Asian and Pacific Coasts 2003 2004
DOI: 10.1142/9789812703040_0059
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Lagrangian Gridless Model of Toe Scouring of Seawall Due to Tsunami Return Flow

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Cited by 3 publications
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“…By following Hayashi et al (2003) and Ikari et al (2010), both the normal and the tangential velocity components of the flow are used to evaluate the sediment initiation. The two flow velocities acting on a movable bed particle are obtained by interpolating the velocities of nearby inner fluid particles to this reference particle using the SPH kernel function, as follows (Ran et al, 2013):…”
Section: Fig 1 Different Types Of Particles Near Movable Bed In Isphmentioning
confidence: 99%
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“…By following Hayashi et al (2003) and Ikari et al (2010), both the normal and the tangential velocity components of the flow are used to evaluate the sediment initiation. The two flow velocities acting on a movable bed particle are obtained by interpolating the velocities of nearby inner fluid particles to this reference particle using the SPH kernel function, as follows (Ran et al, 2013):…”
Section: Fig 1 Different Types Of Particles Near Movable Bed In Isphmentioning
confidence: 99%
“…Equation (26) follows Hayashi et al (2003), in which collision F = fluid force on the bed surface and is assumed to be the self-weight of sediment grain under critical condition, m = mass of sediment grain and t  = computational time step.…”
Section: Fig 1 Different Types Of Particles Near Movable Bed In Isphmentioning
confidence: 99%
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“…In terms of existing SPH practice to model the sediment scouring, there are two different approaches: (1) Most of documented works treated the water and sediment as different fluid components and therefore, relevant interaction models are used to link the two phases (Shakibaeinia and Jin, 2011;Manenti et al, 2016); (2) The other approach, which will also be adopted in the present paper, considered the counterbalance between the fluid force and sediment bed resistance. As a result, either the critical velocity (Hayashi et al, 2003;Ran et al 2005) or the critical shear stress (Manenti et al, 2012) criterion can be used to determine the initiation of sediment particles when the threshold condition is satisfied. The purpose of present research is to develop a 3D ISPH sediment erosion model to study movable bed scours around a vertical circular cylinder.…”
Section: Introductionmentioning
confidence: 99%