Harmonic decomposition of forces and estimates of reduced mean flow in jackets subjected to waves and current

Aidan J. Archer*, Paul H. Taylor, Hugh Wolgamot, Jana Orszaghova, Saishuai Dai

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

Abstract

The interaction between porous structures and flows with mean and oscillatory components has many applications in fluid dynamics. One such application is the hydrodynamic forces on offshore jacket structures from waves and current, which have been shown to give a significant blockage effect, leading to a reduction in drag forces. To better understand this, we derived analytical expressions that describe the effect of current on drag forces from large waves, and conducted experiments that measured forces on a model jacket in collinear waves and currents. We utilised symmetry and phase-inversion techniques, relying on the underlying physics of wave structure interaction, to separate Morison drag and inertia-type forces and to decompose these forces into their respective frequency harmonics. We find that the odd harmonics of the drag force mostly contain the loads from waves, while even harmonics vary much more rapidly with the current speed flowing through the jacket. At the time of peak force, these current speeds were estimated to be 40 % of the undisturbed current and 50 % of the industry-standard estimates, a result that has significant implications for design and re-assessment of jackets. At times away from the peak force, when there are no waves and only current, the blockage effects are reduced. Hence, the variation in blocked current speeds appears to occur on a relatively fast time scale similar to the compact wave envelope. These findings may be generalisable to any jacket-type structure in flows with mean and high Keulegan–Carpenter number oscillatory components.
Original languageEnglish
Article numberA7
Number of pages34
JournalJournal of Fluid Mechanics
Volume1009
DOIs
Publication statusPublished - 14 Apr 2025

Funding

The authors acknowledge support from the ARC ITRH for Transforming energy Infrastructure through Digital Engineering (TIDE, http://TIDE.edu.au) which is led by The University of Western Australia, delivered with The University of Wollongong and several other Australian and International research partners, and funded by the Australian Research Council, INPEX Operations Australia, Shell Australia, Woodside Energy, Fugro Australia Marine, Wood Group Kenny Australia, RPS Group, Bureau Veritas and Lloyd’s Register Global Technology (Grant No. IH200100009). A.J.A. acknowledges financial support from a Forrest Research Foundation scholarship and an Australian Government Research Training Program scholarship. H.A.W. was supported by an Australian Research Council (ARC) Early Career Fellowship (DE200101478) and Shell Australia. H.A.W. and J.O. acknowledge the Australian Research Council Linkage Project LP210100397, the Research Impact Grant from the University of Western Australia and the Blue Economy Cooperative Research Centre CRC-20180101, established and supported under the Australian Government’s Cooperative Research Centres Program.

Keywords

  • waves
  • free-surface flows
  • surface gravity waves

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