Difference between revisions of "Examples/2D/souto etal 2012 standingwave"

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In our simulation <math>g = 1</math>, <math>L = 1</math>, <math>\varepsilon = 0.1</math>, <math>\rho = 1</math> and <math>H / \Delta x = 100</math>, where <math>\Delta x</math> is the initial distance between the particles.
 
In our simulation <math>g = 1</math>, <math>L = 1</math>, <math>\varepsilon = 0.1</math>, <math>\rho = 1</math> and <math>H / \Delta x = 100</math>, where <math>\Delta x</math> is the initial distance between the particles.
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== Setting up the simulation ==
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== References ==
 
== References ==
 
<references />
 
<references />

Revision as of 14:14, 12 March 2015

Introduction

In this examples we are reproducing the simulation of the standing wave carried out by Souto et all (2012) [1].

The standing wave is defined on top of an infinite periodic fluid domain composed by rectangular subdomains of dimensions , with . In such domain a wave with length (i.e. the wave number is ) and amplitude is imposed. Denoting the ratio by the following velocity potential can be considered:

valid for small values of . In previous equations is the angular frequency given by the dispersion relation of gravity waves: , and corresponds to the flat free surface (In Fig. 13 of Souto et all (2012)[1] it is wrong described)

Therefore the velocity field can be computed as . It should be noticed that for a flat free surface is obtained.

With such velocity potential, for a viscous fluid, it is possible to get an analytical solution for the kinetic energy decay[2]:

where the kinematic viscosity can be computed from the Reynolds number:

In our simulation , , , and , where is the initial distance between the particles.

Setting up the simulation

References

  1. 1.0 1.1 Antonio Souto-Iglesias, Fabricio Macià, Leo M. González, Jose L. Cercos-Pita. On the consistency of MPS. Computer Physics Communications, 2012
  2. J. Lighthill. Waves in Fluids. Cambridge University Press, 2001