类号
0814 ; 081505 ; 0824 ; 082401 ;
摘要
A robust mathematical model is presented in this paper for the multi-connected domain with variable bathymetry using dual reciprocity boundary element method (DRBEM) to analyze the combined effects of wave diffraction-refraction and reflection on the arbitrarily shaped harbor. The influence of sloping bathymetry and the impact of the bottom friction on the harbor resonance are investigated. The fluid domain is primarily separated into two regions Region-I (open sea region) and Region-II (harbor region). Further, Region-II is divided into multi-connected regions. The mild slope equation is rearranged to obtain the non-homogeneous Helmholtz equation, and utilizing the ordinary boundary element method to this non-homogeneous equation, the nonhomogeneous part will convert into a domain integral. The present model is verified by comparing it with the analytical examination of Wang et al.2015; Shao et al.2017. The wave amplification is determined for the Tshaped and TT-shaped domains to analyze the influence of bottom friction, and slopping bathymetry. Further, the present numerical approach is employed to the realistic port, Visakhapatnam port, India, and the four key locations are identified to analyze harbor resonance in the bottom friction and slopping bathymetry of the multiconnected region.
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页数:13
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