Study on the propagation of regular water waves in a numerical wave flume with the ?-SPHC model

被引:7
作者
Liang, Guangqi [1 ]
Yang, Xi [1 ]
Zhang, Zhifan [1 ]
Zhang, Guiyong [1 ,2 ]
机构
[1] Dalian Univ Technol, Sch Naval Architecture Engn, State Key Lab Struct Anal Ind Equipment, Dalian 116024, Peoples R China
[2] Collaborat Innovat Ctr Adv Ship & Deep Sea Explora, Shanghai 200240, Peoples R China
基金
中国国家自然科学基金;
关键词
Regular water waves; 2D numerical wave flume; Meshless particle scheme; WCSPH method; -SPHC model; SMOOTHED PARTICLE HYDRODYNAMICS; FINITE-DIFFERENCE METHOD; FREE-SURFACE; NONLINEAR-WAVE; SIMULATION; GENERATION; FLOWS; TANK;
D O I
10.1016/j.apor.2023.103559
中图分类号
P75 [海洋工程];
学科分类号
0814 ; 081505 ; 0824 ; 082401 ;
摘要
Waves, a phenomenon of variable scale fluctuations common to the surface of the ocean, are the major loads acting on marine floats and play a pivotal role in the study of the hydrodynamics of offshore and deep-water structures. In this work, a two-dimensional (2D) numerical wave flume (NWF) is formed to simulate the propagation of regular water waves by the weakly compressible smoothed particle hydrodynamics-based (WCSPH) model. Artificial density and viscosity diffusion terms are used to stabilize the pressure field and numerical simulation, respectively. Based on the o-SPH model, the o-SPHC one is constructed by introducing the correction matrix into the calculation of the pressure gradient operator in the momentum equation. The o-SPHC model can guarantee second-order calculation accuracy even if the kernel function support domain is truncated. Besides, the destruction of momentum conservation can be greatly suppressed with its high symmetric, which facilitates the reduction of energy dissipation in the wave propagation process. In order to confirm the accuracy and stability of the developed 2D o-SPHC-based NWF, five classical benchmark tests are examined and discussed. The simulation results indicate that the adopted numerical wave flume performs well in predicting the dynamic evolution of regular water waves, which shows its potential for further investigation of more challenging hydrodynamic issues in real-world applications.
引用
收藏
页数:16
相关论文
共 78 条
[1]   A generalized wall boundary condition for smoothed particle hydrodynamics [J].
Adami, S. ;
Hu, X. Y. ;
Adams, N. A. .
JOURNAL OF COMPUTATIONAL PHYSICS, 2012, 231 (21) :7057-7075
[2]   David J. Benney: Nonlinear Wave and Instability Processes in Fluid Flows [J].
Akylas, T. R. .
ANNUAL REVIEW OF FLUID MECHANICS, VOL 52, 2020, 52 :21-36
[3]   Long-crested wave generation and absorption for SPH-based DualSPHysics model [J].
Altomare, C. ;
Dominguez, J. M. ;
Crespo, A. J. C. ;
Gonzalez-Cao, J. ;
Suzuki, T. ;
Gomez-Gesteira, M. ;
Troch, P. .
COASTAL ENGINEERING, 2017, 127 :37-54
[4]   The damping of viscous gravity waves [J].
Antuono, M. ;
Colagrossi, A. .
WAVE MOTION, 2013, 50 (02) :197-209
[5]   Numerical diffusive terms in weakly-compressible SPH schemes [J].
Antuono, M. ;
Colagrossi, A. ;
Marrone, S. .
COMPUTER PHYSICS COMMUNICATIONS, 2012, 183 (12) :2570-2580
[6]   Propagation of gravity waves through an SPH scheme with numerical diffusive terms [J].
Antuono, M. ;
Colagrossi, A. ;
Marrone, S. ;
Lugni, C. .
COMPUTER PHYSICS COMMUNICATIONS, 2011, 182 (04) :866-877
[7]   Free-surface flows solved by means of SPH schemes with numerical diffusive terms [J].
Antuono, M. ;
Colagrossi, A. ;
Marrone, S. ;
Molteni, D. .
COMPUTER PHYSICS COMMUNICATIONS, 2010, 181 (03) :532-549
[8]   A two-dimensional numerical wave flume - Part 1: Nonlinear wave generation, propagation, and absorption [J].
Baudic, SF ;
Williams, AN ;
Kareem, A .
JOURNAL OF OFFSHORE MECHANICS AND ARCTIC ENGINEERING-TRANSACTIONS OF THE ASME, 2001, 123 (02) :70-75
[9]  
Cao H.J., 2014, INT J OCEAN SYST ENG, V4, P49, DOI [10.5574/IJOSE.2014.4.1.049, DOI 10.5574/IJOSE.2014.4.1.049]
[10]   Generalized finite difference method for solving two-dimensional non-linear obstacle problems [J].
Chan, Hsin-Fang ;
Fan, Chia-Ming ;
Kuo, Chia-Wen .
ENGINEERING ANALYSIS WITH BOUNDARY ELEMENTS, 2013, 37 (09) :1189-1196