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A free-surface flow on a channel with step bottom is solved numerically by an integral equation method. The flow is assumed to be irrotational, two dimensional, and the pattern of flow is steady. Beside that, the fluid is assumed to be ideal which the characteristics are inviscid and incompressible....

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Main Author: SANDY AGUNG , GALIH
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/10480
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:10480
spelling id-itb.:104802017-09-27T11:43:07Z#TITLE_ALTERNATIVE# SANDY AGUNG , GALIH Indonesia Final Project Subcritical flow, integral equation method, hodograph variable, Froude Number. INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/10480 A free-surface flow on a channel with step bottom is solved numerically by an integral equation method. The flow is assumed to be irrotational, two dimensional, and the pattern of flow is steady. Beside that, the fluid is assumed to be ideal which the characteristics are inviscid and incompressible. The numerical result shows that the step generates a train of waves to the free-surface of fluid. The size of waves is influenced by the flow velocity, the height and slope of the step. The waves are characterized as long wave with ratio amplitude to wavelength of order 10(-2) or smaller. text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description A free-surface flow on a channel with step bottom is solved numerically by an integral equation method. The flow is assumed to be irrotational, two dimensional, and the pattern of flow is steady. Beside that, the fluid is assumed to be ideal which the characteristics are inviscid and incompressible. The numerical result shows that the step generates a train of waves to the free-surface of fluid. The size of waves is influenced by the flow velocity, the height and slope of the step. The waves are characterized as long wave with ratio amplitude to wavelength of order 10(-2) or smaller.
format Final Project
author SANDY AGUNG , GALIH
spellingShingle SANDY AGUNG , GALIH
#TITLE_ALTERNATIVE#
author_facet SANDY AGUNG , GALIH
author_sort SANDY AGUNG , GALIH
title #TITLE_ALTERNATIVE#
title_short #TITLE_ALTERNATIVE#
title_full #TITLE_ALTERNATIVE#
title_fullStr #TITLE_ALTERNATIVE#
title_full_unstemmed #TITLE_ALTERNATIVE#
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url https://digilib.itb.ac.id/gdl/view/10480
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