Instytut Budownictwa Wodnego
Polskiej Akademii Nauk

Essay #8468 details

ATTRIBUTEVALUE
typeC
database id8468
title
authors
affiliations
year2013
seriesArchives of Hydro-Engineering and Environmental Mechanics
issueVol. 60, No. 1-4
publisherWydawnictwo IBW PAN
placeGdańsk
attributes[published] [reviewed] [scientific] [international reach]
languageen

Parts

ATTRIBUTEVALUE
typeA
database id8469
title60 lat Instytutu Budownictwa Wodnego PAN w Gdańsku
authorsSawicki A.
pages3 — 30
notesKopia w oprac. Tp4392
full text linkhttp://www.ibwpan.gda.pl/storage/app/media/ahem/ahem60str003.pdf
affiliations
  1. Dyrektor IBW PAN, e-mail: as@ibwpan.gda.pl
attributes[reviewed]
languagepl
ATTRIBUTEVALUE
typeA
database id8558
titleLagrangian model for a single saltating grain in the near-wall region of an open-channel flow
authorsCzernuszenko W.
pages31 — 50
full text linkhttp://www.ibwpan.gda.pl/storage/app/media/ahem/ahem60str031.pdf
keywordsLagrangian model, open-channel flow, particle-particle interaction
affiliations
  1. Institute of Geophysics, Polish Academy of Sciences, 01-452 Warszawa, Ks. Janusza 64, Poland, e-mail: wczer@igf.edu.pl
abstractsA mathematical model for the continuous saltation of a particle near the granular bed in an open-channel flow is developed in detail. The model is based on the Lagrangian equations governing particle motion, and it takes into account the following forces: drag, lift, gravitation, virtual mass and the force responsible for particle-particle interactions. A model of particle-particle collisions is developed and used to determine the mean impulsive force acting upon a particle flowing and rebounding from the channel bed. The model can simulate the continuous saltation trajectories of a single particle in the near-bed region of turbulent flows, in which particle motion is controlled by collisions. The model has been calibrated and verified with available published data in a rather wide range of grain sizes from 0.53 mm to 15 mm. All parameters, such as lift, drag, restitution, friction coefficients and roughness height, have been set on the basis of a reanalysis of these published data.
attributes[reviewed] [scientific]
languageen
ATTRIBUTEVALUE
typeA
database id8559
titleLax-Wendroff and McCormack schemes for numerical simulation of unsteady gradually and rapidly varied open channel flow
authorsMachalińska-Murawska J., Szydłowski M.
pages51 — 62
full text linkhttp://www.ibwpan.gda.pl/storage/app/media/ahem/ahem60str051.pdf
keywordsopen channel flow, mathematical modeling, numerical simulation, FDM schemes
affiliations
  1. University of Technology, Faculty of Civil and Environmental Engineering, ul. Narutowicza 11/12, 80–233 Gdańsk, Poland, e-mail: ju ma@tlen.pl
abstractsTwo explicit schemes of the finite difference method are presented and analyzed in the paper. The applicability of the Lax-Wendroff and McCormack schemes for modeling unsteady rapidly and gradually varied open channel flow is investigated. For simulation of the transcritical flow the original and improved McCormack scheme is used. The schemes are used for numerical solution of one dimensional Saint-Venant equations describing free surface water flow. Two numerical simulations of flow with different hydraulic characteristics were performed – the first one for the extreme flow of the dam-break type and the second one for the simplified flood wave propagation problem. The computational results are compared to each other and to arbitrary solutions.
attributes[reviewed] [scientific]
languageen
ATTRIBUTEVALUE
typeA
database id8560
titleOn the SPH approximations in modeling water waves
authorsSzmidt K.
pages63 — 86
full text linkhttp://www.ibwpan.gda.pl/storage/app/media/ahem/ahem60str063.pdf
keywordswater wave, SPH modeling, consistency, kernel correction
affiliations
  1. Institute of Hydro-Engineering, Polish Academy of Sciences, ul. Kościerska 7, 80-328 Gdańsk, Poland, e-mail: jks@ibwpan.gda.pl
abstractsThis paper presents an examination of approximation aspects of the Smoothed Particle Hydrodynamics (SPH) in modeling the water wave phenomenon. Close attention is paid on consistency of the SPH formulation and its relation with a correction technique applied to improve the method accuracy. The considerations are confined to flow fields within finite domains with a free surface and fixed solid boundaries with free slip boundary conditions. In spite of a wide application of the SPH method in fluid mechanics, the appropriate modeling of the boundaries is still not clear. For solid straight line boundaries, a natural way is to use additional (virtual, ghost) particles outside the boundary and take into account mirror reflection of associated field variables. Such a method leads to good results, except for a vicinity of solid horizontal bottoms where, because of the SPH approximations in the description of pressure, a stratification of the fluid material particles may occur. In order to illustrate the last phenomenon, some numerical tests have been made. These numerical experiments show that the solid fluid bottom attracts the material particles and thus, to prevent these particles from penetration into the bottom, a mutual exchange of positions of real and ghost particles has been used in a computation procedure.
attributes[reviewed] [scientific]
languageen
points6
ATTRIBUTEVALUE
typeA
database id8561
titleApplication of an element-free Galerkin method to water wave propagation problems
authorsStaroszczyk R.
pages87 — 105
full text linkhttp://www.ibwpan.gda.pl/storage/app/media/ahem/ahem60str087.pdf
keywordsgravity water wave, transient problem, element-free Galerkin method
affiliations
  1. Institute of Hydro-Engineering, Polish Academy of Sciences, ul. Kościerska 7, 80-328 Gdańsk, Poland, e-mail: rstar@ibwpan.gda.pl
abstractsThe paper is concerned with the problem of gravitational wave propagation in water of variable depth. The problem is solved numerically by applying an element-free Galerkin method. First, the proposed model is validated by comparing its predictions with experimental data for the plane flow in water of uniform depth. Then, as illustrations, results of numerical simulations performed for plane gravity waves propagating through a region with a sloping bed are presented. These results show the evolution of the free-surface elevation, displaying progressive steepening of the wave over the sloping bed, followed by its attenuation in a region of uniform depth. In addition, some of the results of the present model are compared with those obtained earlier by using the conventional finite element method.
attributes[reviewed] [scientific]
languageen
points6

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