Calibration of UWA’s O-tube flume facility

The O-tube facility, designed and established at the University of Western Australia, is an innovative closed loop flume in which a random storm sequence can be reproduced via control of a large pump system. The O-tube facility is capable of simulating hydrodynamic conditions near the seabed and the...

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Published in:Volume 5: Ocean Engineering; CFD and VIV
Main Authors: Luo, Chengcai, An, Hongwei, Cheng, Liang, White, David
Format: Conference Object
Language:English
Published: ASME 2012
Subjects:
Online Access:https://eprints.soton.ac.uk/419913/
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spelling ftsouthampton:oai:eprints.soton.ac.uk:419913 2023-07-30T03:59:50+02:00 Calibration of UWA’s O-tube flume facility Luo, Chengcai An, Hongwei Cheng, Liang White, David 2012 https://eprints.soton.ac.uk/419913/ English eng ASME Luo, Chengcai, An, Hongwei, Cheng, Liang and White, David (2012) Calibration of UWA’s O-tube flume facility. In ASME 2012 31st International Conference on Ocean, Offshore and Arctic Engineering. vol. 5, ASME. pp. 121-131 . (doi:10.1115/OMAE2012-83274 <http://dx.doi.org/10.1115/OMAE2012-83274>). Conference or Workshop Item PeerReviewed 2012 ftsouthampton https://doi.org/10.1115/OMAE2012-83274 2023-07-09T22:22:00Z The O-tube facility, designed and established at the University of Western Australia, is an innovative closed loop flume in which a random storm sequence can be reproduced via control of a large pump system. The O-tube facility is capable of simulating hydrodynamic conditions near the seabed and the interaction with seabed sediment and any infrastructure that is resting on it. The purpose of carrying out the O-tube calibration described in this paper is to obtain the relationship between the motor rotation movement and the flow velocity generated in the O-tube, such that any required storm history within the performance envelope of the O-tube can be reproduced. A range of flow velocities and the corresponding pump speeds were measured under steady current, oscillatory flow and combined flow conditions. It was found that the relationship between the pump speed and the flow velocity varies with the oscillatory flow period. Based on the pump characteristic curves and O-tube system curves, the correlation between the motor speed and the flow velocity was derived by applying hydraulic theory and the principle of energy conservation. The derived correlation is validated by reproducing a wide range of target storm series, including a (1:5.8) scaled 100-year return period storm from the North West Shelf of Western Australia in 40 m water depth. Conference Object Arctic University of Southampton: e-Prints Soton Volume 5: Ocean Engineering; CFD and VIV 121 131
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language English
description The O-tube facility, designed and established at the University of Western Australia, is an innovative closed loop flume in which a random storm sequence can be reproduced via control of a large pump system. The O-tube facility is capable of simulating hydrodynamic conditions near the seabed and the interaction with seabed sediment and any infrastructure that is resting on it. The purpose of carrying out the O-tube calibration described in this paper is to obtain the relationship between the motor rotation movement and the flow velocity generated in the O-tube, such that any required storm history within the performance envelope of the O-tube can be reproduced. A range of flow velocities and the corresponding pump speeds were measured under steady current, oscillatory flow and combined flow conditions. It was found that the relationship between the pump speed and the flow velocity varies with the oscillatory flow period. Based on the pump characteristic curves and O-tube system curves, the correlation between the motor speed and the flow velocity was derived by applying hydraulic theory and the principle of energy conservation. The derived correlation is validated by reproducing a wide range of target storm series, including a (1:5.8) scaled 100-year return period storm from the North West Shelf of Western Australia in 40 m water depth.
format Conference Object
author Luo, Chengcai
An, Hongwei
Cheng, Liang
White, David
spellingShingle Luo, Chengcai
An, Hongwei
Cheng, Liang
White, David
Calibration of UWA’s O-tube flume facility
author_facet Luo, Chengcai
An, Hongwei
Cheng, Liang
White, David
author_sort Luo, Chengcai
title Calibration of UWA’s O-tube flume facility
title_short Calibration of UWA’s O-tube flume facility
title_full Calibration of UWA’s O-tube flume facility
title_fullStr Calibration of UWA’s O-tube flume facility
title_full_unstemmed Calibration of UWA’s O-tube flume facility
title_sort calibration of uwa’s o-tube flume facility
publisher ASME
publishDate 2012
url https://eprints.soton.ac.uk/419913/
genre Arctic
genre_facet Arctic
op_relation Luo, Chengcai, An, Hongwei, Cheng, Liang and White, David (2012) Calibration of UWA’s O-tube flume facility. In ASME 2012 31st International Conference on Ocean, Offshore and Arctic Engineering. vol. 5, ASME. pp. 121-131 . (doi:10.1115/OMAE2012-83274 <http://dx.doi.org/10.1115/OMAE2012-83274>).
op_doi https://doi.org/10.1115/OMAE2012-83274
container_title Volume 5: Ocean Engineering; CFD and VIV
container_start_page 121
op_container_end_page 131
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