A numerical study of onshore ripple migration using a Eulerian two-phase model

dc.contributor.author Salimi‐Tarazouj, Ali
dc.contributor.author Hsu, Tian-Jian
dc.contributor.author Traykovski, Peter A.
dc.contributor.author Cheng, Zhen
dc.contributor.author Chauchat, Julien
dc.date.accessioned 2021-05-10T21:57:05Z
dc.date.available 2021-06-29T06:17:16Z
dc.date.issued 2020-12-29
dc.description Author Posting. © American Geophysical Union, 2021. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Oceans 126(2), (2021): e2020JC016773, https://doi.org/10.1029/2020JC016773. en_US
dc.description.abstract A new modeling methodology for ripple dynamics driven by oscillatory flows using a Eulerian two‐phase flow approach is presented in order to bridge the research gap between near‐bed sediment transport via ripple migration and suspended load transport dictated by ripple induced vortices. Reynolds‐averaged Eulerian two‐phase equations for fluid phase and sediment phase are solved in a two‐dimensional vertical domain with a k‐ε closure for flow turbulence and particle stresses closures for short‐lived collision and enduring contact. The model can resolve full profiles of sediment transport without making conventional near‐bed load and suspended load assumptions. The model is validated with an oscillating tunnel experiment of orbital ripple driven by a Stokes second‐order (onshore velocity skewed) oscillatory flow with a good agreement in the flow velocity and sediment concentration. Although the suspended sediment concentration far from the ripple in the dilute region was underpredicted by the present model, the model predicts an onshore ripple migration rate that is in very good agreement with the measured value. Another orbital ripple case driven by symmetric sinusoidal oscillatory flow is also conducted to contrast the effect of velocity skewness. The model is able to capture a net offshore‐directed suspended load transport flux due to the asymmetric primary vortex consistent with laboratory observation. More importantly, the model can resolve the asymmetry of onshore‐directed near‐bed sediment flux associated with more intense boundary layer flow speed‐up during onshore flow cycle and sediment avalanching near the lee ripple flank which force the onshore ripple migration. en_US
dc.description.embargo 2021-06-29 en_US
dc.description.sponsorship This study is supported by National Science Foundation (Grant no. OCE‐1635151) and Strategic Environmental Research and Development Program (Grant no. MR20‐1478). en_US
dc.identifier.citation Salimi-Tarazouj, A., Hsu, T., Traykovski, P., Cheng, Z., & Chauchat, J. (2021). A numerical study of onshore ripple migration using a Eulerian two-phase model. Journal of Geophysical Research: Oceans, 126(2), e2020JC016773. en_US
dc.identifier.doi 10.1029/2020JC016773
dc.identifier.uri https://hdl.handle.net/1912/27090
dc.publisher American Geophysical Union en_US
dc.relation.uri https://doi.org/10.1029/2020JC016773
dc.subject Orbital ripples en_US
dc.subject Ripple migration en_US
dc.subject Sediment transport en_US
dc.subject Two‐phase model en_US
dc.title A numerical study of onshore ripple migration using a Eulerian two-phase model en_US
dc.type Article en_US
dspace.entity.type Publication
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