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An experimental study on the spatiotemporal evolution of sand waves/ripples in turbulent boundary layer airflow
An experimental study was conducted to investigate the spatiotemporal evolution of sand waves/ripples submerged in a turbulent boundary layer airflow. While a digital image projection technique was applied to achieve temporally resolved measurements of the dynamically evolving sand surface morpholog...
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Published in: | Physics of fluids (1994) 2020-06, Vol.32 (6) |
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container_title | Physics of fluids (1994) |
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creator | Liu, Yang Jiang, Xianyang Lee, Cunbiao Hu, Hui |
description | An experimental study was conducted to investigate the spatiotemporal evolution of sand waves/ripples submerged in a turbulent boundary layer airflow. While a digital image projection technique was applied to achieve temporally resolved measurements of the dynamically evolving sand surface morphology, a combined particle tracking/imaging velocimetry technique was also used to reveal the two-phase (i.e., air–sediment) flow field during the dynamic sand wave/ripple evolution process. It was found that the sand bed surface would evolve from initial random three-dimensional (3D) sand wavelets to two-dimensional (2D) sand waves and further into well-organized sequences of 3D chevron-shaped sand ripples that are separated by longitudinal streaks, when exposed to the turbulent boundary layer airflow. A discrepancy of the local sand wave propagation at different transverse locations was revealed based on the wavelet analysis of the time-series of the sand bed height variation, which was suggested to contribute to the formation of the 3D chevron-shaped sand ripples. It was also found that the evolving sand waves/ripples could dramatically affect the near-bed two-phase (i.e., air–sediment) flow structures as indicated by the dramatically disturbed air–sediment flow structures. By correlating the sand surface profiles and the near-surface sand particle velocity patterns, a complete description of the dynamic sand bedform evolution was revealed with five dominant phases being defined: (I) initial strengthening phase, (II) transition phase, (III) ripple-modulated re-strengthening phase, (IV) stabilizing phase, and (V) longitudinal phase. |
doi_str_mv | 10.1063/1.5144522 |
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While a digital image projection technique was applied to achieve temporally resolved measurements of the dynamically evolving sand surface morphology, a combined particle tracking/imaging velocimetry technique was also used to reveal the two-phase (i.e., air–sediment) flow field during the dynamic sand wave/ripple evolution process. It was found that the sand bed surface would evolve from initial random three-dimensional (3D) sand wavelets to two-dimensional (2D) sand waves and further into well-organized sequences of 3D chevron-shaped sand ripples that are separated by longitudinal streaks, when exposed to the turbulent boundary layer airflow. A discrepancy of the local sand wave propagation at different transverse locations was revealed based on the wavelet analysis of the time-series of the sand bed height variation, which was suggested to contribute to the formation of the 3D chevron-shaped sand ripples. It was also found that the evolving sand waves/ripples could dramatically affect the near-bed two-phase (i.e., air–sediment) flow structures as indicated by the dramatically disturbed air–sediment flow structures. By correlating the sand surface profiles and the near-surface sand particle velocity patterns, a complete description of the dynamic sand bedform evolution was revealed with five dominant phases being defined: (I) initial strengthening phase, (II) transition phase, (III) ripple-modulated re-strengthening phase, (IV) stabilizing phase, and (V) longitudinal phase.</description><identifier>ISSN: 1070-6631</identifier><identifier>EISSN: 1089-7666</identifier><identifier>DOI: 10.1063/1.5144522</identifier><identifier>CODEN: PHFLE6</identifier><language>eng</language><publisher>Melville: American Institute of Physics</publisher><subject>Aerodynamics ; Air flow ; Digital imaging ; Evolution ; Fluid dynamics ; Morphology ; Particle tracking ; Phase transitions ; Ripples ; Sand beds ; Sediments ; Sequences ; Turbulent boundary layer ; Velocimetry ; Wave propagation ; Wavelet analysis</subject><ispartof>Physics of fluids (1994), 2020-06, Vol.32 (6)</ispartof><rights>Author(s)</rights><rights>2020 Author(s). Published under license by AIP Publishing.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c327t-de0108120d62580f2f2ebe554af6bb302b4749a6c2590ae7015c3e2e8b3542373</citedby><cites>FETCH-LOGICAL-c327t-de0108120d62580f2f2ebe554af6bb302b4749a6c2590ae7015c3e2e8b3542373</cites><orcidid>0000-0002-3565-6208 ; 0000-0001-6302-6644 ; 0000-0003-0289-3837 ; 0000-0001-7928-4138</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,1558,27923,27924</link.rule.ids></links><search><creatorcontrib>Liu, Yang</creatorcontrib><creatorcontrib>Jiang, Xianyang</creatorcontrib><creatorcontrib>Lee, Cunbiao</creatorcontrib><creatorcontrib>Hu, Hui</creatorcontrib><title>An experimental study on the spatiotemporal evolution of sand waves/ripples in turbulent boundary layer airflow</title><title>Physics of fluids (1994)</title><description>An experimental study was conducted to investigate the spatiotemporal evolution of sand waves/ripples submerged in a turbulent boundary layer airflow. While a digital image projection technique was applied to achieve temporally resolved measurements of the dynamically evolving sand surface morphology, a combined particle tracking/imaging velocimetry technique was also used to reveal the two-phase (i.e., air–sediment) flow field during the dynamic sand wave/ripple evolution process. It was found that the sand bed surface would evolve from initial random three-dimensional (3D) sand wavelets to two-dimensional (2D) sand waves and further into well-organized sequences of 3D chevron-shaped sand ripples that are separated by longitudinal streaks, when exposed to the turbulent boundary layer airflow. A discrepancy of the local sand wave propagation at different transverse locations was revealed based on the wavelet analysis of the time-series of the sand bed height variation, which was suggested to contribute to the formation of the 3D chevron-shaped sand ripples. It was also found that the evolving sand waves/ripples could dramatically affect the near-bed two-phase (i.e., air–sediment) flow structures as indicated by the dramatically disturbed air–sediment flow structures. By correlating the sand surface profiles and the near-surface sand particle velocity patterns, a complete description of the dynamic sand bedform evolution was revealed with five dominant phases being defined: (I) initial strengthening phase, (II) transition phase, (III) ripple-modulated re-strengthening phase, (IV) stabilizing phase, and (V) longitudinal phase.</description><subject>Aerodynamics</subject><subject>Air flow</subject><subject>Digital imaging</subject><subject>Evolution</subject><subject>Fluid dynamics</subject><subject>Morphology</subject><subject>Particle tracking</subject><subject>Phase transitions</subject><subject>Ripples</subject><subject>Sand beds</subject><subject>Sediments</subject><subject>Sequences</subject><subject>Turbulent boundary layer</subject><subject>Velocimetry</subject><subject>Wave propagation</subject><subject>Wavelet analysis</subject><issn>1070-6631</issn><issn>1089-7666</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp9kE1LAzEQhoMoWKsH_0HAk8K2-dgk3WMpfkHBi56X7O4Et2yTNR-t_femtGdPM8w8887Li9A9JTNKJJ_TmaBlKRi7QBNKFlWhpJSXx16RQkpOr9FNCBtCCK-YnCC3tBh-R_D9FmzUAw4xdQfsLI7fgMOoY-8ibEfn8w52bkh5YLEzOGjb4b3eQZj7fhwHCLjPV8k3achSuHHJdtof8KAP4LHuvRnc_hZdGT0EuDvXKfp6ef5cvRXrj9f31XJdtJypWHRAsnvKSCeZWBDDDIMGhCi1kU3DCWtKVVZatkxURIMiVLQcGCwaLkrGFZ-ih5Pu6N1PghDrjUve5pc1KylXigrKMvV4olrvQvBg6jEHkU3XlNTHPGtan_PM7NOJDW0fj7HYf-A_V2F2Ig</recordid><startdate>20200601</startdate><enddate>20200601</enddate><creator>Liu, Yang</creator><creator>Jiang, Xianyang</creator><creator>Lee, Cunbiao</creator><creator>Hu, Hui</creator><general>American Institute of Physics</general><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope><orcidid>https://orcid.org/0000-0002-3565-6208</orcidid><orcidid>https://orcid.org/0000-0001-6302-6644</orcidid><orcidid>https://orcid.org/0000-0003-0289-3837</orcidid><orcidid>https://orcid.org/0000-0001-7928-4138</orcidid></search><sort><creationdate>20200601</creationdate><title>An experimental study on the spatiotemporal evolution of sand waves/ripples in turbulent boundary layer airflow</title><author>Liu, Yang ; Jiang, Xianyang ; Lee, Cunbiao ; Hu, Hui</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c327t-de0108120d62580f2f2ebe554af6bb302b4749a6c2590ae7015c3e2e8b3542373</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Aerodynamics</topic><topic>Air flow</topic><topic>Digital imaging</topic><topic>Evolution</topic><topic>Fluid dynamics</topic><topic>Morphology</topic><topic>Particle tracking</topic><topic>Phase transitions</topic><topic>Ripples</topic><topic>Sand beds</topic><topic>Sediments</topic><topic>Sequences</topic><topic>Turbulent boundary layer</topic><topic>Velocimetry</topic><topic>Wave propagation</topic><topic>Wavelet analysis</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Liu, Yang</creatorcontrib><creatorcontrib>Jiang, Xianyang</creatorcontrib><creatorcontrib>Lee, Cunbiao</creatorcontrib><creatorcontrib>Hu, Hui</creatorcontrib><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Physics of fluids (1994)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Liu, Yang</au><au>Jiang, Xianyang</au><au>Lee, Cunbiao</au><au>Hu, Hui</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>An experimental study on the spatiotemporal evolution of sand waves/ripples in turbulent boundary layer airflow</atitle><jtitle>Physics of fluids (1994)</jtitle><date>2020-06-01</date><risdate>2020</risdate><volume>32</volume><issue>6</issue><issn>1070-6631</issn><eissn>1089-7666</eissn><coden>PHFLE6</coden><abstract>An experimental study was conducted to investigate the spatiotemporal evolution of sand waves/ripples submerged in a turbulent boundary layer airflow. While a digital image projection technique was applied to achieve temporally resolved measurements of the dynamically evolving sand surface morphology, a combined particle tracking/imaging velocimetry technique was also used to reveal the two-phase (i.e., air–sediment) flow field during the dynamic sand wave/ripple evolution process. It was found that the sand bed surface would evolve from initial random three-dimensional (3D) sand wavelets to two-dimensional (2D) sand waves and further into well-organized sequences of 3D chevron-shaped sand ripples that are separated by longitudinal streaks, when exposed to the turbulent boundary layer airflow. A discrepancy of the local sand wave propagation at different transverse locations was revealed based on the wavelet analysis of the time-series of the sand bed height variation, which was suggested to contribute to the formation of the 3D chevron-shaped sand ripples. It was also found that the evolving sand waves/ripples could dramatically affect the near-bed two-phase (i.e., air–sediment) flow structures as indicated by the dramatically disturbed air–sediment flow structures. By correlating the sand surface profiles and the near-surface sand particle velocity patterns, a complete description of the dynamic sand bedform evolution was revealed with five dominant phases being defined: (I) initial strengthening phase, (II) transition phase, (III) ripple-modulated re-strengthening phase, (IV) stabilizing phase, and (V) longitudinal phase.</abstract><cop>Melville</cop><pub>American Institute of Physics</pub><doi>10.1063/1.5144522</doi><tpages>22</tpages><orcidid>https://orcid.org/0000-0002-3565-6208</orcidid><orcidid>https://orcid.org/0000-0001-6302-6644</orcidid><orcidid>https://orcid.org/0000-0003-0289-3837</orcidid><orcidid>https://orcid.org/0000-0001-7928-4138</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Aerodynamics Air flow Digital imaging Evolution Fluid dynamics Morphology Particle tracking Phase transitions Ripples Sand beds Sediments Sequences Turbulent boundary layer Velocimetry Wave propagation Wavelet analysis |
title | An experimental study on the spatiotemporal evolution of sand waves/ripples in turbulent boundary layer airflow |
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