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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Published in:Royal Society Open Science
Main Authors: Mitchell P. Ford, Hong Kuan Lai, Milad Samaee, Arvind Santhanakrishnan
Format: Article in Journal/Newspaper
Language:English
Published: The Royal Society 2019
Subjects:
Q
Online Access:https://doi.org/10.1098/rsos.191387
https://doaj.org/article/4f91dee8b89e4ed7913fdc30980a5f7b
id ftdoajarticles:oai:doaj.org/article:4f91dee8b89e4ed7913fdc30980a5f7b
record_format openpolar
spelling 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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