Visualisation of Flow at the Headland-generated Recirculation Zone

Experimental investigations were carried out in the Manchester Tidal flow Facility (MTF) to study the recirculation zone generated by flow past a headland in shallow steady flow. The experiments were performed in a flume with a rough, sloped beach. Fluorescent dye was released at specific points on...

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Main Author: Tang, Fu Ee
Other Authors: Associate Professor Dr Sobri Harun
Format: Conference Paper
Published: Universiti Teknologi Malaysia 2009
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/34706
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author Tang, Fu Ee
author2 Associate Professor Dr Sobri Harun
author_facet Associate Professor Dr Sobri Harun
Tang, Fu Ee
author_sort Tang, Fu Ee
building Curtin Institutional Repository
collection Online Access
description Experimental investigations were carried out in the Manchester Tidal flow Facility (MTF) to study the recirculation zone generated by flow past a headland in shallow steady flow. The experiments were performed in a flume with a rough, sloped beach. Fluorescent dye was released at specific points on a grid located in the generated recirculation zone. The Planar laser-induced fluorescence (PLIF) technique was used for flow visualisation. Residual dye decay profiles were also produced from raw PLIF images to study the flushing characteristics. Compared to discharge at other locations, trapping of released dye here is significant, and a relatively long time is needed to flush the residual dye. The decay profiles agreed with the observations from flow visualisation. The recirculatory flow acted to retain and increase the residual dye, and eventually flushed it into the free stream. A dead zone, where flow is almost stagnant and severe trapping occurs, has been identified about one width of the headland away, near the shore. This has serious implications towards the water quality in such areas in real life situations.
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spelling curtin-20.500.11937-347062017-10-02T02:27:48Z Visualisation of Flow at the Headland-generated Recirculation Zone Tang, Fu Ee Associate Professor Dr Sobri Harun headland wakes recirculation flushing steady flow Coastal environment Experimental investigations were carried out in the Manchester Tidal flow Facility (MTF) to study the recirculation zone generated by flow past a headland in shallow steady flow. The experiments were performed in a flume with a rough, sloped beach. Fluorescent dye was released at specific points on a grid located in the generated recirculation zone. The Planar laser-induced fluorescence (PLIF) technique was used for flow visualisation. Residual dye decay profiles were also produced from raw PLIF images to study the flushing characteristics. Compared to discharge at other locations, trapping of released dye here is significant, and a relatively long time is needed to flush the residual dye. The decay profiles agreed with the observations from flow visualisation. The recirculatory flow acted to retain and increase the residual dye, and eventually flushed it into the free stream. A dead zone, where flow is almost stagnant and severe trapping occurs, has been identified about one width of the headland away, near the shore. This has serious implications towards the water quality in such areas in real life situations. 2009 Conference Paper http://hdl.handle.net/20.500.11937/34706 Universiti Teknologi Malaysia restricted
spellingShingle headland wakes
recirculation
flushing
steady flow
Coastal environment
Tang, Fu Ee
Visualisation of Flow at the Headland-generated Recirculation Zone
title Visualisation of Flow at the Headland-generated Recirculation Zone
title_full Visualisation of Flow at the Headland-generated Recirculation Zone
title_fullStr Visualisation of Flow at the Headland-generated Recirculation Zone
title_full_unstemmed Visualisation of Flow at the Headland-generated Recirculation Zone
title_short Visualisation of Flow at the Headland-generated Recirculation Zone
title_sort visualisation of flow at the headland-generated recirculation zone
topic headland wakes
recirculation
flushing
steady flow
Coastal environment
url http://hdl.handle.net/20.500.11937/34706