Temat: breaking dam - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: SPH - a comparison of neighbor search methods based on constant number of neighbors and constant cut-off radius
Autorzy:: Wróblewski, P.
Kopeć, M.
Boryczko, Krzysztof
Powiązania:: https://bibliotekanauki.pl/articles/1933174.pdf
Data publikacji:: 2007
Wydawca:: Politechnika Gdańska
Tematy:: SPH
simulations
incompressible fluids
constant cut-off radius method
constant number of neighbors method
breaking dam
side gap
time effectiveness
Opis:: Two methods of neighbor search for the SPH algorithm are presented, based on a constant number of neighbors and a constant cut-off radius. First, feasible methods of comparison were analyzed. Then, the two selected methods were compared visually and computationally. Considering the use of the SPH algorithm for simulating incompressible fluids, the obtained results suggest that the method with a constant cut-off radius is better than that with a constant number of neighbors. The simulation results of both methods are practically indistinguishable, while the computational costs favor one of them.
Źródło:: TASK Quarterly. Scientific Bulletin of Academic Computer Centre in Gdansk; 2007, 11, 3; 273-283
1428-6394
Pojawia się w:: TASK Quarterly. Scientific Bulletin of Academic Computer Centre in Gdansk
Dostawca treści:: Biblioteka Nauki

Artykuł

Skocz do pozycji: 2.

Tytuł:: Geomorphological effects of the catastrophic drainage of artificial reservoir in the Młynówka valley at Górowo Iławeckie, Poland
Autorzy:: Brykała, D.
Gierszewski, P.
Gębica, P.
Powiązania:: https://bibliotekanauki.pl/articles/294550.pdf
Data publikacji:: 2003
Wydawca:: Stowarzyszenie Geomorfologów Polskich
Tematy:: flood, breaking of dam
flood forms and deposits
valley of the Młynówka Górowska river
Opis:: The problem concerns the catastrophic flood flow caused by the breaking of the dam of the artificial reservoir in the valley of the small river Młynówka Górowska. Extensive studies were focused on the section just below the broken dam, were the geomorphological effects of that event were most noticeable. A number of erosional and accumulative forms have been distinguished. The structure and grain size of the flood deposits have been studied. The occurrence of deposit sequences characteristic of slurry-flows has been found. The rapid fall of the flood wave was associated with the deposition of the coarser deposit fractions on the sides of the valley and of the finer ones on its floor.
Źródło:: Landform Analysis; 2003, 4; 75-82
1429-799X
Pojawia się w:: Landform Analysis
Dostawca treści:: Biblioteka Nauki

Artykuł

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