Sand Ripples and Dunes
An erodible bed sheared by a fluid flow, gas or liquid, is generally unstable, and bed forms grow. This review discusses the following issues, in light of the recent literature: What are the relevant dynamical mechanisms controlling the emergence of bed forms? Do they form by linear instability or n...
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Veröffentlicht in: | Annual review of fluid mechanics 2013-01, Vol.45 (1), p.469-493 |
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creator | Charru, François Andreotti, Bruno Claudin, Philippe |
description | An erodible bed sheared by a fluid flow, gas or liquid, is generally unstable, and bed forms grow. This review discusses the following issues, in light of the recent literature: What are the relevant dynamical mechanisms controlling the emergence of bed forms? Do they form by linear instability or nonlinear processes such as pattern coarsening? What determines their timescales and length scales, so different in air and water? What are the similarities and differences between aeolian and subaqueous patterns? What is the influence of the mode of transport: bed load, saltation, or suspension? Can bed forms emerge under any hydrodynamical regime, laminar and turbulent? Guided by these questions, we propose a unified description of bed-form growth and saturation, emphasizing the hydrodynamical regime in the inner layer and the relaxation phenomena associated with particle transport. |
doi_str_mv | 10.1146/annurev-fluid-011212-140806 |
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Guided by these questions, we propose a unified description of bed-form growth and saturation, emphasizing the hydrodynamical regime in the inner layer and the relaxation phenomena associated with particle transport.</description><identifier>ISSN: 0066-4189</identifier><identifier>EISSN: 1545-4479</identifier><identifier>DOI: 10.1146/annurev-fluid-011212-140806</identifier><identifier>CODEN: ARVFA3</identifier><language>eng</language><publisher>Palo Alto, CA: Annual Reviews</publisher><subject>Applied sciences ; bed forms ; Buildings. Public works ; Coarsening ; Condensed Matter ; Earth sciences ; Earth, ocean, space ; Engineering Sciences ; Exact sciences and technology ; Fluid dynamics ; Fluid flow ; Fluid mechanics ; Fluids mechanics ; Geomorphology, landform evolution ; Hydraulic constructions ; instability ; laminar flow ; Mechanics ; Physics ; relaxation phenomena ; Ripples ; River flow control. 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This review discusses the following issues, in light of the recent literature: What are the relevant dynamical mechanisms controlling the emergence of bed forms? Do they form by linear instability or nonlinear processes such as pattern coarsening? What determines their timescales and length scales, so different in air and water? What are the similarities and differences between aeolian and subaqueous patterns? What is the influence of the mode of transport: bed load, saltation, or suspension? Can bed forms emerge under any hydrodynamical regime, laminar and turbulent? Guided by these questions, we propose a unified description of bed-form growth and saturation, emphasizing the hydrodynamical regime in the inner layer and the relaxation phenomena associated with particle transport.</description><subject>Applied sciences</subject><subject>bed forms</subject><subject>Buildings. Public works</subject><subject>Coarsening</subject><subject>Condensed Matter</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Engineering Sciences</subject><subject>Exact sciences and technology</subject><subject>Fluid dynamics</subject><subject>Fluid flow</subject><subject>Fluid mechanics</subject><subject>Fluids mechanics</subject><subject>Geomorphology, landform evolution</subject><subject>Hydraulic constructions</subject><subject>instability</subject><subject>laminar flow</subject><subject>Mechanics</subject><subject>Physics</subject><subject>relaxation phenomena</subject><subject>Ripples</subject><subject>River flow control. Flood control</subject><subject>Sand</subject><subject>sediment transport</subject><subject>Soft Condensed Matter</subject><subject>Surficial geology</subject><subject>Transport</subject><subject>Turbulence</subject><subject>Turbulent flow</subject><issn>0066-4189</issn><issn>1545-4479</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><recordid>eNqVkEtLAzEURoMoWKtb1wURdBHNzTu4sdRHhYKg3YeYSXAknakTp-K_d8Yp3bu64XJyPu6H0BmQKwAur11VtU3Y4JjassAEgALFwIkmcg-NQHCBOVdmH40IkRJz0OYQHeX8QQjRIPQInb66qpi8lOt1CnnSv-_aKuRjdBBdyuFkO8do-XC_nM3x4vnxaTZdYCeY_sJeRKWZloZ4plQRaEFACcaNckxwELKIUcqghdRgFPg3UlAuPY2eM0ENG6PLQfvukl035co1P7Z2pZ1PF7bfEcalUtRsoGMvBnbd1J9tyF92VWYfUnJVqNtsgXV5IA2nHXozoL6pc25C3LmB2L44uy3O_hVnh-LsUFz3-3wb5LJ3KTau8mXeKaii3cm6T7kduF7mUqcrw3f-V9Qv4zKEHA</recordid><startdate>20130101</startdate><enddate>20130101</enddate><creator>Charru, François</creator><creator>Andreotti, Bruno</creator><creator>Claudin, Philippe</creator><general>Annual Reviews</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TB</scope><scope>7U5</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope><scope>1XC</scope><scope>VOOES</scope><orcidid>https://orcid.org/0000-0001-8975-4500</orcidid><orcidid>https://orcid.org/0000-0001-8328-6232</orcidid></search><sort><creationdate>20130101</creationdate><title>Sand Ripples and Dunes</title><author>Charru, François ; Andreotti, Bruno ; Claudin, Philippe</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a538t-c5f7838690c377de2d01753497a354156dff66e85681971cb0d246c2fc435293</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Applied sciences</topic><topic>bed forms</topic><topic>Buildings. Public works</topic><topic>Coarsening</topic><topic>Condensed Matter</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Engineering Sciences</topic><topic>Exact sciences and technology</topic><topic>Fluid dynamics</topic><topic>Fluid flow</topic><topic>Fluid mechanics</topic><topic>Fluids mechanics</topic><topic>Geomorphology, landform evolution</topic><topic>Hydraulic constructions</topic><topic>instability</topic><topic>laminar flow</topic><topic>Mechanics</topic><topic>Physics</topic><topic>relaxation phenomena</topic><topic>Ripples</topic><topic>River flow control. Flood control</topic><topic>Sand</topic><topic>sediment transport</topic><topic>Soft Condensed Matter</topic><topic>Surficial geology</topic><topic>Transport</topic><topic>Turbulence</topic><topic>Turbulent flow</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Charru, François</creatorcontrib><creatorcontrib>Andreotti, Bruno</creatorcontrib><creatorcontrib>Claudin, Philippe</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Hyper Article en Ligne (HAL)</collection><collection>Hyper Article en Ligne (HAL) (Open Access)</collection><jtitle>Annual review of fluid mechanics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Charru, François</au><au>Andreotti, Bruno</au><au>Claudin, Philippe</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Sand Ripples and Dunes</atitle><jtitle>Annual review of fluid mechanics</jtitle><date>2013-01-01</date><risdate>2013</risdate><volume>45</volume><issue>1</issue><spage>469</spage><epage>493</epage><pages>469-493</pages><issn>0066-4189</issn><eissn>1545-4479</eissn><coden>ARVFA3</coden><abstract>An erodible bed sheared by a fluid flow, gas or liquid, is generally unstable, and bed forms grow. This review discusses the following issues, in light of the recent literature: What are the relevant dynamical mechanisms controlling the emergence of bed forms? Do they form by linear instability or nonlinear processes such as pattern coarsening? What determines their timescales and length scales, so different in air and water? What are the similarities and differences between aeolian and subaqueous patterns? What is the influence of the mode of transport: bed load, saltation, or suspension? Can bed forms emerge under any hydrodynamical regime, laminar and turbulent? 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subjects | Applied sciences bed forms Buildings. Public works Coarsening Condensed Matter Earth sciences Earth, ocean, space Engineering Sciences Exact sciences and technology Fluid dynamics Fluid flow Fluid mechanics Fluids mechanics Geomorphology, landform evolution Hydraulic constructions instability laminar flow Mechanics Physics relaxation phenomena Ripples River flow control. Flood control Sand sediment transport Soft Condensed Matter Surficial geology Transport Turbulence Turbulent flow |
title | Sand Ripples and Dunes |
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