Hydrodynamics of metachronal paddling: effects of varying Reynolds number and phase lag
Negatively buoyant freely swimming crustaceans such as krill must generate downward momentum in order to maintain their position in the water column. These animals use a drag-based propulsion strategy, where pairs of closely spaced swimming limbs are oscillated rhythmically from the tail to head. Ea...
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ftdoajarticles:oai:doaj.org/article:4f91dee8b89e4ed7913fdc30980a5f7b 2023-05-15T13:44:08+02:00 Hydrodynamics of metachronal paddling: effects of varying Reynolds number and phase lag Mitchell P. Ford Hong Kuan Lai Milad Samaee Arvind Santhanakrishnan 2019-10-01T00:00:00Z https://doi.org/10.1098/rsos.191387 https://doaj.org/article/4f91dee8b89e4ed7913fdc30980a5f7b EN eng The Royal Society https://royalsocietypublishing.org/doi/pdf/10.1098/rsos.191387 https://doaj.org/toc/2054-5703 2054-5703 doi:10.1098/rsos.191387 https://doaj.org/article/4f91dee8b89e4ed7913fdc30980a5f7b Royal Society Open Science, Vol 6, Iss 10 (2019) metachronal paddling rowing crustacean swimming drag-based propulsion aquatic locomotion Science Q article 2019 ftdoajarticles https://doi.org/10.1098/rsos.191387 2022-12-31T11:48:21Z Negatively buoyant freely swimming crustaceans such as krill must generate downward momentum in order to maintain their position in the water column. These animals use a drag-based propulsion strategy, where pairs of closely spaced swimming limbs are oscillated rhythmically from the tail to head. Each pair is oscillated with a phase delay relative to the neighbouring pair, resulting in a metachronal wave travelling in the direction of animal motion. It remains unclear how oscillations of limbs in the horizontal plane can generate vertical momentum. Using particle image velocimetry measurements on a robotic model, we observed that metachronal paddling with non-zero phase lag created geometries of adjacent paddles that promote the formation of counter-rotating vortices. The interaction of these vortices resulted in generating large-scale angled downward jets. Increasing phase lag resulted in more vertical orientation of the jet, and phase lags in the range used by Antarctic krill produced the most total momentum. Synchronous paddling produced lower total momentum when compared with metachronal paddling. Lowering Reynolds number by an order of magnitude below the range of adult krill (250–1000) showed diminished downward propagation of the jet and lower vertical momentum. Our findings show that metachronal paddling is capable of producing flows that can generate both lift (vertical) and thrust (horizontal) forces needed for fast forward swimming and hovering. Article in Journal/Newspaper Antarc* Antarctic Antarctic Krill Directory of Open Access Journals: DOAJ Articles Antarctic Royal Society Open Science 6 10 191387 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
metachronal paddling rowing crustacean swimming drag-based propulsion aquatic locomotion Science Q |
spellingShingle |
metachronal paddling rowing crustacean swimming drag-based propulsion aquatic locomotion Science Q Mitchell P. Ford Hong Kuan Lai Milad Samaee Arvind Santhanakrishnan Hydrodynamics of metachronal paddling: effects of varying Reynolds number and phase lag |
topic_facet |
metachronal paddling rowing crustacean swimming drag-based propulsion aquatic locomotion Science Q |
description |
Negatively buoyant freely swimming crustaceans such as krill must generate downward momentum in order to maintain their position in the water column. These animals use a drag-based propulsion strategy, where pairs of closely spaced swimming limbs are oscillated rhythmically from the tail to head. Each pair is oscillated with a phase delay relative to the neighbouring pair, resulting in a metachronal wave travelling in the direction of animal motion. It remains unclear how oscillations of limbs in the horizontal plane can generate vertical momentum. Using particle image velocimetry measurements on a robotic model, we observed that metachronal paddling with non-zero phase lag created geometries of adjacent paddles that promote the formation of counter-rotating vortices. The interaction of these vortices resulted in generating large-scale angled downward jets. Increasing phase lag resulted in more vertical orientation of the jet, and phase lags in the range used by Antarctic krill produced the most total momentum. Synchronous paddling produced lower total momentum when compared with metachronal paddling. Lowering Reynolds number by an order of magnitude below the range of adult krill (250–1000) showed diminished downward propagation of the jet and lower vertical momentum. Our findings show that metachronal paddling is capable of producing flows that can generate both lift (vertical) and thrust (horizontal) forces needed for fast forward swimming and hovering. |
format |
Article in Journal/Newspaper |
author |
Mitchell P. Ford Hong Kuan Lai Milad Samaee Arvind Santhanakrishnan |
author_facet |
Mitchell P. Ford Hong Kuan Lai Milad Samaee Arvind Santhanakrishnan |
author_sort |
Mitchell P. Ford |
title |
Hydrodynamics of metachronal paddling: effects of varying Reynolds number and phase lag |
title_short |
Hydrodynamics of metachronal paddling: effects of varying Reynolds number and phase lag |
title_full |
Hydrodynamics of metachronal paddling: effects of varying Reynolds number and phase lag |
title_fullStr |
Hydrodynamics of metachronal paddling: effects of varying Reynolds number and phase lag |
title_full_unstemmed |
Hydrodynamics of metachronal paddling: effects of varying Reynolds number and phase lag |
title_sort |
hydrodynamics of metachronal paddling: effects of varying reynolds number and phase lag |
publisher |
The Royal Society |
publishDate |
2019 |
url |
https://doi.org/10.1098/rsos.191387 https://doaj.org/article/4f91dee8b89e4ed7913fdc30980a5f7b |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic Antarctic Krill |
genre_facet |
Antarc* Antarctic Antarctic Krill |
op_source |
Royal Society Open Science, Vol 6, Iss 10 (2019) |
op_relation |
https://royalsocietypublishing.org/doi/pdf/10.1098/rsos.191387 https://doaj.org/toc/2054-5703 2054-5703 doi:10.1098/rsos.191387 https://doaj.org/article/4f91dee8b89e4ed7913fdc30980a5f7b |
op_doi |
https://doi.org/10.1098/rsos.191387 |
container_title |
Royal Society Open Science |
container_volume |
6 |
container_issue |
10 |
container_start_page |
191387 |
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1766198069838217216 |